用户名: 密码: 验证码:
勃利盆地和鸡西盆地的构造特征及油气远景研究
详细信息    本馆镜像全文|  推荐本文 |  |   获取CNKI官网全文
摘要
目前,随着全球对油气资源需求量的与日俱增,加大对油气田的勘探力度已经成为全球性的重点课题。勃利盆地和鸡西盆地作为大庆探区外围的断陷盆地,具有良好的油气潜力,因此对该区进行构造特征与油气远景分析具有重要的现实意义。
     本文以勃利盆地和鸡西盆地为研究对象,基于《大庆探区外围中、新生代断陷盆地群演化及油气远景分析》项目中的资料,从地球物理角度入手研究了盆地的沉积范围、构造特征、基底起伏和油气远景。首先建立叠加噪声的重力异常模型,通过利用小波分析方法进行信噪分离,认为基于提升算法软阈值的bior3.5小波具有良好的重构精度和滤波效果。随后,利用区域重力异常及其方向导数划分研究区的主要断裂构造,圈定了盆地的沉积范围。利用Park法计算研究区的莫霍面深度并分析其起伏形态。利用bior3.5小波对布设的三条高精度重力剖面数据进行滤波预处理,继而应用欧拉反褶积进行断裂深度计算。在地震剖面约束的基础上,计算重力基底深度并划分出重点凹陷区。最后讨论了研究区在重力和电性上的特征,从而分析勃利和鸡西盆地的油气前景。
Boli basin and Jixi basin located at our country Daqing Oil field prospecting region periphery, have the superiority region superiority and the exploration prospect. Strengthens to two basin geological data research, is advantageous in Daqing periphery prospecting region oil gas reserves investigation thorough expansion. Had the geologist to conduct the petroleum geology characteristic research to these two basins, but is related the geophysics material is more limited. This article studies the Boli basin and the Jixi basin gravitational field characteristic through the regional gravity data, and divides the faulted structure using the gravity reduction data computation basis depth, the union earth electromagnetism depth sounding material carries on the geophysics and the geologic interpretation. Is for the purpose of verifying two basins the basis nature, the basin boundary, the break position and the reciprocity, for geological duties and so on optimal advantageous exploration strategy target area provides the geophysics field the evidence. The research process including the method and the geologic interpretation two aspects, mainly studies the content to be as follows.
     1.In recent years, the wavelet analysis method became in the signal processing when -frequency analysis new method, but was few in number the first generation of wavelet and the promotion wavelet application in the potential field data denoising aspect's literature. Because includes the noise jamming frequently in the gravity actual signal, only then the rejection noise can the signal useful information performance. This article expected that applies the first generation of wavelet and the promotion wavelet carries on processing to the gravity measured data, thus enhances the actual data the application effect.
     In the article has related in detail the wavelet analysis correlation theories, discussed the Fourier transformation and the wavelet transformation time - frequency analysis characteristic and wavelet promotion method own superiority. In the numerous wavelet primary functions, the orthogonal wavelet decomposition has the auto-adapted time - frequency localization function, the biorthogonal wavelet has the good restructuring signal function, the promotion wavelet can, in does not consume the memory under the condition to accelerate the wavelet transformation, is the wavelet transformation highly effective algorithm. In view of the fact that the above several kind of wavelet primary function's characteristic, this article selects the orthogonal db4 wavelet and the biorthogonal bior3.5 wavelet carries on the letter chirp separation to the gravity data.
     2.Because the gravity measured data may the packet of energy include the sudden change signal, therefore divides into the gravity anomaly model the steady signal and the non-steady signal two parts, take this analysis wavelet primary function regarding the different signal's adaptation degree, and using the signal-to-noise ratio, the magnitude of error, the standard deviation and the image similarity does as the denoising effect measurable.
     Discovered through the model experiment that regarding the steady signal, the Fourier transformation, based on Brige-Massart the strategy determination threshold value's db4 wavelet, the bior3.5 wavelet and is biggest based on the promotion algorithm soft threshold value's bior3.5 wavelet to the signal-to-noise ratio promotion scope, their reconstruction effect is similar, is quite ideal.
