松辽盆地滨北中东部构造特征的地球物理证据与油气构造条件分析
|
摘要
滨北中东部地区是松辽盆地的一部分,具有较好的油气前景,是松辽盆地研究中非常重要的区域。本文对松辽盆地滨北中东部的构造特征进行了详细的描述,并且应用了一定的重磁资料分析了研究区的断裂分布。在大量地质、地球物理资料的基础上,通过贯穿南北向的两条地震长剖面及其Vp分布对松辽盆地滨北中东部地区区域构造特征及演化进行了研究,并分析了滨北中东部地区的构造成因机制。蒙古-鄂霍茨克洋的关闭产生向南的挤压应力对松辽盆地的构造演化产生很大影响,表现为上侏罗统与下白垩统之间角度不整合。滨北中东部地区的盆地发育虽然也经历了断陷期、断坳转化期、坳陷期和萎缩期,但具有明显的自身演化特点。滨北中东部地区有利油气聚集带的分析应该放在深层的断陷期和断坳转化期的层位。滨北地区存在两个逆断层带,很可能是以后寻找油气的重点区域。根据滨北中东部地区的构造和圈闭研究,认为林甸断陷、绥化断陷和北安断陷为有利的油气聚集区带。
With the rapid development of science and technology in the world, there are evident progresses in the theories of the petroleum geology and geophysics, which promote oil and gas exploration in the field of exploration targets increasingly complex circumstances continuing to make new discoveries and breakthroughs and achieve great economic benefits. Songliao Basin is an important oil-producing area in China, the fruitful results in the oil and gas reserves has been achieved in the south of the Binzhou railway in the north of Songliao Basin, but the situation of the North Harbin area in the north of Songliao Basin is very different. The North Harbin area has been become an important area for exploration to succeed with the reduced oil and gas resources in the old exploration regions. Because of its especial tectonic location and rich oil and gas resources, the Songliao Basin has become one of the areas of the geological workers concerned, the much concern is on the South Harbin area of Songliao Basin, but the concern on the North Harbin area is relatively less.
In the nearly 50 years of the exploration process on the North Harbin area, the pre-work is all isolated study in a small area, large area integrated explanation has not existed, and the exploration degree is also low. With the abundance of exploration data, the development of geological and geophysical theories and the exploration technology, which provide the necessary conditions for the geological conditions and distribution rule in the formation of deep oil and gas. To this point we selected the northern and eastern North Harbin area in-depth study as the breakthrough and provided reference of oil and gas exploration for deep stratum in the entire Songliao Basin and similar international basins.
Compared to single seismic research, we use a number of gravity and magnetic data to study the fault system in Songliao Basin, and provide a basis for further determining the distribution of fault system. There are decades of basement rifts in North Harbin area, which are important on the framework structure of top layer and oil and gas concentrating. Most faults are in NNE and NE direction.
The seismic reflection layer of T5 corresponds the faulted sequence at the bottom (at the end of Basin interface) reflection. The bedrocks of the mess reflection exist under the seismic reflection layer of T5, and the sedimentary rocks or volcanic rocks exist on the seismic reflection layer of T5. The region is divided into two parts, bedrock raised areas (faulted strata missing regions) and the fault zones. In the raised areas, the bedrocks embed relative shallow, areas of ups and downs are large, has dome-shaped, the deep depression areas are smaller, mostly are residue faulted. In the faulted zones, the bedrocks embed relative deep, and the faulted are developed. The local structures on the reflective layer of T4 mainly reflect the local structural characteristics in the deep northern Songliao Basin. These local structures mainly developed and distributed in the late Jurassic-early Cretaceous faulted basins and the fringe regions around the faulted areas and the deep depressions. The reflective layer of T4 is sporadic distribution on the whole, almost distribute the whole region, but there are relatively concentrated developed areas. The distribution of the partial structures is basically NW and NE-NNE directions, but the former is more.
The generation mechanisms of Songliao Basin are discussed further, the former researches are emphasis that the united functions of the Western Asia Ocean and West Pacific tectonic domain on the Songliao Basin, but through the research of this area, we find that Mongolia-Okhotsk tectonic domain has a very important function on the research of growing mechanism in the Songliao Basin in addition to the above two tectonic domains. The geological and paleomagnetic data indicated that the ancient Okhotsk ocean consisting of the northern part of Heilongjiang and the eastern part of Mongolia closed from west to east since Permian, and in the eastern part completed closure in the Early Cretaceous. The closure of the ocean had a considerable impact on the tectonic evolution of the Northern and Northeastern China located on it’s southeast area.
Compared with the single small-scale and isolated research, through the integrated and united interpretation on the research area, we can gained the more comprehensive research results. We use two seismic profiles and Vp distribution characteristics to analyze regional tectonic characteristics and evolution rules on the northern and eastern areas of North Harbin. Through the integrated and united interpretation on the research area, we found that there were two groups of inverse faults roughly distributed in NE direction in the northern and eastern areas of North Harbin, which broke through several layers, the groups of reverse faults often formed the local anticlinal structures, and might be beneficial hydrocarbon accumulation belts. Integrated the previous research work, we did the further research on deep faulted geological structure and evolution, the bedrock conditions and the forming dynamic background in the northern and eastern areas of North Harbin, the faulted of Lindian, Suihua and Beian had been considered the beneficial oil and gas accumulation zones.
The precision is not enough through the two above profiles describing the features of sedimentary layers in Songliao Basin, but it has a certain credibility on qualitative account of the deep-seated shapes. The local deep study had been processed in Songliao Basin, and there also had some scholars predicting the deep oil and gas prospects in Songliao Basin. In contrast, using two long profiles from a regional point to analyze distributions of the deep stratum and discuss the relationship of oil and gas, it obviously has a more comprehensive understanding. Several major faulted in Songliao Basin almost exist the performance of faulted“concave”or“ancient basins”, and in larger scale. Integrating these conditions, good hydrocarbon prospects had been considered in the deep layers of Songliao Basin. Intensifying the deep oil and gas exploration work has been considered to be necessary. Despite Vp distributed profiles had large approximation (that is, tectonic map of T5 had different accuracy), but the performance of macroscopical consistent could be used as a kind of evidences for deep depressions.
The evaluation of oil and gas prospects in the northern and eastern areas of North Harbin has different nature from the southern part of Songliao basin, the sedimentary layers of depression are shallow in the northern and eastern areas of North Harbin, the account of generating oil and gas is less, can not be compared with the north part of Songliao Basin, the depth of faulted in the northern and eastern areas of North Harbin is similar to the depth of depression in the north part of Songliao Basin. The above geological facts suggest that the faulted and the depression period can not be separated in the oil and gas exploration of the northern and eastern areas of North Harbin. We can affirm that gas exploration in the northern and eastern areas of North Harbin is the overall exploration and the faulted period is more important. The faulted sequence in the northern and eastern areas of North Harbin and the overlying depression sequence belong to two sequences forming by different period of basins, and we should treat differently. Based on the exploration actuality of Songliao Basin, the depression sequence should be looked for oil mainly, and the faulted sequence for gas mainly.“Concave in the apophysis”within the deep fault and the groups of inverse faults in the mid-shallow layers are the important areas of the gas in deep layers and the mid-shallow oil and gas exploration in the northern and eastern areas of North Harbin.
With the rapid development of science and technology in the world, there are evident progresses in the theories of the petroleum geology and geophysics, which promote oil and gas exploration in the field of exploration targets increasingly complex circumstances continuing to make new discoveries and breakthroughs and achieve great economic benefits. Songliao Basin is an important oil-producing area in China, the fruitful results in the oil and gas reserves has been achieved in the south of the Binzhou railway in the north of Songliao Basin, but the situation of the North Harbin area in the north of Songliao Basin is very different. The North Harbin area has been become an important area for exploration to succeed with the reduced oil and gas resources in the old exploration regions. Because of its especial tectonic location and rich oil and gas resources, the Songliao Basin has become one of the areas of the geological workers concerned, the much concern is on the South Harbin area of Songliao Basin, but the concern on the North Harbin area is relatively less.
In the nearly 50 years of the exploration process on the North Harbin area, the pre-work is all isolated study in a small area, large area integrated explanation has not existed, and the exploration degree is also low. With the abundance of exploration data, the development of geological and geophysical theories and the exploration technology, which provide the necessary conditions for the geological conditions and distribution rule in the formation of deep oil and gas. To this point we selected the northern and eastern North Harbin area in-depth study as the breakthrough and provided reference of oil and gas exploration for deep stratum in the entire Songliao Basin and similar international basins.
Compared to single seismic research, we use a number of gravity and magnetic data to study the fault system in Songliao Basin, and provide a basis for further determining the distribution of fault system. There are decades of basement rifts in North Harbin area, which are important on the framework structure of top layer and oil and gas concentrating. Most faults are in NNE and NE direction.
The seismic reflection layer of T5 corresponds the faulted sequence at the bottom (at the end of Basin interface) reflection. The bedrocks of the mess reflection exist under the seismic reflection layer of T5, and the sedimentary rocks or volcanic rocks exist on the seismic reflection layer of T5. The region is divided into two parts, bedrock raised areas (faulted strata missing regions) and the fault zones. In the raised areas, the bedrocks embed relative shallow, areas of ups and downs are large, has dome-shaped, the deep depression areas are smaller, mostly are residue faulted. In the faulted zones, the bedrocks embed relative deep, and the faulted are developed. The local structures on the reflective layer of T4 mainly reflect the local structural characteristics in the deep northern Songliao Basin. These local structures mainly developed and distributed in the late Jurassic-early Cretaceous faulted basins and the fringe regions around the faulted areas and the deep depressions. The reflective layer of T4 is sporadic distribution on the whole, almost distribute the whole region, but there are relatively concentrated developed areas. The distribution of the partial structures is basically NW and NE-NNE directions, but the former is more.
The generation mechanisms of Songliao Basin are discussed further, the former researches are emphasis that the united functions of the Western Asia Ocean and West Pacific tectonic domain on the Songliao Basin, but through the research of this area, we find that Mongolia-Okhotsk tectonic domain has a very important function on the research of growing mechanism in the Songliao Basin in addition to the above two tectonic domains. The geological and paleomagnetic data indicated that the ancient Okhotsk ocean consisting of the northern part of Heilongjiang and the eastern part of Mongolia closed from west to east since Permian, and in the eastern part completed closure in the Early Cretaceous. The closure of the ocean had a considerable impact on the tectonic evolution of the Northern and Northeastern China located on it’s southeast area.
Compared with the single small-scale and isolated research, through the integrated and united interpretation on the research area, we can gained the more comprehensive research results. We use two seismic profiles and Vp distribution characteristics to analyze regional tectonic characteristics and evolution rules on the northern and eastern areas of North Harbin. Through the integrated and united interpretation on the research area, we found that there were two groups of inverse faults roughly distributed in NE direction in the northern and eastern areas of North Harbin, which broke through several layers, the groups of reverse faults often formed the local anticlinal structures, and might be beneficial hydrocarbon accumulation belts. Integrated the previous research work, we did the further research on deep faulted geological structure and evolution, the bedrock conditions and the forming dynamic background in the northern and eastern areas of North Harbin, the faulted of Lindian, Suihua and Beian had been considered the beneficial oil and gas accumulation zones.
The precision is not enough through the two above profiles describing the features of sedimentary layers in Songliao Basin, but it has a certain credibility on qualitative account of the deep-seated shapes. The local deep study had been processed in Songliao Basin, and there also had some scholars predicting the deep oil and gas prospects in Songliao Basin. In contrast, using two long profiles from a regional point to analyze distributions of the deep stratum and discuss the relationship of oil and gas, it obviously has a more comprehensive understanding. Several major faulted in Songliao Basin almost exist the performance of faulted“concave”or“ancient basins”, and in larger scale. Integrating these conditions, good hydrocarbon prospects had been considered in the deep layers of Songliao Basin. Intensifying the deep oil and gas exploration work has been considered to be necessary. Despite Vp distributed profiles had large approximation (that is, tectonic map of T5 had different accuracy), but the performance of macroscopical consistent could be used as a kind of evidences for deep depressions.
