多期次构造运动对不同物源成分砂岩控制作用

doi:10.11885/j.issn.1674-5086.2020.01.09.03

西南石油大学学报(自然科学版) ›› 2022, Vol. 44 ›› Issue (1): 27-40.DOI: 10.11885/j.issn.1674-5086.2020.01.09.03

多期次构造运动对不同物源成分砂岩控制作用

王爱¹, 钟大康^2,3, 王威⁴, 周志恒^2,3, 唐自成^2,3

1. 中国石化石油勘探开发研究院，北京海淀 100083;
2. 中国石油大学（北京）地球科学学院，北京昌平 102249;
3. 中国石油大学（北京）油气资源与探测国家重点实验室，北京昌平 102249;
4. 中国石化勘探分公司，四川成都 610041

收稿日期:2020-01-09 发布日期:2022-01-25
通讯作者: 钟大康，E-mail：zhongdakang@263.net
作者简介:王爱，1989年生，男，汉族，湖南衡阳人，博士，主要从事岩石学和储层地质学等方面的研究工作。E-mail：wangai.syky@sinopec.com;
钟大康，1961年生，男，汉族，四川资中人，教授，博士生导师，主要从事储层地质学及沉积学方面的教学及研究。E-mail：zhongdakang@263.net;
王威，1980年生，男，汉族，江苏徐州人，高级工程师，博士，主要从事储层评价与油气成藏方面的研究。E-mail：wangw.ktnf@sinopec.com;
周志恒，1994年生，男，汉族，山东东营人，硕士研究生，主要从事岩石学和储层地质学等方面的研究。E-mail：zzh3400learner@qq.com;
唐自成，1993年生，男，汉族，重庆大足人，硕士研究生，主要从事储层地质学方面的研究工作。E-mail：chengzitang112207@163.com
基金资助:
国家科技重大专项（2016ZX05002004 -011）; 中国石油化工股份有限公司科技部项目（P19012-2）

Controls of Multi-stage Tectonic Movement on Sandstones with Different Provenances

WANG Ai¹, ZHONG Dakang^2,3, WANG Wei⁴, ZHOU Zhiheng^2,3, TANG Zicheng^2,3

1. Petroleum Exploration and Production Research Institute, SINOPEC, Haidian, Beijing 100083, China;
2. College of Geosciences, China University of Petroleum, Changping, Beijing 102249, China;
3. State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum, Changping, Beijing 102249, China;
4. SINOPEC Exploration Company, Chengdu, Sichuan 610041, China

Received:2020-01-09 Published:2022-01-25

摘要/Abstract

摘要： 通过普通岩石薄片和孔隙铸体薄片观察、扫描电镜、阴极发光和X衍射分析及压汞实验等手段，对川东北地区须家河组致密砂岩储层的岩石学特征、成岩作用、物性特征及孔隙类型和孔隙演化等方面进行分析，进而研究多期次构造运动对不同物源成分砂岩的控制作用。结果表明，印支晚期，研究区盆缘造山活动的强弱控制了须家河组物源供给和物源区母岩类型的差异，形成了不同类型的砂岩，包括元坝西须二段岩屑砂岩、元坝西须三段钙屑砂岩、巴中须四段长石岩屑砂岩、马路背须家河组石英砂岩和岩屑砂岩。在燕山运动和喜马拉雅运动的持续影响下，从大巴山前陆挤压带向盆地内由近及远依次发育马路背强变形区、巴中中等变形区和元坝西弱变形区，不同构造部位不同类型砂岩经历了不同的成岩序列和孔隙演化过程。构造部位控制了构造挤压强弱与裂缝及断层发育程度及规模，进而决定了原始孔隙与后期溶蚀孔隙保存程度以及孔隙的连通性，也控制了源储关系与油气充注程度，最终控制天然气产能。