     Regarding non-steady signal, but the packet of energy includes the sudden change information, some high frequency exceptionally often with the noise signal dopes in together. The model experiment indicated that the traditional Fourier transformation method cannot satisfy the non-steady signal the filter processing request, because this method cannot differentiate by the noise production high-frequency unit and the high-frequency unit which produces by the shallow layer geologic body. Because can not be able to attend to one thing without losing track of another thing purely to the frequency range filter, outside bandpass frequency spectrum is not differentiated filters. But in the wavelet transformation the noise signal and the unusual signal high frequency have the different threshold value level, may the selective discrimination not use the origin according to this characteristic high frequency exceptionally. The orthogonal wavelet and the biorthogonal wavelet have the very strong separating capacity regarding the noise signal and the high frequency signal, may restructure in the elimination noise foundation high frequency exceptionally. Is best based on the promotion algorithm soft threshold value's biorthogonal wavelet bior3.5 restructuring effect, may raise the counting yield during separation letter chirp.
     3.Through to the wavelet analysis in filter's research, used based on the promotion algorithm soft threshold value bior3.5 wavelet has processed Boli and the Jixi basin observed gravity data. When carries on the computation using the Euler deconvolution, if is not good using the letter chirp separation effect, the inversion result will receive the noise jamming to produce many separate spots, will create some break position insufficient centralism, the resolution is bad, will thus affect to the break position division. But after using the wavelet analysis in method's promotion wavelet bior3.5 carries on the denoising, some do not restrain the inversion point position obtains the elimination, enables the break division the accuracy to have the enhancement.
     4.0n the study of Boli basin and Jixi basin, uses the region Bouguer gravity anomaly, the derivative chart and in the upward continuation chart division research area faulted structure, M discontinuity's depth and carries on the analysis contact surface fluctuation shape using Park the law computation basin. Has carried on the division to the basin deposition scope, has selected the basin boundary, and has analyzed the gravitational field change rule. Synthesis massive geology and geophysics material, analysis peripheral faulted structure to basin influence. The analysis result indicated that Boli and the Jixi two basins have the close gravitational field characteristic, and structurally receives the peripheral deep big break the influence, once some scholars thought that Boli and Jixi have the same thing source, is the unified prototype basin has carried on the inference to the eastern basin. Therefore looked from the gravity angle that Boli and the Jixi basin should for the unified prototype basin, this regarding analyze both's oil gas potential to have the important geological significance.
     5.0n the study of the two basins important boundary structure belt and controls the trough break the geophysics field characteristic. Carries on the restraint using the neighboring area Hulin basin's three seismic cross-section to the gravity basis inversion result, based on this calculates three gravity reductions using the linear method of inversion the basis depth, divides the section plane using the Euler deconvolution computation's result and the electrical method material union the faulted structure. And the DB2 section plane located at the Boli basin east end, uses this section plane gravity data recognition Boli basin the south reason and north the reason boundary breaks each two, these breaks are affecting the Boli basin deposition scope and the conformation. The earth electromagnetism depth sounding material demonstrated that after entering the Boli basin, the electric properties have the obvious change, from this may distinguish the basin boundary break similarly. Discovered in the parsing process that the sincere dense break presents group of fault zones in the gravity and in the earth electromagnetism depth sounding material the mop shape. The DB3 section plane passes through two basins, located at the Boli basin middle. May distinguish Boli and the Jixi basin boundary break using the gravity data, has the change similarly in this position electric properties. The DB4 section plane located at the Boli basin's west end, distinguishes the Boli basin using the gravity and the electrical method material the west reason boundary break. The analysis thought that - Yitong breaks the similar performance located at Boli west of the basin is the same group of fault zone shape.
     6. Based on the gravitational and magnetotelluric data, we divided structural divisions in the sections. We also divided setion DB2 of Danbizhen, Dadingshan uplift, Dunmi subsidence, Mishan uplift, Boli basin, Fenshuigang uplift, Baoqing subsidence.The deepest depth of the gravity floor is 3 km.Then divided setion DB3 of Suiyang uplift, Dunmi subsidence, Muling uplift, Jixi Basin, Nadanhada uplift, Qitaihe uplift, Boli Basin, Qitaihe uplift, Beixing depression and Qixingzhen uplift. The deepest depth of the gravity floor is 5 km in Dunmi subsidence. We also divided setion DB4 of Xiaoxinganling uplift, Tangyuan subsidence, Yilan subsidence, Guokuishan uplift and Boli Basin. The deepest depth of the gravity floor is 2km in Tangyuan subsidence. Studyed the gravitational and magnetotelluric data, we analysics the area which have differed density and resistivity. We made an emphasis study the gravity anomaly, gravity floor and the variation of resistivity.
