羌塘盆地双湖地区侏罗系白云岩成因及储集性研究
|
摘要
羌塘盆地位于青藏高原的腹地，是中国油气勘探程度最低的盆地之一，也是我国在特提斯域内最具潜力的油气勘探目标。侏罗系具有良好的生烃潜力，但是本地区储集层物性整体偏低，明显具有致密层的特点，能否找到优质储层已经成为制约对该盆地评价的关键问题之一。目前地表所发现的含油层系几乎都与白云岩有关，故确定白云岩的成因及孔隙演化史与油气运聚的关系，对于研究白云岩油藏至关重要。
本论文详细研究了双湖地区毕洛错—昂达尔错区块侏罗系白云岩成因及油气储集性，取得了以下进展和创新：
1．通过对主干剖面沉积相研究，确定了研究区侏罗系白云岩所处的相带：局限台地潮坪相和台地边缘礁滩相。米级旋回层序揭示了高频海平面变化引起的海水—淡水和盐水—淡水混合水白云石化。
2．在本研究区，首次应用岩相学、同位素地球化学、微量元素、电子探针、X-衍射等手段，对白云岩的白云石化过程从微观角度上进行了深入研究，得出本区白云石的三个世代及其相应的形成环境，第一世代为同生成岩阶段混合水白云石化形成，第二世代为早成岩期调整白云石化形成，第三世代为晚成岩期热液白云化作用形成。白云石的有序度高，为0.81-1.00。
3．对白云岩储层的储集性研究表明，储集空间主要为晶间孔、晶间溶孔、溶孔，孔隙度平均为6.50％；渗透率平均为15.24×10~(-3)μm~2，排驱压力很低，一般为0.06-0.42Mpa。喉道类型主要为片状和缩颈状，喉道分选较好，孔隙结构以大孔粗喉、中孔中喉为主。综合孔隙结构特征，本区块白云岩储层属Ⅰ、Ⅱ类型，为中孔中渗、低孔低渗类储层，整体评价为较好—好。
4．白云岩油气储集层的荧光发光部位以晶间溶孔、晶间孔、裂缝、溶孔、为主。荧光颜色主要为黄绿色、绿黄色、和黄色，发光强度大部份为亮和中亮。本区块油气绝大部分是晚成岩作用阶段后期二次运移进的。
5．研究区白云岩的孔隙演化经历了同生成岩、早成岩、晚成岩三个阶段，由最初的孔隙度35％降至如今的7％。孔隙演化与白云岩的埋藏史、研究区的生烃史和两次构造运动紧密相联。孔隙演化、圈闭形成、油气充注比较匹配，形成了如今布曲组白云岩的构造—岩性油藏。
6．利用激光碳氧同位素技术和包裹体分析并结合岩相学，研究了异形白云石对白云岩储集层物性的破坏作用，降低了孔隙度和渗透率。异形白云石的形成对应于燕山运动对油藏的初次破坏，同时表明有两期热液活动。
通过以上研究证实，双湖地区毕洛错-昂达尔错区块侏罗系白云岩的白云石化和孔隙度演化，与本地的生烃史、构造史匹配恰当，储集性能和含油气性良好，是羌塘盆地重要的油气储集层和潜在的产层，为下一步羌塘盆地油气勘探指明了方向。
Qiangtang Basin is located in the center of Qinghai-Xizang(Tibet) Plateau. It is a basin with the lowest degree in oil and gas exploration in China and is the most potential target for petroleum exploration in Tethys region. The Jurassic strata have a good hydrocarbon-generating potential, but the physical characteristics of reservoirs in the study area are poor on the whole, which are obviously characterized by densed reservoirs. Searching for the reservoirs of good quality is crucial to assessment of the basin. At present, oil-bearing layers found on the surface are nearly associated with dolomites. Hence, it is of significance in studying dolomite oil pool that the relationship between the origin and porosity evolution of dolomite and the migration and accumulation of oil-gas.
The dissertation has in detail studied the genesis and oil-gas reservoir properties of Jurassic dolomites of Biluoco-Angdarco block in Shuanghu area, and made the following progress and innovation.
1. Based on the research on the sedimentary facies of main sections, the facies belts of Jurassic dolomites in the study area are differentiated as refined platform tidal flat and platform margin reef or shoal facies. The meter scale cyclic sequences reveal the mixing water dolomitization resulted from frequent fluctuation of sea level.
2. In the study area, the dolomitizing process of dolomites has been deeply studied from microcosmic aspect for the first time by means of petrography, stable carbon and oxygen analysis, trace elements analysis, electrical probe and X-ray diffraction analysis, and it is acquired that three generations and corresponding forming environment of dolomites in the study area. The first generational dolomites were resulted from mixing water dolomitization in the syndiagenetic stage, the second generational dolomites were induced by regulating dolomitization in the early diagenetic stage, and the third generations were formed under the hydrothermal dolomitization. The ordering degree of dolomite is very high, ranging from 0.81 to 1.00.
3. Research on the reservoir properties of dolomites indicates that reservoir space consist of intercrystal pore, intercrystal dissolved pore and vug, and the porosity and permeability of dolomites are 6.5% and 15.24×10~(-3) μm~2 respectively. In addition, the value of replacement pressure is lower, ranging from 0.06 to 0.42Mpa. The types of throat are dominantly sheet and necking down, and the sorting of throats is good. The big pore with wide throat and the moderate pore with moderate throat are primary
本论文详细研究了双湖地区毕洛错—昂达尔错区块侏罗系白云岩成因及油气储集性，取得了以下进展和创新：
1．通过对主干剖面沉积相研究，确定了研究区侏罗系白云岩所处的相带：局限台地潮坪相和台地边缘礁滩相。米级旋回层序揭示了高频海平面变化引起的海水—淡水和盐水—淡水混合水白云石化。
2．在本研究区，首次应用岩相学、同位素地球化学、微量元素、电子探针、X-衍射等手段，对白云岩的白云石化过程从微观角度上进行了深入研究，得出本区白云石的三个世代及其相应的形成环境，第一世代为同生成岩阶段混合水白云石化形成，第二世代为早成岩期调整白云石化形成，第三世代为晚成岩期热液白云化作用形成。白云石的有序度高，为0.81-1.00。
3．对白云岩储层的储集性研究表明，储集空间主要为晶间孔、晶间溶孔、溶孔，孔隙度平均为6.50％；渗透率平均为15.24×10~(-3)μm~2，排驱压力很低，一般为0.06-0.42Mpa。喉道类型主要为片状和缩颈状，喉道分选较好，孔隙结构以大孔粗喉、中孔中喉为主。综合孔隙结构特征，本区块白云岩储层属Ⅰ、Ⅱ类型，为中孔中渗、低孔低渗类储层，整体评价为较好—好。
4．白云岩油气储集层的荧光发光部位以晶间溶孔、晶间孔、裂缝、溶孔、为主。荧光颜色主要为黄绿色、绿黄色、和黄色，发光强度大部份为亮和中亮。本区块油气绝大部分是晚成岩作用阶段后期二次运移进的。
5．研究区白云岩的孔隙演化经历了同生成岩、早成岩、晚成岩三个阶段，由最初的孔隙度35％降至如今的7％。孔隙演化与白云岩的埋藏史、研究区的生烃史和两次构造运动紧密相联。孔隙演化、圈闭形成、油气充注比较匹配，形成了如今布曲组白云岩的构造—岩性油藏。
6．利用激光碳氧同位素技术和包裹体分析并结合岩相学，研究了异形白云石对白云岩储集层物性的破坏作用，降低了孔隙度和渗透率。异形白云石的形成对应于燕山运动对油藏的初次破坏，同时表明有两期热液活动。
通过以上研究证实，双湖地区毕洛错-昂达尔错区块侏罗系白云岩的白云石化和孔隙度演化，与本地的生烃史、构造史匹配恰当，储集性能和含油气性良好，是羌塘盆地重要的油气储集层和潜在的产层，为下一步羌塘盆地油气勘探指明了方向。
Qiangtang Basin is located in the center of Qinghai-Xizang(Tibet) Plateau. It is a basin with the lowest degree in oil and gas exploration in China and is the most potential target for petroleum exploration in Tethys region. The Jurassic strata have a good hydrocarbon-generating potential, but the physical characteristics of reservoirs in the study area are poor on the whole, which are obviously characterized by densed reservoirs. Searching for the reservoirs of good quality is crucial to assessment of the basin. At present, oil-bearing layers found on the surface are nearly associated with dolomites. Hence, it is of significance in studying dolomite oil pool that the relationship between the origin and porosity evolution of dolomite and the migration and accumulation of oil-gas.