The evaluation of oil and gas prospects in the northern and eastern areas of North Harbin has different nature from the southern part of Songliao basin, the sedimentary layers of depression are shallow in the northern and eastern areas of North Harbin, the account of generating oil and gas is less, can not be compared with the north part of Songliao Basin, the depth of faulted in the northern and eastern areas of North Harbin is similar to the depth of depression in the north part of Songliao Basin. The above geological facts suggest that the faulted and the depression period can not be separated in the oil and gas exploration of the northern and eastern areas of North Harbin. We can affirm that gas exploration in the northern and eastern areas of North Harbin is the overall exploration and the faulted period is more important. The faulted sequence in the northern and eastern areas of North Harbin and the overlying depression sequence belong to two sequences forming by different period of basins, and we should treat differently. Based on the exploration actuality of Songliao Basin, the depression sequence should be looked for oil mainly, and the faulted sequence for gas mainly.“Concave in the apophysis”within the deep fault and the groups of inverse faults in the mid-shallow layers are the important areas of the gas in deep layers and the mid-shallow oil and gas exploration in the northern and eastern areas of North Harbin.
引文
[1] 迟元林, 云金表, 蒙启安等. 松辽盆地深部结构及成盆动力学与油气聚集. 石油工业出版社, 2002
[2] 张功成, 蔡希源, 周章宝等. 裂陷盆地分析原理和方法-以松辽盆地为例. 石油工业出版社, 1996
[3] 高瑞祺, 蔡希源. 松辽盆地油气田形成条件与分布规律石油工业出版社,1997. 石油工业出版社,1997
[4] 陈发景, 汪新文, 曹守连等. 中国中、新生代含油气盆地构造和动力学背景. 现代地质, 1992, 6(3):317-327
[5] 王璞珺, 程日辉, 王洪艳等. 松辽盆地滨北地区油气勘探方向探讨. 石油勘探与开发, 2006, 33(4): 426-431
[6] 王伟锋, 陆诗阔, 金强. 中国大陆东部盆地构造动力学分析. 石油大学学报(自然科学版), 1999, 23(4): 1-5
[7] 张恺, 罗志立, 张清等. 中国大陆板块的演化与含油气盆地特点的探讨. 石油勘探与开发, 1981, (1): 13-21
[8] 黄邦强,张朝文,金以钟等. 大地构造学基础及中国区域构造概要. 地质出版社,1984
[9] 万天丰. 中国东部中、新生代板内变形构造应力场及其应用. 地质出版社, 1993
[10] 任建业, 胡祥云, 张俊霞. 中国大陆东部晚中生代构造活化及其演化过程. 大地构造与成矿学, 1998, 22(2): 89-96
[11] 宋维海, 张兴洲, 王璞珺. 中国东部陆缘中区第三纪构造-火山事件及其对含油气盆地的控制. 吉林大学学报(地球科学版), 2003, 33(4): 479-484
[12] 孙哓猛, 王璞珺, 郝福江等. 中国东部陆缘中区中-新生代区域断裂系统时空分布特征、迁移规律及成因类型. 吉林大学学报(地球科学版), 2005, 35(5): 554-563
[13] 赵海玲, 邓晋福, 陈发景等. 中国东北地区中生代火山岩岩石学特征与盆地形成. 现代地质, 1998, 12(1): 56-61
[14] 王璞珺, 陈树民, 刘万洙等. 松辽盆地火山岩相与火山岩储层的关系. 石油与天然气地质, 2003, 24(1): 19-26
[15] 王鸿祯, 刘本培, 李思田. 中国及邻区大地构造划分和构造发展阶段, 见王鸿祯主编, 中国及邻区构造古地理和生物古地理. 中国地质大学出版社, 1990, 3-34
[16] Dou L R, Chang L. Fault linkage patterns and their control on the formation of the petroleum systems of the Erlian Basin, Eastern China. Marine and PetroleumGeology, 2003, 20: 1213-1224
[17] 王鸿祯, 杨森南, 李思田. 中国东部及邻区中、新生代盆地发育及大陆边缘区的构造发展. 地质学报, 1983, 57(3): 213-223
[18] 范小林, 殷勇. 中国大陆东部岩石圈深部地质结构与主要的中、新生代盆地. 江苏地质, 1994, 18(1): 10-18
[19] 朱夏, 陈焕疆. 中国中、新生代构造与含油气盆地. 地质学报, 1983, 57(3): 235-242
[20] 杨宝俊, 张梅生, 王璞珺等. 论中国东部大型盆地区及临区地质-地球物理复合尺度解析. 地球物理学进展, 2002, 17(2): 317-324
[21] 张一伟, 陈发景, 陆克政等. 中国含气(油)盆地的构造格架和成因类型. 中国科学(D 辑), 1996, 26(6): 493-498
[22] 马杏垣, 刘和甫, 王维襄等. 中国东部中、新生代裂陷作用和伸展构造. 地质学报, 1983, 57(10): 22-32
[23] Sorokin A A, Kotov A B, Sal’nikova Y B, et al. Rannepaleozoyskiye gabbro-granitoidnyye assotsiatsii vostochnogo segmenta Mongolo-Okhotskogo skladchatogo poyasa (Priamur'ye); vozrast i tektonicheskoye polozheniye. Early Paleozoic gabbro-granite associations in the eastern Mongolia-Okhotsk fold belt (Amur River basin); age and tectonics. Stratigrafiya, Geologicheskaya Korrelyatsiya, 2007, 15(3): 3-21
[24] 王璞珺, 迟元林, 刘万洙等. 松辽盆地火山岩相: 类型、特征和储层意义. 吉林大学学报(地球科学版), 2003, 33(4): 450-455
[25] 张岳桥, 赵越, 董树文等. 中国东部及邻区早白垩世裂陷盆地构造演化阶段. 地学前缘, 2004, 11(3): 123-132
[26] 张功成, 徐宏, 王同和等. 中国含油气盆地构造. 石油工业出版社, 1999
[27] 吕炳全, 张彦军, 王红罡等. 中国东部中、新生代火山岩油气藏的现状与展望. 海洋石油, 2003, 23(4): 9-11
[28] 汤加富, 高天山, 李怀坤. 中国东部中、新生代构造格局和岩浆岩带的形成与演化. 地质调查与研究, 2004, 27(2): 65-73
[29] Wang P J, Satir M, Siebel W, Chen F. Sr, Nd, Pb and O isotopes of the volcanic rocks in the Songliao basin (SB), NE China: constraint on tectonic setting. European Journal of Mineralogy, 2000(12): 228
[30] 孙加鹏, 张兴洲, 杨宝俊. 中国东部中、新生代盆地成因及其地球动力学. 世界地质, 1997, 16(3): 1-6
[31] 陈胜早. 中国及邻域的深部构造及其成矿意义. 地质学报, 1995, 69(1): 1-15
[32] 胡受奚, 赵乙英, 胡志宏等. 中国东部中-新生代活动大陆边缘构造-岩浆作用演化和发展. 岩石学报, 1994, 10(4): 370-379
[33] Dou L R. The lower cretaceous petroleum system in NE China. Journal of Petroleum Geology, 1997, 20(4): 475-488
[34] Enkin R J, Yang Z Y, Chen Y, et al. Paleomagnetic constraints on the geodynamic history of the major block of China from Permian to the present. Journal of Geophysical Research, 1992, 97(B10): 13953-13989
[35] 李锦轶. 中国东北及邻区若干地质构造问题的新认识. 地质论评, 1998, 44(4): 339-347
[36] 李思田, 杨士恭, 吴冲龙等. 中国东部及邻区新生代裂陷作用的大地构造背景, 见王鸿祯主编, 中国及邻区构造古地理和生物古地理. 地质出版社, 1990: 109-26
[37] Lee K Y. Petroleum geology of the Songliao Basin. Northeast China. USGS Open File Report, USA. 1986
[38] 陈发景, 赵海玲, 陈昭年等. 中国东部中、新生代伸展盆地构造特征及地球动力学背景. 地球科学, 1996, 21(4): 357-365
[39] 杨宝俊, 刘财, 刘万崧等. 中国东北地区岩石圈结构的地震学特征与对矿产资源的动力控制作用. 中国地质, 2006, 33(4): 866-873
[40] Wang P J, Sun X M, Mattern F. Relationship between Yanshanian orogeny and the evolution of Songliao basin (SB), North/Northeast China. (Abstract). European Journal of Mineralogy, 2000(12): 229
[41] Wang P J, Ren Y G, Shan X L, et al. The Cretaceous volcanic succession around the Songliao Basin, NE China: relationship between volcanism and sedimentation. Geological Journal, 2002, 37(2): 97-115
[42] Yang B J, Liu C, Hang L G., et al. A study for the base and the bottom of guantou formation of Lower Cretaceous system in songliao basin, China-using vertical reflection method, In: 30th International geological congress, Abstracts, Beijing, China, 1996, 3(3), 111
[43] 张恺. 板块构造与油气成因二元论. 石油工业出版社, 1997
[44] Yang B J, Liu C, Hou G B, et al. A study of detachment faults in upper basement of songliao basin near Daqing of China by using the vibroseis technique, In: Russian academy of sciences Siberian branch, Methods of study structure and monitoring of the Lithosphere (materials of the international conferences), Novosibirsk spc UIGGM SB RAS, 1998, 140-141
[45] Chen C. Non-marine setting of petroleum in the Songliao Basin of northeastern China. Journal of petroleum Geology, 1980, 2(3): 233-264
[46] Hu W S, Cai C F, Wu Z Y, et al. Structural style and its relation to hydrocarbonexploration in the Songliao Basin, northern China. Marine and Petroleum Geology, 1998, 15: 41-55
[47] 俞凯,侯洪斌,郭念发等. 松辽盆地南部断陷层系石油天然气地质. 石油工业出版社, 2002
[48] Zhang G F, Shen X H, Zou L J, et al. Detection of hydrocarbon bearing sand through remote sensing techniques in the western slope zone of Songliao basin, China. International Journal of Remote Sensing, 2007, 28(7-8): 1818-1833
[49] Graham S A, Hendrix M S, Badamgarav D. Sedimentary record and tectonic implication of Mesozoic rifing in southeast Mongolia. GSA Bulletin, 2001, 113(12): 1560-1579
[50] 罗群, 孙宏智. 松辽盆地深大断裂对天然气的控制作用. 天然气工业, 2000, 20(3): 16-21
[51] 杨宝俊, 张梅生, 王璞珺. 中国油气区地质地球物理解析(上卷). 科学出版社, 2003
[52] Kirillova G L. Late Mesozoic-Cenozoic sedimentary basins of active continental margin of Southeast Russia: paleogeography, tectonics, and coal-oil-gas presence. Marine and Petroleum Geology, 2003, 20: 385-397
[53] Klimetz M P. Speculations on the Mesozoic plate tectonic evolution of Eastern China. Tectonics, 1983, 2(2): 139-166
[54] 郭占谦, 萧德铭, 唐金生. 深大断裂在油气藏形成中的作用. 石油学报, 1996, 17(3): 27-32
[55] 鲁兵, 黎冰, 刘忠等. 松辽盆地滨北地区基底断裂及其对油气的控制作用. 大庆石油学院学报, 2000, 24(4): 8-11
[56] Wang P J, Ren Y G, Shan X L. The Cretaceous volcanic succession around the Songliao Basin, NE China: relationship between volcanism and sedimentation. Geological Journal, 2002, 37(2): 97-115
[57] Wu F Y, Sun D Y, Li H M, et al. The nature of basement beneath the Songliao Basin in NE China: geochemical and isotopic constraints. Phys. Chem. Earth(A), 2001, 26(9-10): 793-803
[58] 程三友. 中国东北地区区域构造特征与中、新生代盆地演化. 博士学位论文, 2006
[59] 王鸿祯, 杨森楠, 李思田. 中国东部及邻区中、新生代盆地发育及大陆边缘区的构造发展. 地质学报, 1983, (3): 213-222
[60] Xue L Q, Galloway W E. Genetic sequence stratigraphic framework, depositional style, and hydrocarbon occurrence of the upper Cretaceous QYN formations in theSongliao lacustrine Basin, northeastern China. The American Association of Petroleum Geology, 1993, 77(10): 1792-1808
[61] 李瑞磊. 松辽盆地(南部)深层构造特征及油气富集规律研究. 博士学位论文, 2005
[62] Zhou Y S, Littke R. Numerical simulation of the thermal maturation, oil generation and migration in the Songliao Basin, Northeastern China. Marine and Petroleum Geology, 1999, 16: 771-792
[63] Li D S, Jiang R Q, Barry J K. Petroleum generation in the nonmarine Qingshankou formation(lower Cretaceous), Songliao Basin, China. In barry Jay Katz, ed. Petroleum source rocks: New York, Springer-Verlag, 1995, 131-148
[64] 邱春光, 王璞珺. 试论盆地内火山岩地层发育的层序位置-以松辽盆地徐家围子断陷为例. 新疆石油天然气, 2006, 2(1): 13-17
[65] 王璞珺, 杜小弟, 王俊等. 松辽盆地白垩纪年代地层研究及地层时代划分. 地质学报, 1995, 69(4): 372-380
[66] 刘万洙, 王璞珺, 门广田等. 松辽盆地北部深层火山岩储层特征. 石油与天然气地质, 2003, 24(1): 28-31
[67] 程日辉, 朱德丰, 王洪艳等. 松辽盆地林甸断陷白垩纪沙河子期盆地次级构造单元与沉积体系. 吉林大学学报(地球科学版), 2006, 36(5): 793-798
[68] 宋维海, 王璞珺, 张兴洲等. 松辽盆地中生代火山岩油气藏特征. 石油与天然气地质, 2003, 24(1): 12-17
[69] Hawkes A D, Korton B P, Grand P C. A microfossil-based approach to constraining megathrust-induced coseismic land displacement in the pacific Northwest. Abstracts with Programs - Geological Society of America, 2007, 39(6): 158
[70] Xie X N, Jiao J J, Tang Z H, et al. Evolution of abnormally low pressure and its implications for the hydrocarbon system in the southeast uplift zone of Songliao Basin, China. AAPG Bulletin, 2003, 87(1): 99-119