     7. Because the influence oil gas production, the accumulation, the storage and the escape factor is numerous, the oil gas analysis included all geological condition and the geological process nearly. Therefore through the preamble analysis, according to the collection geophysics and the geological data, has inferred Boli and the Jixi basin and the neighboring area oil gas prospect area from the gravity and the electrical angle.
     The first-level oil gas prospect area located at Boli basin north of treasure clear hollow (located at the DB2 section plane north most part). Analyzes from the structure, the gravity recognition's two breaks in 12 kilometers depths gather, break cutting is together deep, in the electric properties also distinguishes a break. In present's exploration, should pay attention to this break emphatically to this area oil gas influential role. The break has the possibility to destroy the oil gas accumulation, the structure causes the oil gas escape stave; Also has the possibility for the oil-gas migration constitution channel. Analyzes from the electric properties, lower part this depression's low resistivity extends the scope to be big, the electronic resistivity is extremely low, the magnitude only then severalΩ·m, in this crystallizing field's low stop-band possibly seeks for the oil gas Tibet's advantageous region. The second-level prospect area breaks located at Tangyuan falls the interior (the DB4 section plane Yilan County position). From the structure analyzes, the gravity distinguishes a Yilan - Yitong master fracture in this area, extends to 10km about. The electric properties demonstrate this area existence Yilan-Yitong fault zone. If this position existence transformation oil gas's condition, these big breaks should be possible to provide the good transportation channel, but breaks to the oil gas destructiveness also exists. Analyzes from the electric properties, should break falls internal has had the big area low density material, possibly was follows breaks falls in the drop process, middle had the partial magma invasion, creates the nowadays top and bottom low, the middle electronic resistivity high structure framework. Level mop width approximately 5km, in this part of low resistivity flank existence obvious electrical difference. This region surface layer was the low resistivity, the lower level was still a low resistivity, inferred it is the advantageous oil gas field, and suggested that carried on next step sifts the work.
     As the small oil field prospect area, may develop to further Boli and the Jixi basin sifts the work. Periphery looks over in three section planes the Boli basin resistivity distribution situation, the Boli basin interior electronic resistivity whole is lower than constructs the belt, anti- follows the few low resistivity distribution primarily basically by, the shallow layer often has the small area low resistivity in the partial distribution, has certain ethylene prospect, but the section plane material demonstration low resistivity area scale is not big. DB3 (the Suifen River - Big Dipper town) in the section plane Jixi basin scope width about 45km, between the section plane 149-174th spot, is middle the Jixi basin secondary structure. Among the gravity basis has blister, the deepest place is 2 km. The electronic resistivity reflects lower part the Jixi basin is extends the deep conductive bed downward. Two basins both belong to the fault comparison growth area, creates Boli area region Cheng Cengxing the difference. Has the possibility to form the fault seal structure, from this produces the fault block bulge or drops the area, has the possibility to form the good oil storage place. Speaking of these two basin's geological situation possibly forms the middle and small scale the oil-gas field.
     In summary, this article research has made certain progress, has studied each kind of wavelet base and the promotion wavelet in the method to the gravity data filter effect, has studied the wavelet base and the promotion wavelet with emphasis in processing steady and in the non-steady unusual signal characteristic, thus enhanced the gravity data inversion accuracy. In the data processing and the explanation aspect, have studied the Boli basin and the Jixi basin gravitational field essential feature, gained with the basin oil gas prospect related geophysics field evidence, has provided the beneficial supplement for the foundation geological data.
引文
[1]王谦身,安玉林,张赤军,等.重力学[M].北京:地质出版社,2003.
    [2]罗孝宽,郭绍雍.应用地球物理教程-重力 磁法[M].北京:地质出版社,1991.