The dissertation has in detail studied the genesis and oil-gas reservoir properties of Jurassic dolomites of Biluoco-Angdarco block in Shuanghu area, and made the following progress and innovation.
1. Based on the research on the sedimentary facies of main sections, the facies belts of Jurassic dolomites in the study area are differentiated as refined platform tidal flat and platform margin reef or shoal facies. The meter scale cyclic sequences reveal the mixing water dolomitization resulted from frequent fluctuation of sea level.
2. In the study area, the dolomitizing process of dolomites has been deeply studied from microcosmic aspect for the first time by means of petrography, stable carbon and oxygen analysis, trace elements analysis, electrical probe and X-ray diffraction analysis, and it is acquired that three generations and corresponding forming environment of dolomites in the study area. The first generational dolomites were resulted from mixing water dolomitization in the syndiagenetic stage, the second generational dolomites were induced by regulating dolomitization in the early diagenetic stage, and the third generations were formed under the hydrothermal dolomitization. The ordering degree of dolomite is very high, ranging from 0.81 to 1.00.
3. Research on the reservoir properties of dolomites indicates that reservoir space consist of intercrystal pore, intercrystal dissolved pore and vug, and the porosity and permeability of dolomites are 6.5% and 15.24×10~(-3) μm~2 respectively. In addition, the value of replacement pressure is lower, ranging from 0.06 to 0.42Mpa. The types of throat are dominantly sheet and necking down, and the sorting of throats is good. The big pore with wide throat and the moderate pore with moderate throat are primary
引文
[1] 强子同．碳酸盐岩储层地质学[M]．东营：石油大学出版社．1998．1-470
[2] 郝石生，贾振远．碳酸盐岩油气形成和分布[M]．北京：石油工业出版社．1989．1-401
[3] 曾允孚，夏文杰．沉积岩石学[M]．北京：地质出版社．1986．1-274
[4] 姜在兴．沉积学[M]．北京：石油工业出版社．2003．1-540
[5] 赵澄林．沉积学原理[M]．北京：石油工业出版社．2001．1-214
[6] 范嘉松．中国生物礁与油气[M]．北京：海洋出版社．1996．1-329
[7] F．K．诺斯．石油地质学[M]．北京：石油工业出版社．1994．1-582
[8] 冯增昭，彭永民，金振奎等．中国寒武纪和奥陶纪岩相古地理[M]．北京：石油工业出版社．2004．29-47
[9] 赵政璋，李永铁，叶和飞等．青藏高原羌塘盆地石油地质[M]．北京：科学出版社．2000．1-398
[10] 赵政璋，李永铁，叶和飞等．青藏高原中生界沉积相及油气储盖层特征[M]．北京：科学出版社．2000．1-347
[11] 方少仙，董兆雄，侯方浩等．层状白云岩储层特征与成因[M]．北京：地质出版社．1999．1-115
[12] 顾家裕，朱筱敏，贾进华等．塔里木盆地沉积与储层[M]．北京：石油工业出版社．2003．1-400
[13] 马永生，梅冥相，陈小兵等．碳酸盐岩储层沉积学[M]．北京：地质出版社．1999．1-364
[14] 刘岫峰．沉积岩实验室研究方法[M]．北京：地质出版社．1991．1-298
[15] 许怀先，陈丽华，万玉金等．石油地质实验测试技术与应用[M]．北京：石油工业出版社．2001．1-308
[16] 钱峥，黄先雄．碳酸盐岩成岩作用及储层—以中国四川东部石炭系为例[M]．北京：石油工业出版社．2000．1-119
[17] 王成善，伊海生，李勇等．西藏羌塘盆地地质演化与油气远景评价[M]．北京：地质出版社．2001．184—215
[18] H．G．里丁等．沉积环境和相[M]．北京：科学出版社．1985．222-390
[19] 赵政璋，李永铁，王岫岩，等．羌塘盆地南部海相侏罗系古油藏例析[J]．海相油气地质，2002，7(3)：34-36
[20] 伊海生，高春文，张小青，等．羌塘盆地双湖地区古油藏白云岩储层的显微成岩组构特征及意义[J]．成都理工大学学报，2004，31(6)：611-615
[21] 王成善，伊海生，刘池洋，等．西藏羌塘盆地古油藏发现及其与油气远景评价的意义[J]．石油与天然气地质，2004，25(2)：139-143
[22] 黄思静．上扬子地台区晚古生代海相碳酸盐岩的碳、锶同位素研究[J]．地质学报，1997，71(1)：45-53
[23] 黄思静，石和，毛晓东等．早古生代海相碳酸盐的成岩蚀变性及其对海水信息的保存[J]．成都理工大学学报，2003，30(1)：9-18[24] 郑荣才，刘文均，李祥辉等．白云岩成因在层序地层研究中的应用[J]．矿物岩石，1996，16(1)：28-37
[25] 田景春，陈洪德，侯明才等．右江盆地晚古生代白云岩与层序地层的关系及其储集性[J]．成都理工大学学报，2004，31(1)：34-39
[26] 杨华，付锁堂，马振芳，等．天环地区奥陶系白云岩储集体特征[J]．天然气工业，2004，24(9)：11-15．
[27] 李振宏，杨永恒．白云岩成因研究现状及进展[J]．油气地质与采收率，2005，12(2)：5-8
[28] 杨威，王清华，刘效曾．塔里木盆地和田河气田下奥陶统白云岩成因[J]．沉积学报，2000，18(4)：544-548
[29] 顾家裕．塔里木盆地下奥陶统白云岩特征及成因[J]．新疆石油地质，2000，21(2)：120-122
[30] 邵龙义，何宏，彭苏萍等．塔里木盆地巴楚隆起寒武系及奥陶系白云岩类型及形成机理[J]．古地理学报，2002，4(2)：19-30
[31] 朱井泉，李永铁．藏北羌塘盆地侏罗系白云岩类型、成因及油气储集特征[J]．古地理学报，2000，2(4)：30-42
[32] 杨桂芳，藤玉洪，卓胜广等．藏北羌塘盆地双湖地区油气成藏条件[J]．地质通报，2003，22(4)：285-289
[33] 魏国齐，杨威，张林等．川东北飞仙关组鲕滩储层白云石化成因模式[J]．天然气地球科学，2005，16(2)：162-166
[34] 张立强，纪友亮，李永铁．羌塘盆地侏罗系白云岩储层特征研究[J]．石油实验地质，2001，23(4)：384-389
[35] 张传禄，张永生，康祺发等．鄂尔多斯南部奥陶系马家沟群马六组白云岩成因[J]．石油学报，2001，22(3)：22-25
[36] 曾理，万茂霞，彭英．白云石有序度及其在石油地质中的应用[J]．天然气勘探与开发，2004，27(4)：64-66
[37] 贾振远，蔡忠贤．成岩地层学与层序地层学[J]．地球科学—中国地质大学学报，1997，22(5)：538-543
[38] 桑树勋，郑永飞，张华等．徐州地区下古生界碳酸盐岩的碳、氧同位素研究[J]．岩石学报，2004，20(3)：707-716
[39] 杨万容，杨长庚，沈建伟．湖南慈利晚二叠世长兴期珊瑚礁白云石化及其成岩环境[J]．地质学报，2002，76(1)：114-124
[40] 邓长瑜，张秀莲，陈建文等．黔东南地区寒武系碳酸盐岩成岩作用分析[J]．沉积学报，2004，22(4)：588-596
[41] 胡明毅，高振中，李建明．中上扬子区古生界深水斜坡及台地边缘碳酸盐岩成岩作用[J]．石油实验地质，1998，20(3)：239-247
[42] 张秀莲．碳酸盐岩中氧、碳稳定同位素与古盐度、古水温的关系[J]．沉积学报，1985，3(4)：17-29
[43] 何道清．碳酸盐岩碳、氧同位素分析激光微取样技术[J]西南石油学院学报，2003，25(1)：12-15
[44] 王英华．碳酸盐岩成岩作用与孔隙演化[J]．沉积学报，1992，10(3)：85-95
[45] 王剑，谭富文，李亚林等．青藏高原重点沉积盆地油气资源潜力分析[M]．北京：地质出版社．2004．1-317[46] 张小青，伊海生，朱迎堂．羌塘盆地双湖地区白云岩储集层特征研究[J]．西南石油学院学报，2005，27(5)：10-13．
[47] 何自新，杨奕华．鄂尔多斯盆地奥陶系储层图册[M]．北京：石油工业出版社．2004．1-244．
[48] 王剑，谭富文，王小龙等．藏北羌塘盆地早侏罗世—中侏罗世早期沉积构造特征[J]．沉积学报，2004，22(2)：198-206
[49] BT库兹涅左夫．地史上碳酸盐聚积演化的若干特点——白云石形成演化和碳酸盐聚积与全球地质环境的关系[J]．天然气地球科学，2002，13(1～2)：18-29
[50] 覃建雄，曾允孚．鄂尔多斯盆地东部下奥陶统白云岩地球化学研究[J]．矿物学报，1994，14(1)：22-32
[51] 姜月华，岳文浙，柳祖汉等．湖南晚二叠世生物礁成岩作用的碳、氧同位素研究[J]．地质论评，2000，46(2)：190-197
[52] 郑永飞，徐宝龙，周根陶．矿物稳定同位素地球化学研究[J]．地学前缘，2000，7(2)：299-321
[53] 许建华，侯中昊，王金友等．羌塘盆地流体包裹体特征及其在储层成岩研究中的应用[J]．石油实验地质，2003，25(1)：81-87