[71] 胡金祥. 松辽盆地滨北断陷期构造单元划分及其都油气的控制. 硕士学位论文, 2004
[72] 杨宝俊, 刘财. 论松辽盆地基底的地球物理特征. 长春科技大学学报, 1999, 29(增刊): 13-19
[73] Engebretson D C, Cox A, Gordon R G. Relative motions between oceanic and continental plates in the Pacific basin. The Geological Society of America, Special Paper, 1985, 206: 1-59
[74] Yamamura M, Kawahata H, Matsumoto K, et al. Paleoceanography of the northwestern Pacific during the Albian. Palaeogeography, Palaeoclimatology,Palaeoecology, 2007, 254(3-4): 477-491
[75] 侯启军. 松辽盆地北部深层断陷地质结构及演化研究. 博士学位论文, 2006
[76] Zhang F Q, Song J S, Shen Z Y, et al. A study on fracture orientation and characteristic of remnant magnetization of deep-burial volcanic rocks, north of the Songliao Basin. Chinese Journal of Geophysics, 2007, 50(4): 1011-1017
[77] Guo F. Seismic facies and sedimentary facies of lower cretaceous in Northern Songliao basin. Petroleum Geology & Oilfield Development in Daqing, 2005, 24(6): 20-23
[78] 唐华风. 松辽盆地滨北地区构造样式与构造圈闭预测. 硕士学位论文, 2004
[79] Liu D L. Summarily analysis to multiple tectonic system in Songliao basin. Natural Gas Geoscience, 2005, 16(4): 433-436
[80] 胡望水, 王燮培. 松辽盆地北部变换构造及其石油地质意义. 1994, 15(2), 164-172
[81] Liu Q. Integrated description technique for deep volcanic gas reservoir in northern Songliao Basin. Petroleum Geology & Oilfield Development in Daqing, 2005, 24(3): 21-23
[82] Zhang W Q. Oil gas source and migration on West Slope of Songliao Basin. Petroleum Geology & Oilfield Development in Daqing, 2005, 24(1): 17-19
[83] Lu S F. Denudation thickness and its significance in the deep part of Songliao Basin. Petroleum Geology & Oilfield Development in Daqing, 2005, 24(1): 20-22
[84] Dou L R, Li J C. Structure style and petroleum systems of the Songliao Basin. In: Proceedings of the 30th international geological congress; Geology of fossil fuels; oil and gas. Proceeding of the International Geological Congress. 1997,30 (18): 33-42
[85] Hu W S, Liu B Q, Zhang W J, et al. An approach to tectonic evolution and dynamics of the Songliao Basin. Scientia Geologica Sinica, 2005, 40(1): 16-31
[86] 于平. 松辽盆地滨北地区构造特征与有利油气聚集条件的地震学研究. 博士论文, 2006
[87] Xiang C F, Feng Z Q, Wu H Y, et al. Discussion on the dynamic factors controlling hydrocarbon migration from depression to west slope zone of the Songliao Basin, Northeast China. Acta Sedimentologica Sinica, 2005, 23(4): 719-725
[88] Cloetingh S, Boldreel L O, Larsen R T, et al. Tectonics of sedimentary basin formation: models and constraints. Tectonophysics. 1998. 300: 1-11
[89] Davis G A, Wang C, ZhengY, et al. The enigmatic Yinshan fold-and-thrust belt of northerm China: new views on its intraplate contractional styles. Geology, 1998, 26: 43-46
[90] 陈佩良, 刘德秀. 重磁方法在综合物探中的应用. 成都理工学院学报, 1997, 24(3): 116-122
[91] 王家林. 对我国石油重磁勘探发展的几点思考. 勘探地球物理进展, 2006, 29(2): 82-86
[92] 侯惠群. 重磁勘探方法在石油勘探中的应用. 铀矿地质, 1995, 11(1): 59-64
[93] 王一新, 王家林, 万明浩等. 石油综合地球物理方法与应用. 石油工业出版社, 1995
[94] 管志宁. 我国磁法勘探的研究与进展. 地球物理学报, 1997, 40 卷增刊, 299-306
[95] 刘光鼎, 郝天珧, 刘伊克. 重磁研究对认识盆地的意义. 地球物理学进展, 1996, 11(2): 1-15
[96] 袁业培, 金文丽. 重磁资料在油气勘探中的作用. 物探与化探, 1994, 18(4): 309-316
[97] 钟慧智, 王家林, 陈冰. 综合物探方法在松辽盆地北部基底结构研究中的应用. 上海地质, 1995, 4: 33-40
[98] 王家林, 王一新, 万明浩等. 石油重磁解释. 石油工业出版社, 1991
[99] 何展翔. 非地震勘探技术的进步与发展趋势. 石油地球物理勘探, 2000, 35(3): 354-360
[100] 大庆石油管理局勘探开发研究院. 松辽盆地北部滨北地区侏罗系分布与基底结构研究. 大庆石油管理局勘探开发研究院内部资料, 1988
[101] 陈永峤, 周新桂, 于兴河等. 断层封闭性要素与封闭效应. 石油勘探与开发, 2003, 30(6): 38-40
[102] 朱德丰. 松辽盆地北部深断裂断层结构及其作用研究. 大庆研究院内部资料, 2003
[103] 杨宝俊, 穆石敏, 金旭等. 中国满洲里—绥芬河地学断面地球物理综合研究. 地球物理学报, 1996, 39(6): 772-782
[104] 郭巍, 刘招君, 董清水等. 断陷湖盆层序地层格架中的油气聚集规律—以松辽盆地为例. 吉林大学学报(地球科学版), 2002, 32(3): 233-237
[105] Yu P, Li R L, Fu L, et al. Regional tectonic characteristics and significance of north Harbin Area in Songliao Basin: evidenced from long seismic profiles. Journal of Jilin University (Earth Science Edition), 2005, 35(5): 611-615
[106] Harding T. P. Seismic Characteristics and Identification of Negative Flower Sructures, Positive Folwer Structures and Positive structural Inversion, AAPG, 1985, 63: 1016-1058
[107] Hill R H. Mantle plume and continental tectonics. Science, 1992, 256: 186-192
[108] Kimura G, Takahashi M, Konno M. Mesozoic collision-extrusion tecto- nics ineastern Asia. Tectonophysics, 1990, 181: 15-23
[109] Lister G S, Etheridge E A, Symonds P A. Detachment models for the formation of passive continental margins. Tectonics, 1991, 10: 1038-1064
[110] Maruyama S, Isozaki Y, Kimura G, et al. Pale-geographic maps of the Japanese islands: plate tectonic synthesis from 750Ma to the present. The Island Arc, 1997, 6(1): 121-142
[111] Mitra S. Geometry and kinematic evolution of inversion structures. AAPG Bull, 1993, 77(7): 1159-1191
[112] Mooney W D, Meissner R. Multi-genetic origin of crustal reflectivity: a review of seismic reflection profiling of the continental lower crust and Moho. In: Fountain D M, Arculus R, Kay R W, ed. Continental lower crust, Amstertam: Elsevier Science Publishers B V, 1992. 45-80
[113] 杨宝俊, 于平, 李瑞磊. 用地震长剖面研究华北盆地及邻区区域构造特征. 长春科技大学学报, 2001, 31(地质地球物理综合专辑Ⅳ): 126-131
[114] 杨宝俊. 在地学断面域内用地震学方法研究大陆地壳: 以中国满洲里-绥芬河地学断面为例. 地质出版社, 1999
[115] Nelson R. Rift-segment interaction and its relation to hydrocarbon exploration in continental rift system. AAPG Bull, 1992, 76(8): 1153-1169
[116] Tapponnier P., et al. Propagating extrusion tectonics in Asia: New insights from simple experiments with plasticine. Geology, 1992, 10: 611-616
[117] Thatcher W, Hill D. A simple model for the fault-generated morphology of slow-spreading mid-oceanic ridges. Journal of Geophysical Research, 1995, 100: 561-570
[118] Tucholke B, Lin J. A geological model for the structure of ridge segments in slow spreading oceanic crust. Journal of Geophysical Research, 1994, 99: 11937- 11958
[119] Uyeda S. The Japanese island arc and the subduction process. Episodes, 1991, 14(3): 190-198
[120] Wang H, Mo X. An outline of the tectonic evolution of China. Episodes, 1995, 18(1-2): 6-16
[121] Willett S, Beaumont C, Fullsack P. A mechanical model for the tectonics of doubly -vergent compressional orogens. Geology, 1993, 21: 371-374
[122] Xu J W. The Tancheng-Lujiang wrench fault systerm, JOHN WILEY and SONS, 1993, 45-60
[123] Yang B J, Liu C, Hang L, et al. A study of detachment faults of the upper crust in Manzhouli-Suifenhe GGT by the method of vertical seismic reflection. In Liu G, ed.Proceeding of 30th International Geological Congress, VSP, UTRECHT THE NETHELANDS, 1997, 20: 51-61
[124] Yang B J, Mu S M, Jin xu, et al. Comprehensive geology study in the Manzhouli- Suifenhe geoscience transect, China, Chinese Journal of Geophysics (ACTA GEOPHYSICA SINICA), Allerton Press, Inc, NEW YORK, 1997, 40(1): 27-40
[125] Yang B J, Liu C, Yang P H. The basic characteristics of Moho near Daxinganling gravity gradient zone of China and it’s geological interpretation, In: Russian academy of sciences branch, Methods of study structure and monitoring of the Lithosphere (materials of the international conferences), Novosibirsk spc UIGGM SB RAS, 1998, 406-409
[126] Yang B J, Liu C, Tang J R, et al. The basic characteristics of the structure of Anda-Fengle nearly vertical seismic reflection profile of CHINA, In: Consejo superior de Investigacienes Cientificas (CSIC) and University of Barcelona, 8th International symposium on deep seismic profiling of the continents and their margins, Barcelona, Spain, 1998, 134
[127] Yin A, Nie S. A Phanerozoic palinspastic reconstruction of China and its neighboring regions. In: Yin A, Harrison T M, eds. The tectonic evolution of Asia. Cambridge: Cambridge University Press, 1996: 442-485
[128] 刘洋. 中国东北地区地壳物性分布特征及其与大地构造关系. 博士论文, 2006
[129] Bigg G R, Clark C D, Hughes A L C. A last glacial ice sheet on the Pacific Russian coast and catastrophic change arising from coupled ice-volcanic interaction. Earth and Planetary Science Letters, 2008, 265(3-4): 559-570
[130] Sun W D, Ding X, Hu Y H, et al. The golden transformation of the Cretaceous plate subduction in the West Pacific. Earth and Planetary Science Letters, 2007, 262(3-4): 533-542
[131] Liu S F, Liu B P. Comparative study on the juxtaposition events of Jurassic terranes in the Northern circum-Pacific belt, in Lithospheric Plate Tectonics and Dynamics. Geological Pubishing House,1995
[132] Graham D W, Reid M R, Jordan B T, et al. Mantle source provinces beneath the pacific Northwest revealed by helium isotope variations in basaltic lavas. Abstracts with Programs - Geological Society of America, 2007, 39(6): 455
[133] Zhao X X, Antretter M, Riisager P, et al. Rock magnetic results from Ocean Drilling Program Leg 192; implications for Ontong Java Plateau emplacement and tectonics of the Pacific. Geological Society Special Publications, 2004, 229: 45-61
[134] Roland, Burgmann, David D. P. Slip distributions on faults: effects of stress gradients,inelastic deformation, heterogeneous host-rock stiffness, and fault interaction. Journal of Structural Geology, 1994, 16(12): 1675-1690
[135] Zorin Y A. Geodynamics of the western part of the Mongolia-Okhotsk collisional belt,Trans-Bsikal region(Russia)and Mongolia. Tectonophysics, 1999, 306: 33-56
[136] Feng F K. Circum-Tethys and circum-Pacific basins. Journal of Southeast Asian Earth Sciences, 1996, 13(3-5): 305-315
[137] Hyeong K, Kim J, Yoo C, et al. Controlling factors of seabed manganese nodule genesis in the Northeast Pacific manganese nodule belt. Abstracts with Programs - Geological Society of America, 2007, 39(6): 71