    [3]汪新文.中国东北地区中-新生代盆地构造演化与油气关系[M].北京:地质出版社,2007.8.
    [4]李建平.小波分析与信号处理-理论、应用及软件实现[M].重庆:重庆出版社,1997.
    [5]Mallat S.A.,Theory for multiresolution signal decomposition:the wavelet representation IEEE Trans[J].On PAMI,1989,11(7):647-693.
    [6]Mallat S.Multiresolution and Wavelets[M].Philadephia:university of Pennsylvania,1998.
    [7]Mallat,S.,信号处理的小波导引(第2版)[M].杨力华,戴道清,黄文良,等译.北京:机械工业出版社,2002.
    [8]Mallat S.Multifrequency Channel decomposition and wavelet models IEEE ANS[J].On Acoustics,1989,37:209-211.
    [9]Daubechies I.,Orthonormal Bases of Compactly supported Wavelet[J].Communications on pure and Applied Math,1988(41):909-996.
    [10]Daubechies I.Ten lectures on wavelets.Society for Industrial and A Pplied Math[J].Philadelphia:Pennsylvania,1992.
    [11]Daubechies I.The wavelet transform,time frequency localization and signal analysis[J].I EEE Trans on Information Theory,1990,36:961-1006.
    [12]Sweldens W.The lifting scheme:A custom-design construction of biorthogonal wavelets[J].Appl.Comput.Harmon.Anal.1996,3(2):186-200.
    [13]Sweldens W.The lifting scheme:A construction of second generation wavelets[J].Siam J.Math.Anal.1997,29(2):511-546.
    [14]Maurizio F,Tatiana Q.Wavelet analysis for the regional residual and local separation of potential field anomalies[J].Geophysical Prospecting.1998,46:507-525.
    [15]Moreau F,Gilber D,Holschneider M,et al.Identification of sources of potential fields with the continuous wavelet transform Basic theory[J].Geophys Res.1999,104:5003-5013.
    [16]Hornby P,Boschetti F,Horovitz F G.Analysis of potential field data in the wavelet domain[J].Geophysics.1999,137:175-196.
    [17]Sailhac P,Galdeano A,Gibert D,Moreau F,Delor C.Identification of sources of potential field with the continuous wavelet transform:Complex wavelets and application to aeromagnetic profiles in French Guiana[J].Journal of Geophysical Research.2000,105:19455-19475.
    [18]程正兴.国外小波及应用概况[J].工程数学学报.1992,9(3):125-126.
    [19]侯遵泽,杨文采等.中国重力异常的小波变化与多尺度分析[J].地球物理学报,1997.40(1):85-95.
    [20]李宗杰,杨林.小波变换在位场数据处理中的应用[J].石油物探.1997,36(2):6-93.
    [21]杨文采等,离散小波变换与重力异常多重分解[J].地球物理学报,2001,44(4):534-542.
    [22]李建,周云轩,许惠平.重力场数据处理中小波母函数的选择[J].物探与化探.2001.25(6):410-417.
    [23]杨宇山,李媛媛,刘天佑,等.小波细节的微分特征及其在重力场断裂分析中的应用[J].地质与勘探,2003,39(1):41-44.
    [24]陈玉东.复小波变换反演重力异常[J].物探与化探,2003,27(5):354-361.
    [25]李淑玲,孙长虹,孟小红,等.位场的小波分析研究进展.地质与勘探.2005,41:202-204.
    [26]徐亚,郝天珧,周立宏.位场小波变换研究进展[J].地球物理学进展,2006,21(4):2311-8311.
    [27]张会战,方剑,张子占.小波分析在重力界面反演中的应用[J].武汉大学学报(信息科学版),2006,31(3):332-632.
    [28]邱宁,何展翔,昌彦君.分析研究基于小波分析与谱分析提高重力异常的分辨能力[J]地球物理学进展,2007,22(1):211-021.
    [29]徐亚,郝天珧.提升小波:可用于重磁资料处理的新方法[J].地球物理学进展,2004.
    [30]樊计昌,刘明军,王夫运,等.浅析小波分解最大层[J].科技导报.2008,26(10):40-42.