[54] 罗建宁，朱忠发，谢渊等．羌塘盆地生物礁岩特征与沉积模式[J]．沉积与特提斯地质，2004，24(2)：51-63
[55] 谭富文，王剑，王小龙等．羌塘盆地雁石坪地区中—晚侏罗世碳、氧同位素特征与沉积环境分析[J]．地球学报，2004，25(2)：119-126
[56] 彭军，田景春．陕甘宁盆地中部气田中区马五段白云岩成因类型及其地球化学特征[J]．矿物岩石，1998，18(2)：35-39
[57] 朱井泉．上扬子台地三叠系碳酸盐岩中的特形白云石及其指相意义初探[J]．岩相古地理，1996，16(4)：32-40
[58] 钟建华，温志峰，李勇等．生物礁的研究现状与发展趋势[J]．地质评论，2005，51(3)：288-301
[59] 范嘉松．世界碳酸盐岩油气田的储层特征及其成藏的主要控制因素[J]．地学前缘，2005，12(3)：23-31
[60] 李红亮，汪华，史习杰．四川盆地川东地区上二叠统礁白云石的类型及其特征[J]．天然气勘探与开发，1999，22(3)：25-30
[61] 王志兴，张帆，马青等．四川盆地东部晚二叠世—早三叠世飞仙关期礁、滩特征与海平面变化[J]．沉积学报，2002，20(2)：249-255
[62] 何幼斌，冯增昭．四川盆地及其周缘下二叠统细—粗晶白云岩成因探讨[J]．江汉石油学院学报，1996，18(4)：15-21
[63] 胡恒，陈景山．塔北地区下奥陶统碳酸盐岩成岩作用及孔隙演化[J]．成都理工学院学报(增刊)，1996，23：104-111
[64] 郭建华，沈昭国，李建明．塔北东段下奥陶统白云石化作用[J]．石油与天然气地质，1994，15(1)：51-60
[65] 艾华国，兰林英，张克银．塔里木盆地不整合面下的碳酸盐岩成岩作用及孔隙特征[J]．新疆石油地质，1998，19(2)：112-122
[66] 杨威，王清华，刘效曾．塔里木盆地和田河气田下奥陶统白云岩成因[J]．沉积学报，2000，18(4)：544-549
[67] 蒋凌志，于德龙．塔里木盆地麦盖提斜坡石炭系生屑灰岩段储层特征研究[J]．北京大学学??报(自然科学版)，2003，39(3)：428-435
[68] 沈昭国，陈永武，郭建华．塔里木盆地下古生界白云石化成因机理及模式探讨[J]．新疆石油地质，1995，16(4)：319-325
[69] 王志兴，王振宇，马青等．塔里木盆地中部生物屑灰岩段滩体特征及储集性[J]．石油与天然气地质，2002，23(1)：58-64
[70] 翟永红，王泽中，王正允等．塔中1井储层段岩石学特征集成岩作用[J]．西安地质学报，1994，16(3)：38-46
[71] 王嗣敏，吕修祥．塔中地区奥陶系碳酸盐岩储层特征及其油气意义[J]．西安石油大学学报(自然科学版)，2004，19(7)：72-78
[72] 翟永红，郭建华，刘生国．塔中地区石炭系碳酸盐岩成岩作用与储层评价[J]．江汉石油学院学报，1995，17(3)：13-19
[73] 周根陶，郑永飞．碳酸钙—水体系氧同位素分馏系数的低温实验研究[J]．地学前缘，2000，7(2)：320-338
[74] 郑永飞，周根陶，龚冰．碳酸盐矿物氧同位素分馏的理论研究[J]．高校地质学报，1997，3(3)：241-256
[75] 李双应，金福全，王道轩．碳酸盐岩成岩作用的微量元素地球化学特征[J]．石油实验地质，1995，17(1)：55-64
[76] 杨威，王清华，赵仁德等．碳酸盐岩成岩作用及其对储层控制的定量评价[J]．地球学报，2001，22(5)：441-447
[77] 陈方鸿，谢庆斌，王贵文．碳酸盐岩成岩作用与层序地层学关系研究——以鄂尔多斯盆地寒武系为例[J]．岩相古地理，1999，19(1)：20-25
[78] 杨华，付锁堂，马振芳等．天环地区奥陶系白云岩储集体特征[J]．天然气工业，2004，24(9)：11-17
[79] 杜学斌，张成，张彩明．稳定同位素地球化学在盆地流体分析中的应用现状及发展前景[J]．油气地质与采收率，2005，12(4)：20-25
[80] 陈学时，周进高．下扬子区寒武纪斜坡—盆地相沉积的成岩作用及储集类型[J]．石油与天然气地质，1994，15(1)：70-82
[81] 朱莲芳．中国天然气碳酸盐岩储层形成的成岩模式[J]．沉积学报，1995，13(2)：140-149
[82] 胡明毅，朱忠德，郭成贤．中扬子地区海相碳酸盐岩储层类型和特征[J]．石油勘探与开发，1994，21(1)：106-115
[83] 梁百和，朱素琳，刘英霞等．中扬子晚石炭世碳酸盐岩的成岩作用[J]．中山大学学报(自然科学版)，1996，35(2)：106-112
[84] 翟永红，郭成贤，郭建华等．中扬子台地北缘灯影组白云岩研究[J]．矿物岩石，1996，16(3)：36-42
[85] 翟永红，郭成贤．中扬子台地北缘灯影组碳酸盐岩成岩作用序列集成岩模式[J]．地质地球化学，1997，(2)：45-52
[86] Denis Lavoie, Guoxiang Chi. The Lower Silurian Sayabec Formation in northern Gaspe:carbonate diagenesis and reservoir potential[J]. Bulletin of Canadian Petroleum Geology,2001,49,(2):282-298
[87] Michael W.Rasser, Alois Ferminger. Paleoenvirortmental and diagenetic implications of δ 180and δ 13C isotpe ratios from the Upper Jurassic Piassen limestone(Northern Calcareous Alps,Austria)[J].Geobios,2002,35:41-49
[88] Achour Madi, Martine M. Savard, Pierre-Andre Bourque, et al. Hydrocarbon potential of the Mississippian carbonate platform, Bechar basin, Algerian Sahara[J]. AAPG Bulletin, 2000,84(2):266-287
[89] Ihsan S. Al-Aasm, Karem K. Azmy. Diagenesis and evolution of microporosity of Middle-Upper Devonian Kee scarp reefs, Norman wells, Northwest territories, Canada: petrographic and chemical evidence[J]. AAPG Bulletin,1996,80(1):82-l00
[90] Robert E. Woody, Jay M. Gregg, Leonard F. Koederitz. Effect of texture on petrophysical properties of dolomite: evidence from the Cambrian-Ordovician of Southeastern Missouri[J]. AAPG Bulletin, 1996,80(1):119-132
[91] Jeff Lonnee, Ihsan S.Al-Aasm. Dolomitization and fluid evolution in the Middle Devonian Sulphur Point Formation, Rainbow South Field, Alberta: petrographic and geochemical evidence[J]. Bulletin of Canadian Petroleum Geology,2000,48(3):262-283
[92] Huang Sijing, Xiao Linping, Yang Junjie et al. Experimental Simulation of Dolomite Dissolution Under Burial Diagenesis Conditions and Thermodynamic Interpretation[J]. Chinese Journal of geochemistry,2000,19(1) :58-65
[93] Esref Atabey. Peirography and origin of dolomites of yaniktepe formation (upper cretaceous) in gurun autochthonous, eastern Taurus turkey[J]. Mineral Res.Expl.Bull., 1995,117:59-67
[94] Scott Durocher, Ihsan S. Al-Aasm. Dolomitization and Neomorphism of Mississippian (Visean) Upper Debolt Formation, Blueberry field, Northeastern British Columbia: geologic, petrologic, and chemical evidence[J]. AAPG Bulletin,1997,81(6):954-977
[95] F. Jerry Lucia. Rock-fabric/petrophysical classification of carbonate pore space for reservoir characterization[J]. AAPG Bulletin,1995,79(9):1275-1300
[96] Eric W. Mountjoy, Xiomara M. Marquez. Predicting reservoir properties in dolomites: Upper Devonian Leduc Buildups, deep Alberta basin[J]. AAPG Memoir, 1997, 69:267-306
[97] Piere-Andre Bourque, Martine M. Savard, Guoxiang Chi, et al. Diagenesis and porosity evolution of the Upper Silurian-Lowermost Devonian West Point reef limestone, eastern Gaspe Belt, Quebec Appalachians[J]. Bulletin of Canadian Petroleum Geology,2001,49(2):299-326
[98] Denis Lavoie, Guoxiang Chi. The Lower Silurian Sayabec Formation in northern Gaspe: carbonate diagenesis and reservoir potential[J]. Bulletin of Canadian Petroleum Geology,2001,49(2):282-298