[138] Hawkes A D, Korton B P, Grand P C. A microfossil-based approach to constraining megathrust-induced coseismic land displacement in the pacific Northwest. Abstracts with Programs - Geological Society of America, 2007, 39(6): 158
[139] Hong C H, Yoon J H. A three-dimensional numerical simulation of Typhoon Holly in the northwestern Pacific Ocean. Journal of Geophysical Research, 2003, 108(c8): 18
[140] Konstantinovskaia E A. Arc-continent collision and subduction reversal in the Cenozoic evolution of the Northwest Pacific: an example from Kamchataka(NE Russia). Tectonophysics, 2001, 333: 75-94
[141] Hilde, T W C, Uyeda S, Kroenke L. Evolution of the western Pacific and its margin. Tectonophysics, 1977, 38(1-2): 145-165
[142] Davis G A, Darby B J, Zheng Y D, et al. Geometric and temporal evolution of an extensional detachment fault, Hohhot metamorphic core complex. Inner Mongo- lia, China. Geology, 2002, 30(11): 1003-1008
[143] Darby B J, Davis G A, Zheng Y D. Structural evolution of the southwestern Daqingshan, Yinshan belt, Inner Mongolia, China. Geological Society of America, Memoir, 2001, 194: 199-214
[144] Ozawa S, Suito H, Nishimura T, et al. Possibility of recovery of slip deficit rate between the North American plate and the Pacific plate off Sanriku, northeast Japan. American Geophysical Union, 2007, 34(20): 25-28
[145] 杜旭东, 薛林福, 邬光辉. 中国东部大陆内部中生代盆地分布特征与地球动力学背景探讨. 长春科技大学学报, 1999, 29(2): 138-143
[146] Halim N, Kravchinsky V, Gilder S, et al. A Palaeomagnetic study from the Mongol-Okhotsk region: rotated Early Cretaceous volcanics and remagnetized Mesozoic sediments. Earth and Planetary Science Letters, 1998, 159: 133-145
[147] Keller G R, Drenth B J, Okure M S. A regional geophysical overview of the geoswath: pacific Northwest to the Appalachians. Abstracts with Programs - Geological Societyof America, 2007, 38(6): 614
[148] Northrup C J, Royden L H, Burchfiel B C. Motion of the Pacific Plate relative to Eurasia and its potential relation to Cenozoic extension along the eastern margin of Eurasia. Geology(Boulder), 1995, 23(8): 719-722
[149] 李乃胜, 赵松龄, 鲍·瓦西里耶夫. 西北太平洋边缘海地质. 黑龙江教育出版社, 2000
[150] Obata H, Alibo D S, Nozaki Y. Dissolved aluminum, indium, and cerium in the Sea of Japan and the Sea of Okhotsk; comparison to the marginal seas of the western North Pacific. Journal of Geophysical Research, 2007, 112(c12): 12003
[151] Verzhbitsky E V, Kononov M V, Kotelkin V D. Plate tectonics of the northern part of the Pacific Ocean. Oceanology, 2007, 47(5): 705-717
[152] Natal’in B. History and modes of Mesozoic accretion in Southeastern Russia. The island Arc. 1993, 2: 15-34
[153] A K ровушкина 等. 鄂霍茨克海北部沉积盆地的结构. 海洋地质动态, 2004, 20(12): 26-27
[154] Cao C R, Cao L. Crust structures and sectonic evolution of Northeast China in Mesonzoic. Journaly Geoscience Res. NE Asia, 1999, 2(2): 166-171
[155] 李家彪, 高抒. 中国边缘海岩石层结构与动力过程. 海洋出版社, 2003
[156] Chen B, Zhao G C, Wilde S A. Subduction and collision-related granitoids from Southern Sonidzuoqi, Inner Mongolia: Isotopic ages and tectonic implications. Geol. Rev, 2001, 47(4): 361-367
[157] Chen B, Jahn B M, Wilde S, et al. Two contrasting Paleozoic magmatic belts in northern Inner Mongolia, China: Petrogenesis and tectonic implications. Tectonophysics, 2000, 328: 157-182
[158] Darby B J, Davis G A, Zheng Y. Structural evolution of the southwestern Daqing Shan tectonic evolution of central Asia: From continental assembly to intracontinental deformation: Boulder, Colorado. Geological Society of America Memoir, 2001, 194: 199-214
[159] Davis G A, Darby B J, Zheng Y, et al. Geometric and temporal evolution of an extensional detachment fault, Hohhot metamorphic core complex, Inner Mongolia, China. Geology, 2002, 30: 1003-1006
[160] Davis G A, Xu B, Zhang Y D, et al. Indosinian extension in the Solonker suture zone: The Sonid Zuoqi metamorphic core complex, Inner Mongolia. China. Earth Science Frontiers, 2004, 11(3): 135-144
[161] Davis G A, Zheng Y D, Wang C, et al. Mesozoic tectonic evolution of the Yanshanfold and thrust belt, with emphasis on Hebei and Liaoning provinces, northern China. In: Hendrix M S, Davis G A, eds. Paleozoic and Mesozoic tectonic evolution of central Asia: From continental assembly to intracontinental deformation: Boulder, Colorado. Geological Society of America Memoir, 2001, 194: 171-197
[162] Dickinson W R. Basin geodynamics. Basin Research, 1993, 5: 195-196
[163] Dobretsov N L, Buslov M M, Yu U. Fragments of oceanic islands in accretion-collision areas of Gorny Altai and Salair, southern Siberia, Russia, In early stages of continental crustal growth of the Siberian continent in Vendian-Early Cambrian time. Journal of Asian Earth Sciences, 2004, 23: 673-690
[164] 郝天珧, Yuri Neprochnov, 江为为. 鄂霍茨克海的地球物理场与地质构造. 地球物理学进展, 2001, 16(1): 1-10
[165] 莫申国, 韩美莲, 李锦轶. 蒙古-鄂霍茨克造山带的组成及造山过程. 山东科技大学学报(自然科学版). 2005, 24(3): 50-64
[166] Kravchinsky V A, Cogne J P, Harbert W P, et al. Evolution of the Mongol-Okhotsk Ocean as constrained by new palaeomagnetic data from the Mongol-Okhotsk suture zone, Siberia. Geophys. J. Int, 2002, 148: 34-57
[167] Liu X W, Meng X G, Tamaki K, et al. Palinspastic reconstruction for tectonics of northeast China and its vicinity. Journal of China University of Geoscience, 1998, 9(3): 206-216
[168] Shakirov R B, Obzhirov A I, Salyuk A N, et al. Classification of anomalous methane fields in the Sea of Okhotsk Polar Meteorology and Glaciology, 2005, 19: 50-66
[169] Meng Q, Hu J, Jin J, et al. Tectonics of the late Mesozoic wide extensional basin system in the China-Mongolia border region. Basin Research, 2003a, 15: 397-415
[170] Meng Q. What drove late Mesozoic extension of the northern China-Mongolia tract? Tectonophysics, 2003b, 369: 155-174
[171] Verzhbitsky E V, Kononov M V. Geodynamic evolution of the lithosphere of the Sea of Okhotsk region from geophysical data. Izvestiya - Russian Academy of Sciences. Physics of the Solid Earth, 2006, 42(6): 490-501
[172] Ren J Y, Tamaki K, Li S T, et al. Late Mesozoic and Cenozoic rifting and its dynamic setting in eastern China and adjacent areas. Tectonophysics, 2002, 344: 175-205
[173] Ren S M, Zhu R X, Huang B C, et al. Paleomagnetic study on orogenic belt: An example from Early Cretaceous volcanic rocks, Inner Mongolia. China, Science in China Ser. D Earth Sciences, 2004, 47(12): 1127-1133
[174] Ritts B D, Darby B J, Cope T. Early Jurassic extensional basin formation in the Daqing Shan segment of the Yinshan belt, northern North China Block, InnerMongolia. Tectonophysics, 2001, 339: 239-258
[175] Rowley D B. Age of initiation of collision between India and Asia: a review of stratigraphic data. Earth and Planetary Science Letters, 1996, 145: 1-13
[176] Schellart W P, Lister G S. The role of the East Asian active margin in widespread extensional and strike-slip deformation in East Asia. Journal of the Geological Society, 2005, 162: 959-972
[177] Sha J G, Matsukawa M, Cai H W, et al. The Upper Jurassic-Lower Cretaceous of eastern Heilongjiang, northeast China: stratigraphy and regional basin history. Ctetaceous Research, 2003, 24: 715-728
[178] K ровушкинаОА等. 鄂霍茨克海北部沉积盆地的构造演化. 海洋地质动态, 2005, 21(1): 137-39
[179] Kravchinsky V A, Sorokin A A, Courtillot V. Paleomagnetism of Paleozoic and Mesozoic sediments from southern margin of Mongol-Okhotsk Ocean, far eastern Russia. Journal of Geophysical Research, 2002, 107(B10): 22
[180] Halim N, Kravchinsky V, Gilder S, etal. A palaeomagnetic study from the Mongol-Okhotsk region; rotated Early Cretaceous volcanics and remagnetized Mesozoic sediments. Earth and Planetary Science Letters, 1998, 159(3-4): 133-145
[181] Tomurtogoo O, Windley B F, Kroener A, etal. Zircon age and occurrence of the Adaatsag Ophiolite and Muron shear zone, central Mongolia; constraints on the evolution of the Mongol-Okhotsk ocean, suture and orogen. Journal of the Geological Society of London, 2005, 162(1): 125-134
[182] Kirillova G L. Late Mesozoic-Cenozoic sedimentary basins of active continental margin of Southeast Russia; paleogeography, tectonics, and coal-oil-gas presence. Marine and Petroleum Geology, 2003, 20(3-4): 385-397
[183] Ren S M, Zhu R X, Huang B C, etal. Paleomagnetic study on orogenic belt; an example from Early Cretaceous volcanic rocks, Inner Mongolia, China. Science in China. Series D, Earth Sciences, 2004, 47(12): 1127-1133
[184] Zhu B Q, Chang X Y, Qiu H N, etal. racteristics of Proterozoic basements on the geochemical steep zones in the continent of China and their implications for setting of superlarge deposits. Science in China. Series D, Earth Sciences, 1998, 41 卷增刊: 54-64
[185] Shang Q H. Occurrences of Permian radiolarians in central and eastern Nei Mongol(Inner Mongolia)and their geological significance to the northern China orogen. Chinese Science Bulletin, 2004, 49(24): 2613-2619
[186] Shao J, Liu F, Chen H, et al. Deep geological process and its shallow response duringMesozoic transfer of tectonic framework in eastern North China. Geol. Rev, 2000, 46: 32-40
[187] Tomurtogoo O, Windley B F, Kroner O, et al. Zircon age and occurence of the Adaatsag ophiolite and Muron shear zone, central Mongolia: constraints on the evolution of the Mongol-Okhotsk Ocean, suture and orogen. Journal of the Geological Society, 2005, 162: 125-134
[188] Wang H Z, Mo X X. An outline of the tectonic evolution of China: Episodes, 1995, 18: 6-16
[189] Lelikov E P, Emel’yanova T A. Volcanogenic complexes of the Sea of Okhotsk and the Sea of Japan (comparative analysis). Oceanology, 2007, 47(2): 273-281