    [31]张莲,秦华峰,余成波.基于小波阈值去噪算法的研究[J].计算机工程与应用.2008,44(9):173.
    [32]赵军龙,谭成仟,焦积田.小波域阈值滤波在测井信号去噪中的应用[J].西安科技大学学报.2007,27(2):263-267.
    [33]赵池航,高成发,周百令,等.海洋重力异常数据处理中小波阈值选择规则分析[J].东南大学学报(自然科学版).2005,35(5):820-823.
    [34]钟凌云,刘天佑.小波线性软阈值法在航磁资料去噪中的应用[J].勘探地球物理进展.2004,27(4):280-284.
    [35]徐玉玲,贺振华,黄德济.基于小波变换的阈值降噪方法在地震资料处理中的应用[J].物探化探计算技术,2008,30(6).
    [36]王典,刘财,刘洋.基于提升算法和百分位数软阈值的小波去噪技术,2008,23(4):124-1129.
    [37]何永红,文鸿雁,靳鹏伟.一种基于小波模极大值去噪的改进方法[J].大地测量与地球动力学,2007,27(2):49-89.
    [38]王振国,周熙襄,李晶.基于小波变换的最小光滑滤波去噪[J].石油地球物理勘探,2002,37(6):594-600.
    [39]张旭东,詹毅,马永琴.小波变换与傅里叶变换在地震资料去噪中的对比[J]内蒙古石油化丁,2007,7:29-32.
    [40]钟凌云.小波变换方法在地震资料噪声消除中的应用[J].物探与化探,2007,31(3):245.
    [41]张学英.提升格式下几种去噪方法的比较[J].数学杂志.2006,26(6):701-705.
    [42]高德章,候遵泽,唐建.东海及邻区重力异常多尺度分解[J].地球物理学报,2000,43(6):842-849.
    [43]殷秀华,黎益仕,刘占波.塔里木盆地重力场与地壳上地幔结构[J].地震地质,1998,20(4):370-378.
    [44]黎海龙,朱国器.桂西地区重力场小波多重分解及地质意义[J].物探与化探,2007,31(5):564-864.
    [45]吴健生,刘苗.基于小波的位场数据融合[J].同济大学学报(自然科学版),2008,36(8):4311-7311.
    [46]刁博.重力异常小波多分辨分析[D].陕西:西北大学地质学系,2004.
    [47]候遵泽,杨文采,小波分析应用研究[J],物探化探计算技术,1995,17:1-9.
    [48]刁博,王家林,程顺有.重力异常小波多分辨分析分解阶次的确定[J].地球科学-中国地质大学学报,2007,32(4):565-865.
    [49]刘文龙.大庆探区外围盆地构造演化与油气资源赋存方式[J].大庆石油地质与开发.2005,24(1):23-26.
    [50]大庆油田石油地质志编写组.中国石油地质志(卷二.大庆油田)[M].北京:石油工业出版社,1993.
    [51]于恩君.黑龙江省鸡西-勃利含煤盆地地层序地层学讨论[J].吉林地质.2008,27(2):8-13.
    [52]杨晓平,李仰春,柳震,等.黑龙江东部鸡西盆地构造层序划分与盆地动力学演化[J].吉林大学学报.2005.35(5):616-621.
    [53]周兴福,杨晓平,郝永鸿,等.鸡两盆地高分辨率层序地层研究与聚煤作用分析[J].地质调查与研究.2005,28(2).
    [54]崔荣往,管叶君,李勤学,等.大庆油气地球物理技术发展史例[M].北京:石油工业出版社.2003.12.
    [55]江为为,刘伊克,郝天珧,等.四川盆地综合地质、地球物理研究[J].地球物理学进展,2001,16(1):12-23.
    [56]姜贵周.中国东北中新生代盆地成因与演化[J].大庆石油学院学报,1997,21(1):1-6.
    [57]韩春花,勃利盆地中生界地质特征及油气资源潜力分析[D].吉林:吉林大学地球科学学院,2005.
    [58]韩春花,曹成润,曹宪双,等.勃利盆地中生界地质特征及油气资源量计算[J].世界地质,2004,23(4):365-370.