[99] Herbert Th. Eichenseer, Frederic R. Walgenwitz, Patrick J. Biondi. Stratigraphic control on facies and diagenesis of dolomitized oolitic siliciclastic ramp sequences (Pinda Group, Albian, Offshore Angola)[J]. AAPG Bulletin, 1999,83(11):1729-1758
[100] Maurice E. Tucker. Sedimentary Petrology (3rd Edition) [M]. Oxford: Blackwell Science. 2001.1-262
[101] Moss,S.J,,Tucker, M.E. Dolomitisation associated with transgressive surfaces: a mid-Cretaceous example[J]. Sedimentary Geology, 1996,107:11-20
[102] Hans G Machel, Jeff Lonnee. Hydrothermal dolomite—a product of poor definition and
imagination[J]. Sedimentary Geology,2002,152:163-171
[103] Fred J.Longstaffe, Ran Calvo, Avner Ayalon et al. Stable isotope evidence for multiple fluid regimes during carbonate cementation of the Upper Tertiary Hazeva Formation,Dead Sea Graben, southerm Israel[J]. Journal of Geochemical Exploration,2003,80:151-170
[104] Reinhold R.Leinfelder, Stuttgart. Upper Jurassic reef types and controlling factors[J]. Stuttgart, 1993,19(5): 1-45
[105] M.Boni, G.Parente, T.Bechstadt et al. Hydrothermal dolomites in SW Sardinia (Italy): evidence for a widespread late-Variscan fluid flow event[J]. Sedimentary Geology,2000,131:181-200
[106] M. Esteban, C. Taberner. Secondary porosity development during late burial in carbonate reservoirs as a result of mixing and/or cooling of brines[J]. Journal of Geochemical Exploration,2003,78- 79:355- 359
[107] A. Torok. Formation of dolomite mottling in Middle Triassic ramp carbonates (Southern Hungary)[J]. Sedimentary Geology,2000,131:131-145
[108] Hairuo Qing. Petrography and geochemistry of early-stage, fine and medium-crystalline dolomites in the Middle Devonian Presqu'ile Barrier at Pine Point,Canada[J]. Sedimentology, 1998,45:433-446
[109] Joachim E. Amthor, Gerald M. Friedman. Dolomite-rock textures and secondary porosity development in Ellenburger Group Carbonate (Lower Ordovician), west Texas and southeastern New Mexico[J]. Sedimentology, 1991,38:343-362
[110] Fadi H. Nader, Rudy Swennen. Petroleum prospects of Lebanon: some remarks from sedimentological and diagenetic studies of Jurassic carbonates[J]. Marine and Petroleum Geology ,2004,21: 427-441.
[111] John Warren. Dolomite: occurrence, evolution and economically important associations[J]. Earth-Science,2000,52:1 -81
[112] Alex MacNeil, Brian Jones. Dolomitization of the Pedro Castle Formation (Pliocene), Cayman Brac, British West Indies[J].Sedimentary Geology 2003,162:219-238
[113] Leslie A.Melim, Peter A.Scholle. Dolomitization of the Capitan Formation forereef facies (Permian, west Texas and New Mexico): seepage reflux revisited [J]. Sedimentology, 2002,49:1207-1227
[114] Feng Zengzhao, Zhang Yongsheng, Jin Zhenkui. Type ,origin and reservoir characteristics of dolostones of the Ordovician Majiagou Group,Ordos,North China Platform[J]. Sedimentary Geology 1998,118:127-140
[115] John D. Humphrey. New geochemical support for mixing-zone dolomitization at Golden Grove, Barbados[J]. Journal of Sedimentary Research,2000,70(5):1160-1170
[116] Jay M. Gregg, Kevin L. Shelton, Aaron W. Johnson, et al. Dolomitization of the Waulsortian Limestone (Lower Carboniferous) in the Irish Midlands[J]. Sedimentology,2001,48:745-766
[117] S. Zeeh, T. Bechstadt, J. Mckenzie, et al. Diagenetic evolution of the Carnian Wetterstein platforms of the Eastern Alps[J]. Sedimentology, 1995,42:199-222
[118] F.Jerry Lucia. Rock-fabric/petrophysical ciassification of carbonate pore space for reservoir characterization[J]. AAPG Bulletin, 1995,79(9): 1275-1300
[119] Hairuo Qing, Eric W.Mountjoy. Formation of coarsely crystalline, hydrothermal dolomite reservoirs in the presqu'ile barrier, western Canada sedimentary basin[J].AAPG Bulletin,1994,78(1):55-77
[120] Avner Ayalon, FRED J.Longstaffe. Stable isotope evidence for the origin of diagenetic carbonate minerals from the lower Jurassic inmar formation, southern Israel [J]. Sedimentoology, 1995,42:147-160
[121] Tad M.Smrth, Steven L.Dorobek. Alteration of early-formed dolomite during shallow to deep burial: Mississippan Mission Canyon Formation, cent to southwestern Montana[J]. Geological Society of America Bulletin, 1993,105(10):1389-1399
[122] Guoqiu Gao, Lynton S.Land, Robert L.Folk. Meteoric modification of early dolomite and Late dolomitization by basinal fluids,Upper arbuckle group,Slick hills,Southwestern Oklahoma[J]. The American Association of Petrpleum Geologists Bulletin, 1992,76(11): 1649-1664
[123] J.Auajjar, J.Boulegue. Dolomitization pattern of the Liassic platform of the Tazekka Pb-Zn district,Taza, eastern Morocco: petrographic and geochemical study[J]. Journal of South American Earth Sciences,2003,16:167-178
[124] James R.Hein, Sarah C.Gray, Bruce M.Richmond et al. Dolomitization of Quaternary reef limestone, Aitutaki, Cook Islands[j]. Sedimentology,1992,39:645-661
[125] Leslie A.Melim, Peter A.Scholle. Dolomitization of the Capitan Formation forereef facies (Permian, west Texas and New Mexico):seepage reflux revisited[J]. Sedimentology, 2002, 49:1207-1227