[190] Wu F, Lin J, Wilde S A, et al. Nature and significance of the early Cretaceous gian igneous event in eastern China. Earth and Planetary Science Letters, 2005, 233: 103-119
[191] Xiao W J, Windley B F, Hao J, et al. Accretion leading to collision and the Permaian Solonker suture, Inner Mongolia, China: termination of the central Asian orogenic belt. Tectonics, 2003, 22(6): 1-20
[192] Xu X, Harbert W, Dril S, et al. New paleomagnetic data from the Mongol-Okhotsk collision zone, Chita region, south-central Russia: implication for Paleozoic paleogeography of the Mongol-Okhotsk Ocean. Tectonophysics, 1997, 269: 113-129
[193] Yarmolyuk V V, Kovalenko V I. The Mesozoic-Cenozoic of Mongolia. In: Tectonics, Magmatism and Metallogeny of Mongolia(Ed.by A.B.Dergunov), Taylor and Francis Group, 2001, 203-244
[194] Zheng Y D, Zhang Q, Wang Y, et al. Great Jurassic thrust sheets in Beishan(North Mountains)-Gobi areas of China and southern Mongolia. Journal of Structural Geology, 1996, 18(9): 1111-1126
[195] Zhu R X, Yang Z Y, Wu H N, et al. Paleomagnetic constraints on the tectonic history of the major blocks of China during the Phanerozoic. Science in China(Series D), 1998, 41: 1-19
[196] Tamura T, Nanayama F, Saito Y, et al. Intra-shoreface erosion in response to rapid sea-level fall; depositional record of a tectonically uplifted strand plain, Pacific coast of Japan. Sedimentology, 2007, 54(5): 1149-1162
[197] Kirillova G L. The Late Mesozoic-Cenozoic sedimentary basins at the continental margin of southeastern Russia; geodynamic evolution and coal and petroleum potential. Geotectonics, 2005, 39(5): 389-407
[198] Kelty T K, Yin A, Dash B, et al. Detrital-zircon geochronology of the Hangay-HenteyBasin; implications for the tectonics of the Mongol-Okhotsk Ocean, Mongolia. Abstracts with Programs - Geological Society of America, 2005, 37(7): 56
[199] 蒋志勇, 臧绍先, 周元泽. 鄂霍茨克海下间断面的起伏及俯冲带的穿透. 科学通报, 2003, 48(4): 320-327
[200] Galanin A A, Glushakova O Y. Oledeneniya, klimat i rastitel'nost' rayona Tauyskoy guby, Severnoye Priokhot'e, v pozdnechetvertichnoye vremya. Late Quaternary glaciation, climate and flora in the Tauy estuary, northern Okhotsk region. Geomorfologiya, 2006, 2: 50-62
[201] Kuz’min V K, Glebovitsky V A, Matukov D I, et al. The oldest basic granulites of Northeast Russia (Okhotsk Terrane). Doklady Earth Sciences, 2005, 402(4): 506-510
[202] Yuri Neprochnov, Hao T Y. Geophysical field and geological structure in Okhotsk Sea (in Russian). Journal of ocean geology, 1999, 39(4): 622-627
[203] Zonenshain L P, Lisitsin A P, Kuzmin M I, etal. Tectonics and hydrothermal activity in the TAG area (central Atlantic) according to MIR submersible dives. Eos, Transactions, American Geophysical Union, 1990, 71(43): 1577
[204] 吕延防, 孙永河, 付晓飞等. 逆断层中天然气运移特征的物理模拟. 地质科学, 2005, 40(4): 464-475
[205] 付立新, 王东林, 肖玉永. 伸展断层作用对油气二次运移的影响. 石油大学学报(自然科学版), 2000, 24(4): 71-74
[206] 邹华耀, 金燕, 黄光辉. 断层封闭与油气运移和聚集. 江汉石油学院学报, 1999, 21(1): 9-17
[207] 侯康明, 闻学泽. 板内逆断层地震破裂的基本特征及分段标志研究. 西北地震学报, 1999, 21(3): 302-309
[208] 陆绍俊. 深部逆断层对地震响应的影响研究. 河海大学学报, 1998, 26(6): 51-56
[209] 丁文龙, 金之钧, 丁艳红. 逆断层和聚敛型扭断层下盘圈闭条件分析及勘探意义. 江汉石油学院学报, 2003, 25(1): 30-31
[210] Yin A, Nie S Y. A Phanerozoic palinspastic reconstruction of China and its neighboring regions, in Yin A, and Harrison T M, eds. The tectonic evolution of Asia. Cambridge University Press, 1996, 442-485
[211] Yin A, Nie S Y. An indentation model for North and South China collision and the development of the TanLu and Honam fault systems, eastern Asia. Tectonics, 1993, 12: 801-813
[212] Zhang Y Q, Ma Y S, Yang N, et al. Cenozoic extensional stress evolution in North China. Journal of Geodynamics, 2003, 36: 591-613
[213] Zhang X D. Formation, evolution and earth dynamics of Jurassic and Cretaceousbasins in northern China. Petroleum Geology & Oilfield Development in Daqing, 2005, 24(5): 6-8
[214] Zhang Z, Yang L, Yu S, et al. Mirror image symmetry between sedimentary basin and consolidated crust in China. Geophysical Research Abstract, S2. 06, Volume 4. EGS, Nice, France, 2002
[215] Zhao W J, Nelson K K. Deep seismic reflection evidence for continental underthrusting beneath south Tibet. Nature, 1993, 366: 557-559
[216] 胡艳飞, 于平, 孔庆莹, 王世煜. 松辽盆地北安地区断陷期构造特征的地震学证据及其油气意义. 地球物理学进展, 2007, 22(5): 1455-1459
[217] Gawthorpe R L, Sharp L. Linked sequence stratigraphic and structural evolution of propagating normal faults. Geology, 1997, 25(9): 795-798
[218] Gupta S, Cowie P. A. A mechanism to explain rift-basin subsidence and stratigraphic patterns through fault-array evolution. Geology, 1998, 26(7): 595-598
[219] Kusznir N J, Ziegler M. The mechanics of continental extension and sedimentary basin formation: A simple-shear/pure-shear flexural cantilever model. Tectonophysics, 1992, 215: 117-131
[220] Malavieille J. Late orogenic extension in mountain belts: Insights from the basin and range province and the late Paleozoic variscan belt. Tectonics, 1993, 12(5): 1115-1130
[221] Patience A C, Christopher H S. Physical explanation for the displacement-length relationship of faults using a post-yield fracture mechanics model. Journal of Structual Geology, 1992, 14(10): 1133-1148
[222] Peacock D C P, Sanderson D J. Displacements, segment linkage and relay ramps in normal fault zones. Journal of Structural Geology, 1991, 13(6): 721-733
[223] Blundell D J. Some observations on basin evolution and dynamics. Journal of the Geological Society, 1991, 148: 789-800
[2] 张功成, 蔡希源, 周章宝等. 裂陷盆地分析原理和方法-以松辽盆地为例. 石油工业出版社, 1996
[3] 高瑞祺, 蔡希源. 松辽盆地油气田形成条件与分布规律石油工业出版社,1997. 石油工业出版社,1997
[4] 陈发景, 汪新文, 曹守连等. 中国中、新生代含油气盆地构造和动力学背景. 现代地质, 1992, 6(3):317-327
[5] 王璞珺, 程日辉, 王洪艳等. 松辽盆地滨北地区油气勘探方向探讨. 石油勘探与开发, 2006, 33(4): 426-431
[6] 王伟锋, 陆诗阔, 金强. 中国大陆东部盆地构造动力学分析. 石油大学学报(自然科学版), 1999, 23(4): 1-5
[7] 张恺, 罗志立, 张清等. 中国大陆板块的演化与含油气盆地特点的探讨. 石油勘探与开发, 1981, (1): 13-21
[8] 黄邦强,张朝文,金以钟等. 大地构造学基础及中国区域构造概要. 地质出版社,1984
[9] 万天丰. 中国东部中、新生代板内变形构造应力场及其应用. 地质出版社, 1993
[10] 任建业, 胡祥云, 张俊霞. 中国大陆东部晚中生代构造活化及其演化过程. 大地构造与成矿学, 1998, 22(2): 89-96
[11] 宋维海, 张兴洲, 王璞珺. 中国东部陆缘中区第三纪构造-火山事件及其对含油气盆地的控制. 吉林大学学报(地球科学版), 2003, 33(4): 479-484
[12] 孙哓猛, 王璞珺, 郝福江等. 中国东部陆缘中区中-新生代区域断裂系统时空分布特征、迁移规律及成因类型. 吉林大学学报(地球科学版), 2005, 35(5): 554-563
[13] 赵海玲, 邓晋福, 陈发景等. 中国东北地区中生代火山岩岩石学特征与盆地形成. 现代地质, 1998, 12(1): 56-61
[14] 王璞珺, 陈树民, 刘万洙等. 松辽盆地火山岩相与火山岩储层的关系. 石油与天然气地质, 2003, 24(1): 19-26
[15] 王鸿祯, 刘本培, 李思田. 中国及邻区大地构造划分和构造发展阶段, 见王鸿祯主编, 中国及邻区构造古地理和生物古地理. 中国地质大学出版社, 1990, 3-34
[16] Dou L R, Chang L. Fault linkage patterns and their control on the formation of the petroleum systems of the Erlian Basin, Eastern China. Marine and PetroleumGeology, 2003, 20: 1213-1224
[17] 王鸿祯, 杨森南, 李思田. 中国东部及邻区中、新生代盆地发育及大陆边缘区的构造发展. 地质学报, 1983, 57(3): 213-223
[18] 范小林, 殷勇. 中国大陆东部岩石圈深部地质结构与主要的中、新生代盆地. 江苏地质, 1994, 18(1): 10-18
[19] 朱夏, 陈焕疆. 中国中、新生代构造与含油气盆地. 地质学报, 1983, 57(3): 235-242
[20] 杨宝俊, 张梅生, 王璞珺等. 论中国东部大型盆地区及临区地质-地球物理复合尺度解析. 地球物理学进展, 2002, 17(2): 317-324
[21] 张一伟, 陈发景, 陆克政等. 中国含气(油)盆地的构造格架和成因类型. 中国科学(D 辑), 1996, 26(6): 493-498
[22] 马杏垣, 刘和甫, 王维襄等. 中国东部中、新生代裂陷作用和伸展构造. 地质学报, 1983, 57(10): 22-32
[23] Sorokin A A, Kotov A B, Sal’nikova Y B, et al. Rannepaleozoyskiye gabbro-granitoidnyye assotsiatsii vostochnogo segmenta Mongolo-Okhotskogo skladchatogo poyasa (Priamur'ye); vozrast i tektonicheskoye polozheniye. Early Paleozoic gabbro-granite associations in the eastern Mongolia-Okhotsk fold belt (Amur River basin); age and tectonics. Stratigrafiya, Geologicheskaya Korrelyatsiya, 2007, 15(3): 3-21
[24] 王璞珺, 迟元林, 刘万洙等. 松辽盆地火山岩相: 类型、特征和储层意义. 吉林大学学报(地球科学版), 2003, 33(4): 450-455
[25] 张岳桥, 赵越, 董树文等. 中国东部及邻区早白垩世裂陷盆地构造演化阶段. 地学前缘, 2004, 11(3): 123-132
[26] 张功成, 徐宏, 王同和等. 中国含油气盆地构造. 石油工业出版社, 1999
[27] 吕炳全, 张彦军, 王红罡等. 中国东部中、新生代火山岩油气藏的现状与展望. 海洋石油, 2003, 23(4): 9-11
[28] 汤加富, 高天山, 李怀坤. 中国东部中、新生代构造格局和岩浆岩带的形成与演化. 地质调查与研究, 2004, 27(2): 65-73
[29] Wang P J, Satir M, Siebel W, Chen F. Sr, Nd, Pb and O isotopes of the volcanic rocks in the Songliao basin (SB), NE China: constraint on tectonic setting. European Journal of Mineralogy, 2000(12): 228
[30] 孙加鹏, 张兴洲, 杨宝俊. 中国东部中、新生代盆地成因及其地球动力学. 世界地质, 1997, 16(3): 1-6
[31] 陈胜早. 中国及邻域的深部构造及其成矿意义. 地质学报, 1995, 69(1): 1-15
[32] 胡受奚, 赵乙英, 胡志宏等. 中国东部中-新生代活动大陆边缘构造-岩浆作用演化和发展. 岩石学报, 1994, 10(4): 370-379
[33] Dou L R. The lower cretaceous petroleum system in NE China. Journal of Petroleum Geology, 1997, 20(4): 475-488
[34] Enkin R J, Yang Z Y, Chen Y, et al. Paleomagnetic constraints on the geodynamic history of the major block of China from Permian to the present. Journal of Geophysical Research, 1992, 97(B10): 13953-13989
[35] 李锦轶. 中国东北及邻区若干地质构造问题的新认识. 地质论评, 1998, 44(4): 339-347
[36] 李思田, 杨士恭, 吴冲龙等. 中国东部及邻区新生代裂陷作用的大地构造背景, 见王鸿祯主编, 中国及邻区构造古地理和生物古地理. 地质出版社, 1990: 109-26
[37] Lee K Y. Petroleum geology of the Songliao Basin. Northeast China. USGS Open File Report, USA. 1986
[38] 陈发景, 赵海玲, 陈昭年等. 中国东部中、新生代伸展盆地构造特征及地球动力学背景. 地球科学, 1996, 21(4): 357-365
[39] 杨宝俊, 刘财, 刘万崧等. 中国东北地区岩石圈结构的地震学特征与对矿产资源的动力控制作用. 中国地质, 2006, 33(4): 866-873
[40] Wang P J, Sun X M, Mattern F. Relationship between Yanshanian orogeny and the evolution of Songliao basin (SB), North/Northeast China. (Abstract). European Journal of Mineralogy, 2000(12): 229
[41] Wang P J, Ren Y G, Shan X L, et al. The Cretaceous volcanic succession around the Songliao Basin, NE China: relationship between volcanism and sedimentation. Geological Journal, 2002, 37(2): 97-115