    [59]王艳霞.鸡西盆地油气生成条件[J].煤炭技术.2005.24(5):100-101.
    [60]王建国,王林凤.鸡西含煤沉积盆地早期油气勘探[J].中国海上油气,1999,15(2):120-126.
    [61]彭淑芹,刘长军,马立军等.鸡西盆地煤层气远景初探[J].2006.24(6).
    [62]李春先,韩淑云,齐军.鸡西盆地油气赋存规律[J].煤炭技术.2005.24(05).
    [63]张健,王彦霞.鸡西煤田煤层气开发可行性分析[J].煤炭技术,2004,23(3):104-106.
    [64]王杰,和种铧,刘招君,等.鸡西盆地白垩纪碎屑岩地球化学特征及其对物源的制约[J].世界地质,2006,25(4):341-348.
    [65]白元真.勃利盆地煤层气资源远景评价[J].工业技术.2006.3:6.
    [66]高红梅,高福红,樊馥,等.鸡西盆地早白垩世烃源岩可溶有机质地球化学特征[J].吉林大学学报(地球科学版),2007,37(1):86-90.
    [67]张姗.黑龙江省东部早白垩世地层序列与盆地构造演化[D].吉林:吉林大学地球科学学院,2007.
    [68]何星,杨建国,李映雁,等.鸡西盆地烃源岩特征与评价[J].2008,27(4):24-44.
    [69]温泉波,刘永波,李俊杰,等.鸡西、勃利盆地白垩纪砂岩的物源分析及构造意义[J].沉积与特提斯地质,2008.28(3):25-95.
    [70]沈野.黑龙江省东部中生代盆地群边界特征及盆地演化[D].吉林:吉林大学地球科学探测与技术学院,2007.
    [71]刘殿秘.松辽盆地及其周围典型盆地部分地球物理特征[D].吉林:吉林大学地球科学探测与技术学院,2008.
    [72]孟令顺,杜晓娟.勘探重力学与地磁学[M].北京:地质出版社,2008.
    [73]Parker R L.The rapid calculation of potential anomalies[J].Geophysics Jour Roy Soc.1973,31:447-455.
    [74]Parker R L.The theory of ideal bodies for gravity interpretation[J].Geophysics,J.R.astr,Soc.,1975,42:315-334.
    [75]Thompson,D.T.,A new technique for making computer-assisted depth estimates from magnetic data[J].Geophysics,1982,47:32-38.
    [76]Reid,A.B.,Allsop,J.M.,Granser,H.,Millet,A.J.and Somerton,I.W.,Magnetic interpretation in three dimension using Euler deconvolution[J].Geophysics,1990,55:80-91.
    [77]Reid,a.b.,Euler Deconvoluti A Review[C].SEG Meeting,Houston.1995.
    [78]范美宁.欧拉反褶积方法的研究及应用[D].吉林:吉林大学地球科学探测与技术学院,2006.
    [79]穆石敏,申宁华,孙运生.区域地球物理数据处理方法及其应用[M].吉林:吉林科学技术版社,1990.
    [80]徐宝慈,李春华.位场数据处理理论与问题[M],吉林:吉林大学出版社,1995.
    [81]刘沈衡,吴燕冈.利用欧拉算反演磁性界面[J].石油物探,2000,39:101-106.
    [82]姚长利,管志宁,吴其斌,等.欧拉反演方法分析及实用技术改进[J].物探与化探,2004,28(2):150-155.
    [83]R.J.Durrheim and G.R.J.Cooper,Euldep:A program for the Euler deconvolution of magnetic and gravity data[J].Computers & Geosciences,1998,24(6):545-550.
    [84]陈玉东.地球物理信息处理基础[M].北京:地质出版社.2006.
    [85]向锋.小波理论在地球物理勘探中的应用[J].内蒙古石油化工.2008,13:22-32.
    [86]董长虹.Matlab小波分析与应用(第二版)[M].北京:国防工业出版社.2007.
    [87]刘天佑.位场勘探数据处理新方法[M].北京:科学出版社.2007.
    [88]葛哲学.小波分析理论与MATLABR2007实现[M].北京:电子工业出版社.2007.