[126] Jonathan Kaufman, Gilbert N. Hanson, William J.Meyers. Dolomitization of the Devonian Swan Hills Formation, Rosevear Field, Alberta,Canada[J]. Sedimentology,1991,38:41-66
[127] Ihsan S.AL-Aasm, Jeff Lonnee, Lulie Clarke. Multiple fluid flow events and the formation of saddle dolomitexase studies from the Middle Devonian of the Western Canada Sedimentary Sasin[J]. Marine and Petroleum Geology,2002,19:209-217
[128] Yongqiang Wu, Zhuodan Wu. Diagenetic modification of dolomite in middle Ordovician carbonates,Taiyuan City area,China[J]. Sedimentary Geology,1998,116:143-156
[129] CReinhold. Multiple episodes of dolomitization and dolomite recrystallization during shallow burial in Upper Jurassic shelf carbonates: easten Swabian Alb,southern Germany [J]. Sedimentary Geology, 1998,121:71-95
[130] Steven D.Hood, Campbell S.Nelson, Peter J.J.Kamp. Burial dolomitisation in a non-tropical carbonate petroleum reservoir: the Oligocene Tikorangi Formation, Taranaki Basin,New Zealand[J]. Sedimentary Geology,2004,172:117-138
[131] MJ.Mayayo, B.Bauluz, A.L6pez-Galindo, et al. Mineralogy and geochemistry of the carbonates in the Calatayud Basin(Zaragoz'a,Spain)[J]. Chemical Geology,1996,130,123-136
[132] Aada Teedumae, Heldur Nestor, Toivo Kallaste. Sedimentary cyclicity and dolomitization of the Raikkula Formation in the Nurme drill core(Silurian,Estonta)[J]. Proc. Estonian Acad. Sic. Geol.,2004,53(1):42-62
[133] Janos Haas, Attila Demeny. Early dolomitisation of Late Triassic platform carbonates in the Transdanubian Range(Hungary)[J]. Sedimentary Geology, 2002, 151:225-242
[134] Arthur H.Sailer, Clyde H.Moore, JR. Geochemistry of meteoric calcite cements in some Pleistocene limestones[J]. Sedimentology, 1991,38:601-621
[135] Hans GMachel. Recrystallization versus neomorphism, and the concept of 'significant recrystallization' in dolomite research[J]. Sedimentary Geology,1997,113:161-168
[136] M. Ziya Kirmaci, Kemal Akdag. Origin of dolomite in the Late Cretaceous-Paleocene limestone turbidites, Eastern Pontides, Turkey[J]. Sedimentary Geology ,2005,181:39-57
[137] R. Martinez-Ibarra, J. Tritlla, E. Cedillo-Pardo, et al. Brine and hydrocarbon evolution during the filling of the Cantarell Oil Field (Gulf of Mexico)[J]. Journal of Geochemical Exploration,2003, 78-79: 399-403
[138] W. Blendinger. Sea level changes versus hydrothermal diagenesis: origin of Triassic carbonate platform cycles in the dolomites, Italy[J]. Sedimentary Geology,2004,169:21-28
[139] Hans G Machel , Jeff Lonnee. Hydrothermal dolomite—a product of poor definition and imagination[J]. Sedimentary Geology ,2002,152: 163-171
[140] Gerhard Einsele. Sedimentary basins: evolution,facies and sediment budget(2nd)[M]. Berlin: Springer-Verlin. 2000.1-792
[141] B. Biju-Duval. Sedimentary Geology: sedimentary basins , depositional environments and petroleum formation[M]. Paris: Editions Technip. 2002. 1-642
[142] Malone, M.J., Baker,P.A.,Burns,S.J.. Recrystallization of dolomite: evidence from the Monterey formation(Miocene),California[J]. Sedimentology, 1994,41:1223-1239
[143] Arthur H.Saller, Kevin Lounsbury, Mark Birchard. Facies control on dolomitization and porosity in the Devonian Swan Hills Formation in the Rosevear area, west-central Alberta[J]. Bulletin of Canadian Petroleum Geology, 2001,49(4):458-471
[144] W.R. Wrighta, A.W. Johnsonb, K.L. Sheltonb,et al. Fluid migration and rock interactions during dolomitisation of the Dinantian Irish Midlands and Dublin Basin[J]. Journal of Geochemical Exploration, 2000,69-70:159-164
[145] T. Kurtis Kyser, Noelp Jamesi, Yvonne Bone. Shallow burial dolomitization and dedolomitization of Cenozoic cool-water limestones, southern Australia: geochemistry and origin [J]. Journal of Sedimentary Research, 2002,72(1):146-157
[146] David W. Morrow. Distribution of porosity and permeability in platform dolomites: Insight from the Permian of west Texas: Discussion[J]. AAPG Bulletin, 2001, 85(3): 525-529
[147] Liu Zaihua, Dreybrodt Wolfgang. Kinetics and rate-limiting mechanisms of dolomite dissolution at various CO2 partial pressures[J]. Science in China(Series B), 2001,44(5):500-509
[148] Douglas W. Kirkland, Rodger E. Denison, Melodye A. Rooney. Diagenetic alteration of Permian strata at oil field of south central Oklahoma,USA[J].Marine and Petroleum Geology, 1995,12(6):629-644
[149] M. T. Cioppa, I. S. Al-Aasm, D. T. A. Symons, et al. Dating penecontemporaneous dolomitization in carbonate reservoirs: Paleomagnetic, petrographic, and geochemical constraints[J]. AAPG Bulletin, 2003, 87(1):71-88
[2] 郝石生，贾振远．碳酸盐岩油气形成和分布[M]．北京：石油工业出版社．1989．1-401
[3] 曾允孚，夏文杰．沉积岩石学[M]．北京：地质出版社．1986．1-274
[4] 姜在兴．沉积学[M]．北京：石油工业出版社．2003．1-540
[5] 赵澄林．沉积学原理[M]．北京：石油工业出版社．2001．1-214
[6] 范嘉松．中国生物礁与油气[M]．北京：海洋出版社．1996．1-329
[7] F．K．诺斯．石油地质学[M]．北京：石油工业出版社．1994．1-582
[8] 冯增昭，彭永民，金振奎等．中国寒武纪和奥陶纪岩相古地理[M]．北京：石油工业出版社．2004．29-47