[42] Yang B J, Liu C, Hang L G., et al. A study for the base and the bottom of guantou formation of Lower Cretaceous system in songliao basin, China-using vertical reflection method, In: 30th International geological congress, Abstracts, Beijing, China, 1996, 3(3), 111
[43] 张恺. 板块构造与油气成因二元论. 石油工业出版社, 1997
[44] Yang B J, Liu C, Hou G B, et al. A study of detachment faults in upper basement of songliao basin near Daqing of China by using the vibroseis technique, In: Russian academy of sciences Siberian branch, Methods of study structure and monitoring of the Lithosphere (materials of the international conferences), Novosibirsk spc UIGGM SB RAS, 1998, 140-141
[45] Chen C. Non-marine setting of petroleum in the Songliao Basin of northeastern China. Journal of petroleum Geology, 1980, 2(3): 233-264
[46] Hu W S, Cai C F, Wu Z Y, et al. Structural style and its relation to hydrocarbonexploration in the Songliao Basin, northern China. Marine and Petroleum Geology, 1998, 15: 41-55
[47] 俞凯,侯洪斌,郭念发等. 松辽盆地南部断陷层系石油天然气地质. 石油工业出版社, 2002
[48] Zhang G F, Shen X H, Zou L J, et al. Detection of hydrocarbon bearing sand through remote sensing techniques in the western slope zone of Songliao basin, China. International Journal of Remote Sensing, 2007, 28(7-8): 1818-1833
[49] Graham S A, Hendrix M S, Badamgarav D. Sedimentary record and tectonic implication of Mesozoic rifing in southeast Mongolia. GSA Bulletin, 2001, 113(12): 1560-1579
[50] 罗群, 孙宏智. 松辽盆地深大断裂对天然气的控制作用. 天然气工业, 2000, 20(3): 16-21
[51] 杨宝俊, 张梅生, 王璞珺. 中国油气区地质地球物理解析(上卷). 科学出版社, 2003
[52] Kirillova G L. Late Mesozoic-Cenozoic sedimentary basins of active continental margin of Southeast Russia: paleogeography, tectonics, and coal-oil-gas presence. Marine and Petroleum Geology, 2003, 20: 385-397
[53] Klimetz M P. Speculations on the Mesozoic plate tectonic evolution of Eastern China. Tectonics, 1983, 2(2): 139-166
[54] 郭占谦, 萧德铭, 唐金生. 深大断裂在油气藏形成中的作用. 石油学报, 1996, 17(3): 27-32
[55] 鲁兵, 黎冰, 刘忠等. 松辽盆地滨北地区基底断裂及其对油气的控制作用. 大庆石油学院学报, 2000, 24(4): 8-11
[56] Wang P J, Ren Y G, Shan X L. The Cretaceous volcanic succession around the Songliao Basin, NE China: relationship between volcanism and sedimentation. Geological Journal, 2002, 37(2): 97-115
[57] Wu F Y, Sun D Y, Li H M, et al. The nature of basement beneath the Songliao Basin in NE China: geochemical and isotopic constraints. Phys. Chem. Earth(A), 2001, 26(9-10): 793-803
[58] 程三友. 中国东北地区区域构造特征与中、新生代盆地演化. 博士学位论文, 2006
[59] 王鸿祯, 杨森楠, 李思田. 中国东部及邻区中、新生代盆地发育及大陆边缘区的构造发展. 地质学报, 1983, (3): 213-222
[60] Xue L Q, Galloway W E. Genetic sequence stratigraphic framework, depositional style, and hydrocarbon occurrence of the upper Cretaceous QYN formations in theSongliao lacustrine Basin, northeastern China. The American Association of Petroleum Geology, 1993, 77(10): 1792-1808
[61] 李瑞磊. 松辽盆地(南部)深层构造特征及油气富集规律研究. 博士学位论文, 2005
[62] Zhou Y S, Littke R. Numerical simulation of the thermal maturation, oil generation and migration in the Songliao Basin, Northeastern China. Marine and Petroleum Geology, 1999, 16: 771-792
[63] Li D S, Jiang R Q, Barry J K. Petroleum generation in the nonmarine Qingshankou formation(lower Cretaceous), Songliao Basin, China. In barry Jay Katz, ed. Petroleum source rocks: New York, Springer-Verlag, 1995, 131-148
[64] 邱春光, 王璞珺. 试论盆地内火山岩地层发育的层序位置-以松辽盆地徐家围子断陷为例. 新疆石油天然气, 2006, 2(1): 13-17
[65] 王璞珺, 杜小弟, 王俊等. 松辽盆地白垩纪年代地层研究及地层时代划分. 地质学报, 1995, 69(4): 372-380
[66] 刘万洙, 王璞珺, 门广田等. 松辽盆地北部深层火山岩储层特征. 石油与天然气地质, 2003, 24(1): 28-31
[67] 程日辉, 朱德丰, 王洪艳等. 松辽盆地林甸断陷白垩纪沙河子期盆地次级构造单元与沉积体系. 吉林大学学报(地球科学版), 2006, 36(5): 793-798
[68] 宋维海, 王璞珺, 张兴洲等. 松辽盆地中生代火山岩油气藏特征. 石油与天然气地质, 2003, 24(1): 12-17
[69] Hawkes A D, Korton B P, Grand P C. A microfossil-based approach to constraining megathrust-induced coseismic land displacement in the pacific Northwest. Abstracts with Programs - Geological Society of America, 2007, 39(6): 158
[70] Xie X N, Jiao J J, Tang Z H, et al. Evolution of abnormally low pressure and its implications for the hydrocarbon system in the southeast uplift zone of Songliao Basin, China. AAPG Bulletin, 2003, 87(1): 99-119
[71] 胡金祥. 松辽盆地滨北断陷期构造单元划分及其都油气的控制. 硕士学位论文, 2004
[72] 杨宝俊, 刘财. 论松辽盆地基底的地球物理特征. 长春科技大学学报, 1999, 29(增刊): 13-19
[73] Engebretson D C, Cox A, Gordon R G. Relative motions between oceanic and continental plates in the Pacific basin. The Geological Society of America, Special Paper, 1985, 206: 1-59
[74] Yamamura M, Kawahata H, Matsumoto K, et al. Paleoceanography of the northwestern Pacific during the Albian. Palaeogeography, Palaeoclimatology,Palaeoecology, 2007, 254(3-4): 477-491
[75] 侯启军. 松辽盆地北部深层断陷地质结构及演化研究. 博士学位论文, 2006
[76] Zhang F Q, Song J S, Shen Z Y, et al. A study on fracture orientation and characteristic of remnant magnetization of deep-burial volcanic rocks, north of the Songliao Basin. Chinese Journal of Geophysics, 2007, 50(4): 1011-1017
[77] Guo F. Seismic facies and sedimentary facies of lower cretaceous in Northern Songliao basin. Petroleum Geology & Oilfield Development in Daqing, 2005, 24(6): 20-23
[78] 唐华风. 松辽盆地滨北地区构造样式与构造圈闭预测. 硕士学位论文, 2004
[79] Liu D L. Summarily analysis to multiple tectonic system in Songliao basin. Natural Gas Geoscience, 2005, 16(4): 433-436
[80] 胡望水, 王燮培. 松辽盆地北部变换构造及其石油地质意义. 1994, 15(2), 164-172
[81] Liu Q. Integrated description technique for deep volcanic gas reservoir in northern Songliao Basin. Petroleum Geology & Oilfield Development in Daqing, 2005, 24(3): 21-23
[82] Zhang W Q. Oil gas source and migration on West Slope of Songliao Basin. Petroleum Geology & Oilfield Development in Daqing, 2005, 24(1): 17-19
[83] Lu S F. Denudation thickness and its significance in the deep part of Songliao Basin. Petroleum Geology & Oilfield Development in Daqing, 2005, 24(1): 20-22
[84] Dou L R, Li J C. Structure style and petroleum systems of the Songliao Basin. In: Proceedings of the 30th international geological congress; Geology of fossil fuels; oil and gas. Proceeding of the International Geological Congress. 1997,30 (18): 33-42
[85] Hu W S, Liu B Q, Zhang W J, et al. An approach to tectonic evolution and dynamics of the Songliao Basin. Scientia Geologica Sinica, 2005, 40(1): 16-31
[86] 于平. 松辽盆地滨北地区构造特征与有利油气聚集条件的地震学研究. 博士论文, 2006
[87] Xiang C F, Feng Z Q, Wu H Y, et al. Discussion on the dynamic factors controlling hydrocarbon migration from depression to west slope zone of the Songliao Basin, Northeast China. Acta Sedimentologica Sinica, 2005, 23(4): 719-725
[88] Cloetingh S, Boldreel L O, Larsen R T, et al. Tectonics of sedimentary basin formation: models and constraints. Tectonophysics. 1998. 300: 1-11
[89] Davis G A, Wang C, ZhengY, et al. The enigmatic Yinshan fold-and-thrust belt of northerm China: new views on its intraplate contractional styles. Geology, 1998, 26: 43-46
[90] 陈佩良, 刘德秀. 重磁方法在综合物探中的应用. 成都理工学院学报, 1997, 24(3): 116-122
[91] 王家林. 对我国石油重磁勘探发展的几点思考. 勘探地球物理进展, 2006, 29(2): 82-86
[92] 侯惠群. 重磁勘探方法在石油勘探中的应用. 铀矿地质, 1995, 11(1): 59-64
[93] 王一新, 王家林, 万明浩等. 石油综合地球物理方法与应用. 石油工业出版社, 1995
[94] 管志宁. 我国磁法勘探的研究与进展. 地球物理学报, 1997, 40 卷增刊, 299-306
[95] 刘光鼎, 郝天珧, 刘伊克. 重磁研究对认识盆地的意义. 地球物理学进展, 1996, 11(2): 1-15
[96] 袁业培, 金文丽. 重磁资料在油气勘探中的作用. 物探与化探, 1994, 18(4): 309-316
[97] 钟慧智, 王家林, 陈冰. 综合物探方法在松辽盆地北部基底结构研究中的应用. 上海地质, 1995, 4: 33-40
[98] 王家林, 王一新, 万明浩等. 石油重磁解释. 石油工业出版社, 1991
[99] 何展翔. 非地震勘探技术的进步与发展趋势. 石油地球物理勘探, 2000, 35(3): 354-360
[100] 大庆石油管理局勘探开发研究院. 松辽盆地北部滨北地区侏罗系分布与基底结构研究. 大庆石油管理局勘探开发研究院内部资料, 1988
[101] 陈永峤, 周新桂, 于兴河等. 断层封闭性要素与封闭效应. 石油勘探与开发, 2003, 30(6): 38-40
[102] 朱德丰. 松辽盆地北部深断裂断层结构及其作用研究. 大庆研究院内部资料, 2003
[103] 杨宝俊, 穆石敏, 金旭等. 中国满洲里—绥芬河地学断面地球物理综合研究. 地球物理学报, 1996, 39(6): 772-782
[104] 郭巍, 刘招君, 董清水等. 断陷湖盆层序地层格架中的油气聚集规律—以松辽盆地为例. 吉林大学学报(地球科学版), 2002, 32(3): 233-237
[105] Yu P, Li R L, Fu L, et al. Regional tectonic characteristics and significance of north Harbin Area in Songliao Basin: evidenced from long seismic profiles. Journal of Jilin University (Earth Science Edition), 2005, 35(5): 611-615
[106] Harding T. P. Seismic Characteristics and Identification of Negative Flower Sructures, Positive Folwer Structures and Positive structural Inversion, AAPG, 1985, 63: 1016-1058
[107] Hill R H. Mantle plume and continental tectonics. Science, 1992, 256: 186-192
[108] Kimura G, Takahashi M, Konno M. Mesozoic collision-extrusion tecto- nics ineastern Asia. Tectonophysics, 1990, 181: 15-23
[109] Lister G S, Etheridge E A, Symonds P A. Detachment models for the formation of passive continental margins. Tectonics, 1991, 10: 1038-1064
[110] Maruyama S, Isozaki Y, Kimura G, et al. Pale-geographic maps of the Japanese islands: plate tectonic synthesis from 750Ma to the present. The Island Arc, 1997, 6(1): 121-142
[111] Mitra S. Geometry and kinematic evolution of inversion structures. AAPG Bull, 1993, 77(7): 1159-1191
[112] Mooney W D, Meissner R. Multi-genetic origin of crustal reflectivity: a review of seismic reflection profiling of the continental lower crust and Moho. In: Fountain D M, Arculus R, Kay R W, ed. Continental lower crust, Amstertam: Elsevier Science Publishers B V, 1992. 45-80
[113] 杨宝俊, 于平, 李瑞磊. 用地震长剖面研究华北盆地及邻区区域构造特征. 长春科技大学学报, 2001, 31(地质地球物理综合专辑Ⅳ): 126-131
[114] 杨宝俊. 在地学断面域内用地震学方法研究大陆地壳: 以中国满洲里-绥芬河地学断面为例. 地质出版社, 1999
[115] Nelson R. Rift-segment interaction and its relation to hydrocarbon exploration in continental rift system. AAPG Bull, 1992, 76(8): 1153-1169
[116] Tapponnier P., et al. Propagating extrusion tectonics in Asia: New insights from simple experiments with plasticine. Geology, 1992, 10: 611-616
[117] Thatcher W, Hill D. A simple model for the fault-generated morphology of slow-spreading mid-oceanic ridges. Journal of Geophysical Research, 1995, 100: 561-570