    [89]王凯红,纪春华,王秀萍.敦密断裂带的地质特征及演化[J].吉林地质.2004.23(4):23-27.
    [90]郭孟习,孙炜,尹国义.郯庐断裂系的北延及地质地球物理特征[J].吉林地质,2000,19(3):36-44.
    [91]张宏,王小凤.郯庐断裂带北段地质特征及中生代演化[J].中国地科院沈阳地质矿产研究所集刊,1993,(2).
    [92]王金山,黑龙江省东部敦化-密山断裂带中的第三纪盆地[J].煤炭技术,2005,24(2):96-98.
    [93]于鸿禄.敦密断裂带构造特征与控煤规律[J].东北煤炭技术.1996.3:37-45.
    [94]葛肖虹,任收麦,刘永江.中国大型走滑断裂的复位研究与油气资源战略选区预测[J].地质通报,2006,25(9-10):1022-1027.
    [95]刘先文,单巨仁.郯庐断裂系研究的新进展-兼论东亚北东向走滑断裂系统[J].地球科学进展.1995,10(2):176-181.
    [96]国家地震局地质研究所.郯-庐断裂[M].北京:地质出版社.1987,27-28.
    [97]顾军,高德利,杨昌龙.大地电磁测深法探测地下油气资源的解释模型[J].中国石油大学学报(自然科学版),2006,30(1).
    [98]张凤旭,孟令顺,王世熠,等.用离散余弦变换(DCT)研究大庆探区外围DB1线重力场特征[J]吉林大学学报(地球科学版).2007,37(5):1009-1015.
    [99]Two-dimensional magnetotelluric inversion in combination of smoothest model and sharp boundary.Abstracts of the 19th International Workshop on Electromagnetic Induction in the Earth[C],2008(2).
    [100]Cagniard L.Basic theory of the magnetotelluric method of geophysical prospecting.Geophysics[C],1953:18.
    [101]Michel,Chouteau,Beno t.MT survey for oil and gas on Anticosti Island(Eastern Canada)[C],The 19th International Workshop on Electromagnetic Induction in the Earth,2008.
    [102]孙卫斌,宋群会,郑莉,等.大地电磁测深技术发展及在油气勘探的应用[J].地质与勘探.2003.39:3-9.
    [103]汤井田,王烨,杜华坤.高频大地电磁测深在深边部矿产勘探中的应用[J].国士资源导刊,2006,3(3):117-120.
    [104]Wenbo Wei,Martyn Unsworth,Alan Jones,et al.Detection of Widespread Fluids in the Tibetan Crust by Magnetotelluric Studies[J].Science,2001,2925517,292(5517):716-718.
    [105]T D Gamble,W M Goubau,J Clarke.Magnetotellurics with a remote magnetic reference [J].Geophysics,1979,441,44(1):53-68.
    [106]Chouteau M,Bouchard K.Two-dimensional terrain correction in magnetotelluric surveys[J].Geophysics,1988,536,53(6):854-862.
    [107]GAMBLE T D,GOUBAU W M,CLARKEJ.Magnetotelluric with a remote magnetic reference[J].Geophysics,1979,44(1):53-68.
    [108]SUTAMO D,VOZOFF K,RUBUST M.Estimation of magnetotelluric impedance tensors[J].Expl Geophysics,1989,22:382-398.
    [109]Applications of Integrated Geophysics in Oil & Gas Prospecting.Abstracts of the 19th International Workshop on Electromagnetic Induction in the Earth[C],2008(2).
    [110]Preliminary results of an MT Survey in the Nechako Sedimentary Basin,B.C.,Canada,designed to assess the usefulness of the technique in oil and gas exploration.Abstracts of the 19th International Workshop on Electromagnetic Induction in the Earth[C],2008(2).
    [111]Sutarno D,Vozoff K.Robust M-estimation of Magnetotelluric impedance tensors,Expl[J].Geophysics,1989,20,20:383-398.
    [112]Groom R W,Bailay R C.Decomposition of magnetotelluric impedance tensors in the present of local 3-D galvanic distortion[J].Geophysics.Res,1989,94,94:1913-1925.
    [113]Sims W E,Jr Bostick F X and Smith H W.The estimation of magnetotelluric impendance tensor elements from measured data[J].Geophysics,1971,36,36:938-942.