[9] 赵政璋，李永铁，叶和飞等．青藏高原羌塘盆地石油地质[M]．北京：科学出版社．2000．1-398
[10] 赵政璋，李永铁，叶和飞等．青藏高原中生界沉积相及油气储盖层特征[M]．北京：科学出版社．2000．1-347
[11] 方少仙，董兆雄，侯方浩等．层状白云岩储层特征与成因[M]．北京：地质出版社．1999．1-115
[12] 顾家裕，朱筱敏，贾进华等．塔里木盆地沉积与储层[M]．北京：石油工业出版社．2003．1-400
[13] 马永生，梅冥相，陈小兵等．碳酸盐岩储层沉积学[M]．北京：地质出版社．1999．1-364
[14] 刘岫峰．沉积岩实验室研究方法[M]．北京：地质出版社．1991．1-298
[15] 许怀先，陈丽华，万玉金等．石油地质实验测试技术与应用[M]．北京：石油工业出版社．2001．1-308
[16] 钱峥，黄先雄．碳酸盐岩成岩作用及储层—以中国四川东部石炭系为例[M]．北京：石油工业出版社．2000．1-119
[17] 王成善，伊海生，李勇等．西藏羌塘盆地地质演化与油气远景评价[M]．北京：地质出版社．2001．184—215
[18] H．G．里丁等．沉积环境和相[M]．北京：科学出版社．1985．222-390
[19] 赵政璋，李永铁，王岫岩，等．羌塘盆地南部海相侏罗系古油藏例析[J]．海相油气地质，2002，7(3)：34-36
[20] 伊海生，高春文，张小青，等．羌塘盆地双湖地区古油藏白云岩储层的显微成岩组构特征及意义[J]．成都理工大学学报，2004，31(6)：611-615
[21] 王成善，伊海生，刘池洋，等．西藏羌塘盆地古油藏发现及其与油气远景评价的意义[J]．石油与天然气地质，2004，25(2)：139-143
[22] 黄思静．上扬子地台区晚古生代海相碳酸盐岩的碳、锶同位素研究[J]．地质学报，1997，71(1)：45-53
[23] 黄思静，石和，毛晓东等．早古生代海相碳酸盐的成岩蚀变性及其对海水信息的保存[J]．成都理工大学学报，2003，30(1)：9-18[24] 郑荣才，刘文均，李祥辉等．白云岩成因在层序地层研究中的应用[J]．矿物岩石，1996，16(1)：28-37
[25] 田景春，陈洪德，侯明才等．右江盆地晚古生代白云岩与层序地层的关系及其储集性[J]．成都理工大学学报，2004，31(1)：34-39
[26] 杨华，付锁堂，马振芳，等．天环地区奥陶系白云岩储集体特征[J]．天然气工业，2004，24(9)：11-15．
[27] 李振宏，杨永恒．白云岩成因研究现状及进展[J]．油气地质与采收率，2005，12(2)：5-8
[28] 杨威，王清华，刘效曾．塔里木盆地和田河气田下奥陶统白云岩成因[J]．沉积学报，2000，18(4)：544-548
[29] 顾家裕．塔里木盆地下奥陶统白云岩特征及成因[J]．新疆石油地质，2000，21(2)：120-122
[30] 邵龙义，何宏，彭苏萍等．塔里木盆地巴楚隆起寒武系及奥陶系白云岩类型及形成机理[J]．古地理学报，2002，4(2)：19-30
[31] 朱井泉，李永铁．藏北羌塘盆地侏罗系白云岩类型、成因及油气储集特征[J]．古地理学报，2000，2(4)：30-42
[32] 杨桂芳，藤玉洪，卓胜广等．藏北羌塘盆地双湖地区油气成藏条件[J]．地质通报，2003，22(4)：285-289
[33] 魏国齐，杨威，张林等．川东北飞仙关组鲕滩储层白云石化成因模式[J]．天然气地球科学，2005，16(2)：162-166
[34] 张立强，纪友亮，李永铁．羌塘盆地侏罗系白云岩储层特征研究[J]．石油实验地质，2001，23(4)：384-389
[35] 张传禄，张永生，康祺发等．鄂尔多斯南部奥陶系马家沟群马六组白云岩成因[J]．石油学报，2001，22(3)：22-25
[36] 曾理，万茂霞，彭英．白云石有序度及其在石油地质中的应用[J]．天然气勘探与开发，2004，27(4)：64-66
[37] 贾振远，蔡忠贤．成岩地层学与层序地层学[J]．地球科学—中国地质大学学报，1997，22(5)：538-543
[38] 桑树勋，郑永飞，张华等．徐州地区下古生界碳酸盐岩的碳、氧同位素研究[J]．岩石学报，2004，20(3)：707-716
[39] 杨万容，杨长庚，沈建伟．湖南慈利晚二叠世长兴期珊瑚礁白云石化及其成岩环境[J]．地质学报，2002，76(1)：114-124
[40] 邓长瑜，张秀莲，陈建文等．黔东南地区寒武系碳酸盐岩成岩作用分析[J]．沉积学报，2004，22(4)：588-596
[41] 胡明毅，高振中，李建明．中上扬子区古生界深水斜坡及台地边缘碳酸盐岩成岩作用[J]．石油实验地质，1998，20(3)：239-247
[42] 张秀莲．碳酸盐岩中氧、碳稳定同位素与古盐度、古水温的关系[J]．沉积学报，1985，3(4)：17-29
[43] 何道清．碳酸盐岩碳、氧同位素分析激光微取样技术[J]西南石油学院学报，2003，25(1)：12-15
[44] 王英华．碳酸盐岩成岩作用与孔隙演化[J]．沉积学报，1992，10(3)：85-95
[45] 王剑，谭富文，李亚林等．青藏高原重点沉积盆地油气资源潜力分析[M]．北京：地质出版社．2004．1-317[46] 张小青，伊海生，朱迎堂．羌塘盆地双湖地区白云岩储集层特征研究[J]．西南石油学院学报，2005，27(5)：10-13．
[47] 何自新，杨奕华．鄂尔多斯盆地奥陶系储层图册[M]．北京：石油工业出版社．2004．1-244．
[48] 王剑，谭富文，王小龙等．藏北羌塘盆地早侏罗世—中侏罗世早期沉积构造特征[J]．沉积学报，2004，22(2)：198-206
[49] BT库兹涅左夫．地史上碳酸盐聚积演化的若干特点——白云石形成演化和碳酸盐聚积与全球地质环境的关系[J]．天然气地球科学，2002，13(1～2)：18-29
[50] 覃建雄，曾允孚．鄂尔多斯盆地东部下奥陶统白云岩地球化学研究[J]．矿物学报，1994，14(1)：22-32
[51] 姜月华，岳文浙，柳祖汉等．湖南晚二叠世生物礁成岩作用的碳、氧同位素研究[J]．地质论评，2000，46(2)：190-197
[52] 郑永飞，徐宝龙，周根陶．矿物稳定同位素地球化学研究[J]．地学前缘，2000，7(2)：299-321
[53] 许建华，侯中昊，王金友等．羌塘盆地流体包裹体特征及其在储层成岩研究中的应用[J]．石油实验地质，2003，25(1)：81-87
[54] 罗建宁，朱忠发，谢渊等．羌塘盆地生物礁岩特征与沉积模式[J]．沉积与特提斯地质，2004，24(2)：51-63
[55] 谭富文，王剑，王小龙等．羌塘盆地雁石坪地区中—晚侏罗世碳、氧同位素特征与沉积环境分析[J]．地球学报，2004，25(2)：119-126
[56] 彭军，田景春．陕甘宁盆地中部气田中区马五段白云岩成因类型及其地球化学特征[J]．矿物岩石，1998，18(2)：35-39
[57] 朱井泉．上扬子台地三叠系碳酸盐岩中的特形白云石及其指相意义初探[J]．岩相古地理，1996，16(4)：32-40
[58] 钟建华，温志峰，李勇等．生物礁的研究现状与发展趋势[J]．地质评论，2005，51(3)：288-301
[59] 范嘉松．世界碳酸盐岩油气田的储层特征及其成藏的主要控制因素[J]．地学前缘，2005，12(3)：23-31
[60] 李红亮，汪华，史习杰．四川盆地川东地区上二叠统礁白云石的类型及其特征[J]．天然气勘探与开发，1999，22(3)：25-30
[61] 王志兴，张帆，马青等．四川盆地东部晚二叠世—早三叠世飞仙关期礁、滩特征与海平面变化[J]．沉积学报，2002，20(2)：249-255
[62] 何幼斌，冯增昭．四川盆地及其周缘下二叠统细—粗晶白云岩成因探讨[J]．江汉石油学院学报，1996，18(4)：15-21
[63] 胡恒，陈景山．塔北地区下奥陶统碳酸盐岩成岩作用及孔隙演化[J]．成都理工学院学报(增刊)，1996，23：104-111
[64] 郭建华，沈昭国，李建明．塔北东段下奥陶统白云石化作用[J]．石油与天然气地质，1994，15(1)：51-60
[65] 艾华国，兰林英，张克银．塔里木盆地不整合面下的碳酸盐岩成岩作用及孔隙特征[J]．新疆石油地质，1998，19(2)：112-122
[66] 杨威，王清华，刘效曾．塔里木盆地和田河气田下奥陶统白云岩成因[J]．沉积学报，2000，18(4)：544-549
[67] 蒋凌志，于德龙．塔里木盆地麦盖提斜坡石炭系生屑灰岩段储层特征研究[J]．北京大学学??报(自然科学版)，2003，39(3)：428-435
[68] 沈昭国，陈永武，郭建华．塔里木盆地下古生界白云石化成因机理及模式探讨[J]．新疆石油地质，1995，16(4)：319-325
[69] 王志兴，王振宇，马青等．塔里木盆地中部生物屑灰岩段滩体特征及储集性[J]．石油与天然气地质，2002，23(1)：58-64
[70] 翟永红，王泽中，王正允等．塔中1井储层段岩石学特征集成岩作用[J]．西安地质学报，1994，16(3)：38-46
[71] 王嗣敏，吕修祥．塔中地区奥陶系碳酸盐岩储层特征及其油气意义[J]．西安石油大学学报(自然科学版)，2004，19(7)：72-78
[72] 翟永红，郭建华，刘生国．塔中地区石炭系碳酸盐岩成岩作用与储层评价[J]．江汉石油学院学报，1995，17(3)：13-19
[73] 周根陶，郑永飞．碳酸钙—水体系氧同位素分馏系数的低温实验研究[J]．地学前缘，2000，7(2)：320-338
[74] 郑永飞，周根陶，龚冰．碳酸盐矿物氧同位素分馏的理论研究[J]．高校地质学报，1997，3(3)：241-256
[75] 李双应，金福全，王道轩．碳酸盐岩成岩作用的微量元素地球化学特征[J]．石油实验地质，1995，17(1)：55-64
[76] 杨威，王清华，赵仁德等．碳酸盐岩成岩作用及其对储层控制的定量评价[J]．地球学报，2001，22(5)：441-447
[77] 陈方鸿，谢庆斌，王贵文．碳酸盐岩成岩作用与层序地层学关系研究——以鄂尔多斯盆地寒武系为例[J]．岩相古地理，1999，19(1)：20-25
[78] 杨华，付锁堂，马振芳等．天环地区奥陶系白云岩储集体特征[J]．天然气工业，2004，24(9)：11-17
[79] 杜学斌，张成，张彩明．稳定同位素地球化学在盆地流体分析中的应用现状及发展前景[J]．油气地质与采收率，2005，12(4)：20-25
[80] 陈学时，周进高．下扬子区寒武纪斜坡—盆地相沉积的成岩作用及储集类型[J]．石油与天然气地质，1994，15(1)：70-82
[81] 朱莲芳．中国天然气碳酸盐岩储层形成的成岩模式[J]．沉积学报，1995，13(2)：140-149
[82] 胡明毅，朱忠德，郭成贤．中扬子地区海相碳酸盐岩储层类型和特征[J]．石油勘探与开发，1994，21(1)：106-115
[83] 梁百和，朱素琳，刘英霞等．中扬子晚石炭世碳酸盐岩的成岩作用[J]．中山大学学报(自然科学版)，1996，35(2)：106-112
[84] 翟永红，郭成贤，郭建华等．中扬子台地北缘灯影组白云岩研究[J]．矿物岩石，1996，16(3)：36-42
[85] 翟永红，郭成贤．中扬子台地北缘灯影组碳酸盐岩成岩作用序列集成岩模式[J]．地质地球化学，1997，(2)：45-52