[118] Tucholke B, Lin J. A geological model for the structure of ridge segments in slow spreading oceanic crust. Journal of Geophysical Research, 1994, 99: 11937- 11958
[119] Uyeda S. The Japanese island arc and the subduction process. Episodes, 1991, 14(3): 190-198
[120] Wang H, Mo X. An outline of the tectonic evolution of China. Episodes, 1995, 18(1-2): 6-16
[121] Willett S, Beaumont C, Fullsack P. A mechanical model for the tectonics of doubly -vergent compressional orogens. Geology, 1993, 21: 371-374
[122] Xu J W. The Tancheng-Lujiang wrench fault systerm, JOHN WILEY and SONS, 1993, 45-60
[123] Yang B J, Liu C, Hang L, et al. A study of detachment faults of the upper crust in Manzhouli-Suifenhe GGT by the method of vertical seismic reflection. In Liu G, ed.Proceeding of 30th International Geological Congress, VSP, UTRECHT THE NETHELANDS, 1997, 20: 51-61
[124] Yang B J, Mu S M, Jin xu, et al. Comprehensive geology study in the Manzhouli- Suifenhe geoscience transect, China, Chinese Journal of Geophysics (ACTA GEOPHYSICA SINICA), Allerton Press, Inc, NEW YORK, 1997, 40(1): 27-40
[125] Yang B J, Liu C, Yang P H. The basic characteristics of Moho near Daxinganling gravity gradient zone of China and it’s geological interpretation, In: Russian academy of sciences branch, Methods of study structure and monitoring of the Lithosphere (materials of the international conferences), Novosibirsk spc UIGGM SB RAS, 1998, 406-409
[126] Yang B J, Liu C, Tang J R, et al. The basic characteristics of the structure of Anda-Fengle nearly vertical seismic reflection profile of CHINA, In: Consejo superior de Investigacienes Cientificas (CSIC) and University of Barcelona, 8th International symposium on deep seismic profiling of the continents and their margins, Barcelona, Spain, 1998, 134
[127] Yin A, Nie S. A Phanerozoic palinspastic reconstruction of China and its neighboring regions. In: Yin A, Harrison T M, eds. The tectonic evolution of Asia. Cambridge: Cambridge University Press, 1996: 442-485
[128] 刘洋. 中国东北地区地壳物性分布特征及其与大地构造关系. 博士论文, 2006
[129] Bigg G R, Clark C D, Hughes A L C. A last glacial ice sheet on the Pacific Russian coast and catastrophic change arising from coupled ice-volcanic interaction. Earth and Planetary Science Letters, 2008, 265(3-4): 559-570
[130] Sun W D, Ding X, Hu Y H, et al. The golden transformation of the Cretaceous plate subduction in the West Pacific. Earth and Planetary Science Letters, 2007, 262(3-4): 533-542
[131] Liu S F, Liu B P. Comparative study on the juxtaposition events of Jurassic terranes in the Northern circum-Pacific belt, in Lithospheric Plate Tectonics and Dynamics. Geological Pubishing House,1995
[132] Graham D W, Reid M R, Jordan B T, et al. Mantle source provinces beneath the pacific Northwest revealed by helium isotope variations in basaltic lavas. Abstracts with Programs - Geological Society of America, 2007, 39(6): 455
[133] Zhao X X, Antretter M, Riisager P, et al. Rock magnetic results from Ocean Drilling Program Leg 192; implications for Ontong Java Plateau emplacement and tectonics of the Pacific. Geological Society Special Publications, 2004, 229: 45-61
[134] Roland, Burgmann, David D. P. Slip distributions on faults: effects of stress gradients,inelastic deformation, heterogeneous host-rock stiffness, and fault interaction. Journal of Structural Geology, 1994, 16(12): 1675-1690
[135] Zorin Y A. Geodynamics of the western part of the Mongolia-Okhotsk collisional belt,Trans-Bsikal region(Russia)and Mongolia. Tectonophysics, 1999, 306: 33-56
[136] Feng F K. Circum-Tethys and circum-Pacific basins. Journal of Southeast Asian Earth Sciences, 1996, 13(3-5): 305-315
[137] Hyeong K, Kim J, Yoo C, et al. Controlling factors of seabed manganese nodule genesis in the Northeast Pacific manganese nodule belt. Abstracts with Programs - Geological Society of America, 2007, 39(6): 71
[138] Hawkes A D, Korton B P, Grand P C. A microfossil-based approach to constraining megathrust-induced coseismic land displacement in the pacific Northwest. Abstracts with Programs - Geological Society of America, 2007, 39(6): 158
[139] Hong C H, Yoon J H. A three-dimensional numerical simulation of Typhoon Holly in the northwestern Pacific Ocean. Journal of Geophysical Research, 2003, 108(c8): 18
[140] Konstantinovskaia E A. Arc-continent collision and subduction reversal in the Cenozoic evolution of the Northwest Pacific: an example from Kamchataka(NE Russia). Tectonophysics, 2001, 333: 75-94
[141] Hilde, T W C, Uyeda S, Kroenke L. Evolution of the western Pacific and its margin. Tectonophysics, 1977, 38(1-2): 145-165
[142] Davis G A, Darby B J, Zheng Y D, et al. Geometric and temporal evolution of an extensional detachment fault, Hohhot metamorphic core complex. Inner Mongo- lia, China. Geology, 2002, 30(11): 1003-1008
[143] Darby B J, Davis G A, Zheng Y D. Structural evolution of the southwestern Daqingshan, Yinshan belt, Inner Mongolia, China. Geological Society of America, Memoir, 2001, 194: 199-214
[144] Ozawa S, Suito H, Nishimura T, et al. Possibility of recovery of slip deficit rate between the North American plate and the Pacific plate off Sanriku, northeast Japan. American Geophysical Union, 2007, 34(20): 25-28
[145] 杜旭东, 薛林福, 邬光辉. 中国东部大陆内部中生代盆地分布特征与地球动力学背景探讨. 长春科技大学学报, 1999, 29(2): 138-143
[146] Halim N, Kravchinsky V, Gilder S, et al. A Palaeomagnetic study from the Mongol-Okhotsk region: rotated Early Cretaceous volcanics and remagnetized Mesozoic sediments. Earth and Planetary Science Letters, 1998, 159: 133-145
[147] Keller G R, Drenth B J, Okure M S. A regional geophysical overview of the geoswath: pacific Northwest to the Appalachians. Abstracts with Programs - Geological Societyof America, 2007, 38(6): 614
[148] Northrup C J, Royden L H, Burchfiel B C. Motion of the Pacific Plate relative to Eurasia and its potential relation to Cenozoic extension along the eastern margin of Eurasia. Geology(Boulder), 1995, 23(8): 719-722
[149] 李乃胜, 赵松龄, 鲍·瓦西里耶夫. 西北太平洋边缘海地质. 黑龙江教育出版社, 2000
[150] Obata H, Alibo D S, Nozaki Y. Dissolved aluminum, indium, and cerium in the Sea of Japan and the Sea of Okhotsk; comparison to the marginal seas of the western North Pacific. Journal of Geophysical Research, 2007, 112(c12): 12003
[151] Verzhbitsky E V, Kononov M V, Kotelkin V D. Plate tectonics of the northern part of the Pacific Ocean. Oceanology, 2007, 47(5): 705-717
[152] Natal’in B. History and modes of Mesozoic accretion in Southeastern Russia. The island Arc. 1993, 2: 15-34
[153] A K ровушкина 等. 鄂霍茨克海北部沉积盆地的结构. 海洋地质动态, 2004, 20(12): 26-27
[154] Cao C R, Cao L. Crust structures and sectonic evolution of Northeast China in Mesonzoic. Journaly Geoscience Res. NE Asia, 1999, 2(2): 166-171
[155] 李家彪, 高抒. 中国边缘海岩石层结构与动力过程. 海洋出版社, 2003
[156] Chen B, Zhao G C, Wilde S A. Subduction and collision-related granitoids from Southern Sonidzuoqi, Inner Mongolia: Isotopic ages and tectonic implications. Geol. Rev, 2001, 47(4): 361-367
[157] Chen B, Jahn B M, Wilde S, et al. Two contrasting Paleozoic magmatic belts in northern Inner Mongolia, China: Petrogenesis and tectonic implications. Tectonophysics, 2000, 328: 157-182
[158] Darby B J, Davis G A, Zheng Y. Structural evolution of the southwestern Daqing Shan tectonic evolution of central Asia: From continental assembly to intracontinental deformation: Boulder, Colorado. Geological Society of America Memoir, 2001, 194: 199-214
[159] Davis G A, Darby B J, Zheng Y, et al. Geometric and temporal evolution of an extensional detachment fault, Hohhot metamorphic core complex, Inner Mongolia, China. Geology, 2002, 30: 1003-1006
[160] Davis G A, Xu B, Zhang Y D, et al. Indosinian extension in the Solonker suture zone: The Sonid Zuoqi metamorphic core complex, Inner Mongolia. China. Earth Science Frontiers, 2004, 11(3): 135-144
[161] Davis G A, Zheng Y D, Wang C, et al. Mesozoic tectonic evolution of the Yanshanfold and thrust belt, with emphasis on Hebei and Liaoning provinces, northern China. In: Hendrix M S, Davis G A, eds. Paleozoic and Mesozoic tectonic evolution of central Asia: From continental assembly to intracontinental deformation: Boulder, Colorado. Geological Society of America Memoir, 2001, 194: 171-197
[162] Dickinson W R. Basin geodynamics. Basin Research, 1993, 5: 195-196
[163] Dobretsov N L, Buslov M M, Yu U. Fragments of oceanic islands in accretion-collision areas of Gorny Altai and Salair, southern Siberia, Russia, In early stages of continental crustal growth of the Siberian continent in Vendian-Early Cambrian time. Journal of Asian Earth Sciences, 2004, 23: 673-690
[164] 郝天珧, Yuri Neprochnov, 江为为. 鄂霍茨克海的地球物理场与地质构造. 地球物理学进展, 2001, 16(1): 1-10
[165] 莫申国, 韩美莲, 李锦轶. 蒙古-鄂霍茨克造山带的组成及造山过程. 山东科技大学学报(自然科学版). 2005, 24(3): 50-64
[166] Kravchinsky V A, Cogne J P, Harbert W P, et al. Evolution of the Mongol-Okhotsk Ocean as constrained by new palaeomagnetic data from the Mongol-Okhotsk suture zone, Siberia. Geophys. J. Int, 2002, 148: 34-57
[167] Liu X W, Meng X G, Tamaki K, et al. Palinspastic reconstruction for tectonics of northeast China and its vicinity. Journal of China University of Geoscience, 1998, 9(3): 206-216
[168] Shakirov R B, Obzhirov A I, Salyuk A N, et al. Classification of anomalous methane fields in the Sea of Okhotsk Polar Meteorology and Glaciology, 2005, 19: 50-66
[169] Meng Q, Hu J, Jin J, et al. Tectonics of the late Mesozoic wide extensional basin system in the China-Mongolia border region. Basin Research, 2003a, 15: 397-415