    [114]米萨克N纳比吉安.勘察地球物理电磁法(第一卷:理论)[M].赵经祥,王艳君,译.北京:地质出版社.1992:180-260.
    [115]大巴山褶皱带MT电性特征及其在油气勘探中的应用[J].工程地球物理学报.2006.3(3):183-186.
    [116]姜勇发,王金山,王宝君.鸡东盆地地热异常与地下热水分布规律研究[J].中国煤出地质.2001,13(3):38-39.
    [117]王靖华,吴汉宁,赵希刚.利用重力资料识别鄂尔多斯盆地断裂构造[J].能源技术与管理.2006,1:14-17.
    [118]杨森楠.中国区域大地构造学[M].北京:地质出版社,1985.
    [119]黄汲清.地质学及大地构造学[M].北京:地质出版社,1992.
    [120]孟卫丁.断陷盆地复杂斜坡带油气分布与成藏规律研究[D].西南石油大学,2006.
    [121]王秉海,钱凯.胜利油区地质研究与勘探实践[M].山东:石油大学出版社,1992.
    [122]陈刚,戴俊生,叶兴树,等.生长指数与断层落差的对比研究[J].西南石油大学学报,2007,29(3):20-23.
    [123]刘震,陈艳鹏,赵阳,等.陆相断陷盆地油气藏形成控制因素及分布规律概述[J].岩性油气藏,2007,19(2):122-133.
    [124]罗群.汤原断陷断裂特征与油气成藏的关系[J].新疆石油地质.1999,20(2):90-98.
    [125]王孔伟,张帆,刘志宏,等.依舒地堑汤原、方正断陷古近纪边界断裂活动特征[J].大地构造与成矿学,2006,30(4):445-454.
    [126]许浚远.依舒地堑新生代构造演化[J].地球科学,1997,22(4).
    [127]赵俊猛,卢造勋,姚长利.准噶尔盆地基底断裂的重磁学研究[J].地震地质.2008,30(1).
    [128]Zhao J M,Liu G D,Lu Z X,et al.Lithospheric structure and dynamic processes of the Tianshan orogenic beltand the Junggar Basin[J].Tectonophysics.2003,376,376:199-239.
    [129]Zhao,J.M.,Liu,G.D.,Lu,Z.X.Lithospheric structure and dynamic processes of the Tianshan orogenic belt and the Junggar Basin[J].Tectonophysics,2003,376,376(3-4):199-239.
    [130]冯建伟.准噶尔盆地乌夏断裂带构造演化及控油作用研究[D].北京:中国石油大学.2008.
    [131]HE Dengfa,LI Desheng,WU Xiaozhi.Basic Types and Structurel Characteristics of Uplifts:An Overview of Sedimentary Basin in China[J].ACTA GEOLOGICA SINICA.2009,83(2).
    [132]Lowell J D.Structural styles in petroleum exploration[J].OGCL.1985:1-43.
    [133]The initial interpretation for the geological structure and its impact on oil and gas in the northeast margin of the Mid-Yangtze[C].Wuhan:JOURNAL OF CHINA UNIVERSITY OF GEOSCIENCES,2007,18.
    [134]Aydin A.Fractures,faults,and hydrocarbon entrapment,migration and flow[J].Marine and Petroleum Geology,2000,17,17:797-814.
    [135]Qiang,Jin;McCabe,Peter J.,Genetic features of petroleum systems in rift basins of eastern China[J].Marine and Petroleum Geology,1998,15(4).
    [136]Huang Y S,GengA S,Fu JM,et al.The investigation of characteristics of biomarker assemblages and their precursors in Dam intun ultrahigh wax oils and related source rocks[J].Organic Geochem,1992,193,19(3):29-39.
    [137]Wessely G,LieblW.Oil and Gas in Alpidic Thrust Belts and Basins of Central and East- em Europe[J].1996:2-76.
    [138]Basin Analysis.Abstracts of 30th International Geological Congress[C].1996,1(3).
    [139]LB.Magoon主编,杨瑞召等译.含油气系统-研究现状和方法[M].北京:地质出版社.

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700