[86] Denis Lavoie, Guoxiang Chi. The Lower Silurian Sayabec Formation in northern Gaspe:carbonate diagenesis and reservoir potential[J]. Bulletin of Canadian Petroleum Geology,2001,49,(2):282-298
[87] Michael W.Rasser, Alois Ferminger. Paleoenvirortmental and diagenetic implications of δ 180and δ 13C isotpe ratios from the Upper Jurassic Piassen limestone(Northern Calcareous Alps,Austria)[J].Geobios,2002,35:41-49
[88] Achour Madi, Martine M. Savard, Pierre-Andre Bourque, et al. Hydrocarbon potential of the Mississippian carbonate platform, Bechar basin, Algerian Sahara[J]. AAPG Bulletin, 2000,84(2):266-287
[89] Ihsan S. Al-Aasm, Karem K. Azmy. Diagenesis and evolution of microporosity of Middle-Upper Devonian Kee scarp reefs, Norman wells, Northwest territories, Canada: petrographic and chemical evidence[J]. AAPG Bulletin,1996,80(1):82-l00
[90] Robert E. Woody, Jay M. Gregg, Leonard F. Koederitz. Effect of texture on petrophysical properties of dolomite: evidence from the Cambrian-Ordovician of Southeastern Missouri[J]. AAPG Bulletin, 1996,80(1):119-132
[91] Jeff Lonnee, Ihsan S.Al-Aasm. Dolomitization and fluid evolution in the Middle Devonian Sulphur Point Formation, Rainbow South Field, Alberta: petrographic and geochemical evidence[J]. Bulletin of Canadian Petroleum Geology,2000,48(3):262-283
[92] Huang Sijing, Xiao Linping, Yang Junjie et al. Experimental Simulation of Dolomite Dissolution Under Burial Diagenesis Conditions and Thermodynamic Interpretation[J]. Chinese Journal of geochemistry,2000,19(1) :58-65
[93] Esref Atabey. Peirography and origin of dolomites of yaniktepe formation (upper cretaceous) in gurun autochthonous, eastern Taurus turkey[J]. Mineral Res.Expl.Bull., 1995,117:59-67
[94] Scott Durocher, Ihsan S. Al-Aasm. Dolomitization and Neomorphism of Mississippian (Visean) Upper Debolt Formation, Blueberry field, Northeastern British Columbia: geologic, petrologic, and chemical evidence[J]. AAPG Bulletin,1997,81(6):954-977
[95] F. Jerry Lucia. Rock-fabric/petrophysical classification of carbonate pore space for reservoir characterization[J]. AAPG Bulletin,1995,79(9):1275-1300
[96] Eric W. Mountjoy, Xiomara M. Marquez. Predicting reservoir properties in dolomites: Upper Devonian Leduc Buildups, deep Alberta basin[J]. AAPG Memoir, 1997, 69:267-306
[97] Piere-Andre Bourque, Martine M. Savard, Guoxiang Chi, et al. Diagenesis and porosity evolution of the Upper Silurian-Lowermost Devonian West Point reef limestone, eastern Gaspe Belt, Quebec Appalachians[J]. Bulletin of Canadian Petroleum Geology,2001,49(2):299-326
[98] Denis Lavoie, Guoxiang Chi. The Lower Silurian Sayabec Formation in northern Gaspe: carbonate diagenesis and reservoir potential[J]. Bulletin of Canadian Petroleum Geology,2001,49(2):282-298
[99] Herbert Th. Eichenseer, Frederic R. Walgenwitz, Patrick J. Biondi. Stratigraphic control on facies and diagenesis of dolomitized oolitic siliciclastic ramp sequences (Pinda Group, Albian, Offshore Angola)[J]. AAPG Bulletin, 1999,83(11):1729-1758
[100] Maurice E. Tucker. Sedimentary Petrology (3rd Edition) [M]. Oxford: Blackwell Science. 2001.1-262
[101] Moss,S.J,,Tucker, M.E. Dolomitisation associated with transgressive surfaces: a mid-Cretaceous example[J]. Sedimentary Geology, 1996,107:11-20
[102] Hans G Machel, Jeff Lonnee. Hydrothermal dolomite—a product of poor definition and
imagination[J]. Sedimentary Geology,2002,152:163-171
[103] Fred J.Longstaffe, Ran Calvo, Avner Ayalon et al. Stable isotope evidence for multiple fluid regimes during carbonate cementation of the Upper Tertiary Hazeva Formation,Dead Sea Graben, southerm Israel[J]. Journal of Geochemical Exploration,2003,80:151-170
[104] Reinhold R.Leinfelder, Stuttgart. Upper Jurassic reef types and controlling factors[J]. Stuttgart, 1993,19(5): 1-45
[105] M.Boni, G.Parente, T.Bechstadt et al. Hydrothermal dolomites in SW Sardinia (Italy): evidence for a widespread late-Variscan fluid flow event[J]. Sedimentary Geology,2000,131:181-200
[106] M. Esteban, C. Taberner. Secondary porosity development during late burial in carbonate reservoirs as a result of mixing and/or cooling of brines[J]. Journal of Geochemical Exploration,2003,78- 79:355- 359
[107] A. Torok. Formation of dolomite mottling in Middle Triassic ramp carbonates (Southern Hungary)[J]. Sedimentary Geology,2000,131:131-145
[108] Hairuo Qing. Petrography and geochemistry of early-stage, fine and medium-crystalline dolomites in the Middle Devonian Presqu'ile Barrier at Pine Point,Canada[J]. Sedimentology, 1998,45:433-446
[109] Joachim E. Amthor, Gerald M. Friedman. Dolomite-rock textures and secondary porosity development in Ellenburger Group Carbonate (Lower Ordovician), west Texas and southeastern New Mexico[J]. Sedimentology, 1991,38:343-362
[110] Fadi H. Nader, Rudy Swennen. Petroleum prospects of Lebanon: some remarks from sedimentological and diagenetic studies of Jurassic carbonates[J]. Marine and Petroleum Geology ,2004,21: 427-441.