[170] Meng Q. What drove late Mesozoic extension of the northern China-Mongolia tract? Tectonophysics, 2003b, 369: 155-174
[171] Verzhbitsky E V, Kononov M V. Geodynamic evolution of the lithosphere of the Sea of Okhotsk region from geophysical data. Izvestiya - Russian Academy of Sciences. Physics of the Solid Earth, 2006, 42(6): 490-501
[172] Ren J Y, Tamaki K, Li S T, et al. Late Mesozoic and Cenozoic rifting and its dynamic setting in eastern China and adjacent areas. Tectonophysics, 2002, 344: 175-205
[173] Ren S M, Zhu R X, Huang B C, et al. Paleomagnetic study on orogenic belt: An example from Early Cretaceous volcanic rocks, Inner Mongolia. China, Science in China Ser. D Earth Sciences, 2004, 47(12): 1127-1133
[174] Ritts B D, Darby B J, Cope T. Early Jurassic extensional basin formation in the Daqing Shan segment of the Yinshan belt, northern North China Block, InnerMongolia. Tectonophysics, 2001, 339: 239-258
[175] Rowley D B. Age of initiation of collision between India and Asia: a review of stratigraphic data. Earth and Planetary Science Letters, 1996, 145: 1-13
[176] Schellart W P, Lister G S. The role of the East Asian active margin in widespread extensional and strike-slip deformation in East Asia. Journal of the Geological Society, 2005, 162: 959-972
[177] Sha J G, Matsukawa M, Cai H W, et al. The Upper Jurassic-Lower Cretaceous of eastern Heilongjiang, northeast China: stratigraphy and regional basin history. Ctetaceous Research, 2003, 24: 715-728
[178] K ровушкинаОА等. 鄂霍茨克海北部沉积盆地的构造演化. 海洋地质动态, 2005, 21(1): 137-39
[179] Kravchinsky V A, Sorokin A A, Courtillot V. Paleomagnetism of Paleozoic and Mesozoic sediments from southern margin of Mongol-Okhotsk Ocean, far eastern Russia. Journal of Geophysical Research, 2002, 107(B10): 22
[180] Halim N, Kravchinsky V, Gilder S, etal. A palaeomagnetic study from the Mongol-Okhotsk region; rotated Early Cretaceous volcanics and remagnetized Mesozoic sediments. Earth and Planetary Science Letters, 1998, 159(3-4): 133-145
[181] Tomurtogoo O, Windley B F, Kroener A, etal. Zircon age and occurrence of the Adaatsag Ophiolite and Muron shear zone, central Mongolia; constraints on the evolution of the Mongol-Okhotsk ocean, suture and orogen. Journal of the Geological Society of London, 2005, 162(1): 125-134
[182] Kirillova G L. Late Mesozoic-Cenozoic sedimentary basins of active continental margin of Southeast Russia; paleogeography, tectonics, and coal-oil-gas presence. Marine and Petroleum Geology, 2003, 20(3-4): 385-397
[183] Ren S M, Zhu R X, Huang B C, etal. Paleomagnetic study on orogenic belt; an example from Early Cretaceous volcanic rocks, Inner Mongolia, China. Science in China. Series D, Earth Sciences, 2004, 47(12): 1127-1133
[184] Zhu B Q, Chang X Y, Qiu H N, etal. racteristics of Proterozoic basements on the geochemical steep zones in the continent of China and their implications for setting of superlarge deposits. Science in China. Series D, Earth Sciences, 1998, 41 卷增刊: 54-64
[185] Shang Q H. Occurrences of Permian radiolarians in central and eastern Nei Mongol(Inner Mongolia)and their geological significance to the northern China orogen. Chinese Science Bulletin, 2004, 49(24): 2613-2619
[186] Shao J, Liu F, Chen H, et al. Deep geological process and its shallow response duringMesozoic transfer of tectonic framework in eastern North China. Geol. Rev, 2000, 46: 32-40
[187] Tomurtogoo O, Windley B F, Kroner O, et al. Zircon age and occurence of the Adaatsag ophiolite and Muron shear zone, central Mongolia: constraints on the evolution of the Mongol-Okhotsk Ocean, suture and orogen. Journal of the Geological Society, 2005, 162: 125-134
[188] Wang H Z, Mo X X. An outline of the tectonic evolution of China: Episodes, 1995, 18: 6-16
[189] Lelikov E P, Emel’yanova T A. Volcanogenic complexes of the Sea of Okhotsk and the Sea of Japan (comparative analysis). Oceanology, 2007, 47(2): 273-281
[190] Wu F, Lin J, Wilde S A, et al. Nature and significance of the early Cretaceous gian igneous event in eastern China. Earth and Planetary Science Letters, 2005, 233: 103-119
[191] Xiao W J, Windley B F, Hao J, et al. Accretion leading to collision and the Permaian Solonker suture, Inner Mongolia, China: termination of the central Asian orogenic belt. Tectonics, 2003, 22(6): 1-20
[192] Xu X, Harbert W, Dril S, et al. New paleomagnetic data from the Mongol-Okhotsk collision zone, Chita region, south-central Russia: implication for Paleozoic paleogeography of the Mongol-Okhotsk Ocean. Tectonophysics, 1997, 269: 113-129
[193] Yarmolyuk V V, Kovalenko V I. The Mesozoic-Cenozoic of Mongolia. In: Tectonics, Magmatism and Metallogeny of Mongolia(Ed.by A.B.Dergunov), Taylor and Francis Group, 2001, 203-244
[194] Zheng Y D, Zhang Q, Wang Y, et al. Great Jurassic thrust sheets in Beishan(North Mountains)-Gobi areas of China and southern Mongolia. Journal of Structural Geology, 1996, 18(9): 1111-1126
[195] Zhu R X, Yang Z Y, Wu H N, et al. Paleomagnetic constraints on the tectonic history of the major blocks of China during the Phanerozoic. Science in China(Series D), 1998, 41: 1-19
[196] Tamura T, Nanayama F, Saito Y, et al. Intra-shoreface erosion in response to rapid sea-level fall; depositional record of a tectonically uplifted strand plain, Pacific coast of Japan. Sedimentology, 2007, 54(5): 1149-1162
[197] Kirillova G L. The Late Mesozoic-Cenozoic sedimentary basins at the continental margin of southeastern Russia; geodynamic evolution and coal and petroleum potential. Geotectonics, 2005, 39(5): 389-407
[198] Kelty T K, Yin A, Dash B, et al. Detrital-zircon geochronology of the Hangay-HenteyBasin; implications for the tectonics of the Mongol-Okhotsk Ocean, Mongolia. Abstracts with Programs - Geological Society of America, 2005, 37(7): 56
[199] 蒋志勇, 臧绍先, 周元泽. 鄂霍茨克海下间断面的起伏及俯冲带的穿透. 科学通报, 2003, 48(4): 320-327
[200] Galanin A A, Glushakova O Y. Oledeneniya, klimat i rastitel'nost' rayona Tauyskoy guby, Severnoye Priokhot'e, v pozdnechetvertichnoye vremya. Late Quaternary glaciation, climate and flora in the Tauy estuary, northern Okhotsk region. Geomorfologiya, 2006, 2: 50-62
[201] Kuz’min V K, Glebovitsky V A, Matukov D I, et al. The oldest basic granulites of Northeast Russia (Okhotsk Terrane). Doklady Earth Sciences, 2005, 402(4): 506-510
[202] Yuri Neprochnov, Hao T Y. Geophysical field and geological structure in Okhotsk Sea (in Russian). Journal of ocean geology, 1999, 39(4): 622-627
[203] Zonenshain L P, Lisitsin A P, Kuzmin M I, etal. Tectonics and hydrothermal activity in the TAG area (central Atlantic) according to MIR submersible dives. Eos, Transactions, American Geophysical Union, 1990, 71(43): 1577
[204] 吕延防, 孙永河, 付晓飞等. 逆断层中天然气运移特征的物理模拟. 地质科学, 2005, 40(4): 464-475
[205] 付立新, 王东林, 肖玉永. 伸展断层作用对油气二次运移的影响. 石油大学学报(自然科学版), 2000, 24(4): 71-74
[206] 邹华耀, 金燕, 黄光辉. 断层封闭与油气运移和聚集. 江汉石油学院学报, 1999, 21(1): 9-17
[207] 侯康明, 闻学泽. 板内逆断层地震破裂的基本特征及分段标志研究. 西北地震学报, 1999, 21(3): 302-309
[208] 陆绍俊. 深部逆断层对地震响应的影响研究. 河海大学学报, 1998, 26(6): 51-56
[209] 丁文龙, 金之钧, 丁艳红. 逆断层和聚敛型扭断层下盘圈闭条件分析及勘探意义. 江汉石油学院学报, 2003, 25(1): 30-31
[210] Yin A, Nie S Y. A Phanerozoic palinspastic reconstruction of China and its neighboring regions, in Yin A, and Harrison T M, eds. The tectonic evolution of Asia. Cambridge University Press, 1996, 442-485
[211] Yin A, Nie S Y. An indentation model for North and South China collision and the development of the TanLu and Honam fault systems, eastern Asia. Tectonics, 1993, 12: 801-813
[212] Zhang Y Q, Ma Y S, Yang N, et al. Cenozoic extensional stress evolution in North China. Journal of Geodynamics, 2003, 36: 591-613
[213] Zhang X D. Formation, evolution and earth dynamics of Jurassic and Cretaceousbasins in northern China. Petroleum Geology & Oilfield Development in Daqing, 2005, 24(5): 6-8
[214] Zhang Z, Yang L, Yu S, et al. Mirror image symmetry between sedimentary basin and consolidated crust in China. Geophysical Research Abstract, S2. 06, Volume 4. EGS, Nice, France, 2002
[215] Zhao W J, Nelson K K. Deep seismic reflection evidence for continental underthrusting beneath south Tibet. Nature, 1993, 366: 557-559
[216] 胡艳飞, 于平, 孔庆莹, 王世煜. 松辽盆地北安地区断陷期构造特征的地震学证据及其油气意义. 地球物理学进展, 2007, 22(5): 1455-1459
[217] Gawthorpe R L, Sharp L. Linked sequence stratigraphic and structural evolution of propagating normal faults. Geology, 1997, 25(9): 795-798
[218] Gupta S, Cowie P. A. A mechanism to explain rift-basin subsidence and stratigraphic patterns through fault-array evolution. Geology, 1998, 26(7): 595-598
[219] Kusznir N J, Ziegler M. The mechanics of continental extension and sedimentary basin formation: A simple-shear/pure-shear flexural cantilever model. Tectonophysics, 1992, 215: 117-131
[220] Malavieille J. Late orogenic extension in mountain belts: Insights from the basin and range province and the late Paleozoic variscan belt. Tectonics, 1993, 12(5): 1115-1130
[221] Patience A C, Christopher H S. Physical explanation for the displacement-length relationship of faults using a post-yield fracture mechanics model. Journal of Structual Geology, 1992, 14(10): 1133-1148
[222] Peacock D C P, Sanderson D J. Displacements, segment linkage and relay ramps in normal fault zones. Journal of Structural Geology, 1991, 13(6): 721-733
[223] Blundell D J. Some observations on basin evolution and dynamics. Journal of the Geological Society, 1991, 148: 789-800