关键词: 构造运动, 物源, 产能, 致密砂岩, 须家河组

Abstract: Based on ordinary thin sections and pore casting thin section observation, scanning electron microscopy, cathodoluminescence and X-ray diffraction analysis as well as mercury intrusion experiments, this thesis analysis the petrological characteristics, diagenesis, physical properties, pore types and pore evolution of the tight sandstone reservoirs of the Xujiahe Formation in the northeastern Sichuan Basin, furthermore studies the control effect of multi-stage tectonic movement on sandstones with different provenances. The results show that in the late Indosinian period, the difference in provenance supply and the type of parent rock of source area caused by the strength of the basin-forming orogenic activities in the study area resulted in different types of sandstone, which were described before, including the lithic sandstone of the Xu-2 tight sandstones, the calcarenaceous sandstone of the Xu-3 tight sandstones, the feldspathic lithic sandstone of the Xu-4 tight sandstones, and the quartz sandstone with lithic sandstone of the Xujiahe Formation in three area (western Yuanba Area, Bazhong Area, Malubei Area), respectively. Under the continuous influence of Yanshan Movement and Xishan Movement, Malubei strong deformation zone, Bazhong medium deformation zone and western Yuanba weak deformation zone are developed from near to far from the Daba Mountain foreland compressive zone. Different types of sandstones in different tectonic locations have experienced different diagenetic sequences and porosity evolution processes. The tectonic action controls the structural extrusion strength, and crack and fault development degree and scale, which further determines the preservation of the original pores and the later dissolution pores and the connectivity of the pores. It also controls the source-storage relationship and the degree of oil and gas charging, and ultimately controls natural gas yield.

Key words: tectonic movement, provenances, gas yield, tight sandstones, Xujiahe Formation

中图分类号:

TE122

王爱, 钟大康, 王威, 周志恒, 唐自成. 多期次构造运动对不同物源成分砂岩控制作用[J]. 西南石油大学学报(自然科学版), 2022, 44(1): 27-40.

WANG Ai, ZHONG Dakang, WANG Wei, ZHOU Zhiheng, TANG Zicheng. Controls of Multi-stage Tectonic Movement on Sandstones with Different Provenances[J]. Journal of Southwest Petroleum University(Science & Technology Edition), 2022, 44(1): 27-40.

0
/ / 推荐

导出引用管理器 EndNote|Ris|BibTeX

链接本文: http://journal15.magtechjournal.com/Jwk_xnzk/CN/10.11885/j.issn.1674-5086.2020.01.09.03