[111] John Warren. Dolomite: occurrence, evolution and economically important associations[J]. Earth-Science,2000,52:1 -81
[112] Alex MacNeil, Brian Jones. Dolomitization of the Pedro Castle Formation (Pliocene), Cayman Brac, British West Indies[J].Sedimentary Geology 2003,162:219-238
[113] Leslie A.Melim, Peter A.Scholle. Dolomitization of the Capitan Formation forereef facies (Permian, west Texas and New Mexico): seepage reflux revisited [J]. Sedimentology, 2002,49:1207-1227
[114] Feng Zengzhao, Zhang Yongsheng, Jin Zhenkui. Type ,origin and reservoir characteristics of dolostones of the Ordovician Majiagou Group,Ordos,North China Platform[J]. Sedimentary Geology 1998,118:127-140
[115] John D. Humphrey. New geochemical support for mixing-zone dolomitization at Golden Grove, Barbados[J]. Journal of Sedimentary Research,2000,70(5):1160-1170
[116] Jay M. Gregg, Kevin L. Shelton, Aaron W. Johnson, et al. Dolomitization of the Waulsortian Limestone (Lower Carboniferous) in the Irish Midlands[J]. Sedimentology,2001,48:745-766
[117] S. Zeeh, T. Bechstadt, J. Mckenzie, et al. Diagenetic evolution of the Carnian Wetterstein platforms of the Eastern Alps[J]. Sedimentology, 1995,42:199-222
[118] F.Jerry Lucia. Rock-fabric/petrophysical ciassification of carbonate pore space for reservoir characterization[J]. AAPG Bulletin, 1995,79(9): 1275-1300
[119] Hairuo Qing, Eric W.Mountjoy. Formation of coarsely crystalline, hydrothermal dolomite reservoirs in the presqu'ile barrier, western Canada sedimentary basin[J].AAPG Bulletin,1994,78(1):55-77
[120] Avner Ayalon, FRED J.Longstaffe. Stable isotope evidence for the origin of diagenetic carbonate minerals from the lower Jurassic inmar formation, southern Israel [J]. Sedimentoology, 1995,42:147-160
[121] Tad M.Smrth, Steven L.Dorobek. Alteration of early-formed dolomite during shallow to deep burial: Mississippan Mission Canyon Formation, cent to southwestern Montana[J]. Geological Society of America Bulletin, 1993,105(10):1389-1399
[122] Guoqiu Gao, Lynton S.Land, Robert L.Folk. Meteoric modification of early dolomite and Late dolomitization by basinal fluids,Upper arbuckle group,Slick hills,Southwestern Oklahoma[J]. The American Association of Petrpleum Geologists Bulletin, 1992,76(11): 1649-1664
[123] J.Auajjar, J.Boulegue. Dolomitization pattern of the Liassic platform of the Tazekka Pb-Zn district,Taza, eastern Morocco: petrographic and geochemical study[J]. Journal of South American Earth Sciences,2003,16:167-178
[124] James R.Hein, Sarah C.Gray, Bruce M.Richmond et al. Dolomitization of Quaternary reef limestone, Aitutaki, Cook Islands[j]. Sedimentology,1992,39:645-661
[125] Leslie A.Melim, Peter A.Scholle. Dolomitization of the Capitan Formation forereef facies (Permian, west Texas and New Mexico):seepage reflux revisited[J]. Sedimentology, 2002, 49:1207-1227
[126] Jonathan Kaufman, Gilbert N. Hanson, William J.Meyers. Dolomitization of the Devonian Swan Hills Formation, Rosevear Field, Alberta,Canada[J]. Sedimentology,1991,38:41-66
[127] Ihsan S.AL-Aasm, Jeff Lonnee, Lulie Clarke. Multiple fluid flow events and the formation of saddle dolomitexase studies from the Middle Devonian of the Western Canada Sedimentary Sasin[J]. Marine and Petroleum Geology,2002,19:209-217
[128] Yongqiang Wu, Zhuodan Wu. Diagenetic modification of dolomite in middle Ordovician carbonates,Taiyuan City area,China[J]. Sedimentary Geology,1998,116:143-156
[129] CReinhold. Multiple episodes of dolomitization and dolomite recrystallization during shallow burial in Upper Jurassic shelf carbonates: easten Swabian Alb,southern Germany [J]. Sedimentary Geology, 1998,121:71-95
[130] Steven D.Hood, Campbell S.Nelson, Peter J.J.Kamp. Burial dolomitisation in a non-tropical carbonate petroleum reservoir: the Oligocene Tikorangi Formation, Taranaki Basin,New Zealand[J]. Sedimentary Geology,2004,172:117-138
[131] MJ.Mayayo, B.Bauluz, A.L6pez-Galindo, et al. Mineralogy and geochemistry of the carbonates in the Calatayud Basin(Zaragoz'a,Spain)[J]. Chemical Geology,1996,130,123-136
[132] Aada Teedumae, Heldur Nestor, Toivo Kallaste. Sedimentary cyclicity and dolomitization of the Raikkula Formation in the Nurme drill core(Silurian,Estonta)[J]. Proc. Estonian Acad. Sic. Geol.,2004,53(1):42-62
[133] Janos Haas, Attila Demeny. Early dolomitisation of Late Triassic platform carbonates in the Transdanubian Range(Hungary)[J]. Sedimentary Geology, 2002, 151:225-242
[134] Arthur H.Sailer, Clyde H.Moore, JR. Geochemistry of meteoric calcite cements in some Pleistocene limestones[J]. Sedimentology, 1991,38:601-621
[135] Hans GMachel. Recrystallization versus neomorphism, and the concept of 'significant recrystallization' in dolomite research[J]. Sedimentary Geology,1997,113:161-168
[136] M. Ziya Kirmaci, Kemal Akdag. Origin of dolomite in the Late Cretaceous-Paleocene limestone turbidites, Eastern Pontides, Turkey[J]. Sedimentary Geology ,2005,181:39-57
[137] R. Martinez-Ibarra, J. Tritlla, E. Cedillo-Pardo, et al. Brine and hydrocarbon evolution during the filling of the Cantarell Oil Field (Gulf of Mexico)[J]. Journal of Geochemical Exploration,2003, 78-79: 399-403
[138] W. Blendinger. Sea level changes versus hydrothermal diagenesis: origin of Triassic carbonate platform cycles in the dolomites, Italy[J]. Sedimentary Geology,2004,169:21-28
[139] Hans G Machel , Jeff Lonnee. Hydrothermal dolomite—a product of poor definition and imagination[J]. Sedimentary Geology ,2002,152: 163-171
[140] Gerhard Einsele. Sedimentary basins: evolution,facies and sediment budget(2nd)[M]. Berlin: Springer-Verlin. 2000.1-792
[141] B. Biju-Duval. Sedimentary Geology: sedimentary basins , depositional environments and petroleum formation[M]. Paris: Editions Technip. 2002. 1-642
[142] Malone, M.J., Baker,P.A.,Burns,S.J.. Recrystallization of dolomite: evidence from the Monterey formation(Miocene),California[J]. Sedimentology, 1994,41:1223-1239
[143] Arthur H.Saller, Kevin Lounsbury, Mark Birchard. Facies control on dolomitization and porosity in the Devonian Swan Hills Formation in the Rosevear area, west-central Alberta[J]. Bulletin of Canadian Petroleum Geology, 2001,49(4):458-471
[144] W.R. Wrighta, A.W. Johnsonb, K.L. Sheltonb,et al. Fluid migration and rock interactions during dolomitisation of the Dinantian Irish Midlands and Dublin Basin[J]. Journal of Geochemical Exploration, 2000,69-70:159-164
[145] T. Kurtis Kyser, Noelp Jamesi, Yvonne Bone. Shallow burial dolomitization and dedolomitization of Cenozoic cool-water limestones, southern Australia: geochemistry and origin [J]. Journal of Sedimentary Research, 2002,72(1):146-157
[146] David W. Morrow. Distribution of porosity and permeability in platform dolomites: Insight from the Permian of west Texas: Discussion[J]. AAPG Bulletin, 2001, 85(3): 525-529
[147] Liu Zaihua, Dreybrodt Wolfgang. Kinetics and rate-limiting mechanisms of dolomite dissolution at various CO2 partial pressures[J]. Science in China(Series B), 2001,44(5):500-509
[148] Douglas W. Kirkland, Rodger E. Denison, Melodye A. Rooney. Diagenetic alteration of Permian strata at oil field of south central Oklahoma,USA[J].Marine and Petroleum Geology, 1995,12(6):629-644
[149] M. T. Cioppa, I. S. Al-Aasm, D. T. A. Symons, et al. Dating penecontemporaneous dolomitization in carbonate reservoirs: Paleomagnetic, petrographic, and geochemical constraints[J]. AAPG Bulletin, 2003, 87(1):71-88
© 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 |