http://journal15.magtechjournal.com/Jwk_xnzk/CN/Y2022/V44/I1/27

参考文献

[1] ZOU Caineng, TAO Shizhen, HOU Lianhua, et al. Unconventional petroleum geology[M]. Beijing: Geological Publishing House, 2011: 50-83. 邹才能, 陶士振, 侯连华, 等. 非常规油气地质[M]. 北京: 地质出版社, 2011: 50-83.
[2] JIA Chengzao, ZHENG Min, ZHANG Yongfeng. Unconventional hydrocarbon resources in China and the prospect of exploration and development[J]. Petroleum Exploration and Development, 2012, 39(2): 129-136. 贾承造, 郑民, 张永峰. 中国非常规油气资源与勘探开发前景[J]. 石油勘探与开发, 2012, 39(2): 129-136.
[3] ZOU Caineng, ZHU Rukai, WU Songtao, et al. Types, characteristics, genesis and prospects of conventional and unconventional hydrocarbon accumulations: Taking tight oil and tight gas in China as an instance[J]. Acta Petrolei Sinica, 2012, 33(2): 173-187. doi: 10.7623/syxb201202001 邹才能, 朱如凯, 吴松涛, 等. 常规与非常规油气聚集类型、特征、机理及展望——以中国致密油和致密气为例[J]. 石油学报, 2012, 33(2): 173-187. doi:10.7623/syxb201202001
[4] WEI Guoqi, LI Jun, SHE Yuanqi, et al. Distribution laws of large gas fields and further exploration orientation and targets in China[J]. Natural Gas Industry, 2018, 38(4): 12-25. doi: 10.3787/j.issn.1000-0976.2018.04.002 魏国齐, 李君, 佘源琦, 等. 中国大型气田的分布规律及下一步勘探方向[J]. 天然气工业, 2018, 38(4): 12-25. doi:10.3787/j.issn.1000-0976.2018.04.002
[5] WANG Wei, YUE Quanling. Genetic mechanisms for tight sandstone reservoir of Xujiahe Formation, northern Sichuan Basin[J]. Natural Gas Exploration and Development, 2012, 35(1): 13-17. doi: 10.3969/j.issn.1673-3177.2012.01.003 王威, 岳全玲. 四川盆地北部须家河组致密砂岩储层成因机制[J]. 天然气勘探与开发, 2012, 35(1): 13-17. doi:10.3969/j.issn.1673-3177.2012.01.003
[6] WANG Wei. High efficient reservoir accumulation models of natural gas of Xujiahe Formation in northeast Sichuan Basin[J]. Lithologic Reservoirs, 2018, 30(3): 27-34. doi: 10.12108/yxyqc.20180304 王威. 川东北地区须家河组天然气高效成藏模式探讨[J]. 岩性油气藏, 2018, 30(3): 27-34. doi:10.12108/yxyqc.20180304
[7] DAN Yong. Analyses of the provenance and the depositional systems of Xujiahe Formation in northeast of Sichuan Basin[D]. Chengdu: Chengdu University of Technology, 2011. 淡永. 川东北须家河组物源分析与沉积体系研究[D]. 成都: 成都理工大学, 2011.
[8] CHENG Lixue, WANG Wei, WANG Tao. Reasons for the productivity difference of quartz sandstone gas reservoirs of Upper Triassic Xu 2 Member between Yuanba and Malubei areas in NE Sichuan Basin[J]. Natural Gas Industry, 2017, 37(8): 14-21. doi: 10.3787/j.issn.1000-0976.2017.08.002 程立雪, 王威, 王涛. 川东北元坝、马路背地区上三叠统须二段石英砂岩储层天然气产能差异的原因[J]. 天然气工业, 2017, 37(8): 14-21. doi:10.3787/j.issn.1000-0976.2017.08.002
[9] XIAO Kaihua, LI Hongtao, JIA Shuang. Characteristics of calcarenaceous sandstone reservoirs and gas accumulation control factors of the 3rd Member of Xujiahe Formation in Yuanba Area, northeast Sichuan Basin[J]. Oil and Gas Geology, 2014, 35(5): 654-660. doi: 10.11743/ogg20140510 肖开华, 李宏涛, 贾爽. 川东北元坝地区须三段钙屑砂岩储层特征及控气因素[J]. 石油与天然气地质, 2014, 35(5): 654-660. doi:10.11743/ogg20140510
[10] DU Hongquan, WANG Wei, ZHOU Xia, et al. Reservoir characteristics and main controlling factors of calcareous coarse clastic rocks of the third Member of Xujiahe Formation in Yuanba Area, northeastern Sichuan Basin[J]. Oil and Gas Geology, 2016, 37(4): 565-571. doi: 10.11743/ogg20160413 杜红权, 王威, 周霞, 等. 川东北元坝地区须三段钙屑砂砾岩储层特征及控制因素[J]. 石油与天然气地质, 2016, 37(4): 565-571. doi:10.11743/ogg20160413
[11] PAN Lei, SHEN Jishan, HAO Jingyu. Provenance types and controlling factors of the 4th Member of the Xujiahe Formation in the Yuanba Tongnanba Area, northeastern Sichuan[J]. Sedimentary Geology and Tethyan Geology, 2016, 36(1): 104-108. 潘磊, 申继山, 郝景宇. 川东北元坝通南巴地区须四段储层物源类型及主控因素分析[J]. 沉积与特提斯地质, 2016, 36(1): 104-108.
[12] LI Jun, HU Dongfeng, ZOU Huayao, et al. Coupling relationship between reservoir diagenesis and gas accumulation in Xujiahe Formation of Yuanba-Tongnanba Area, Sichuan Basin, China[J]. Natural Gas Geoscience, 2016, 27(7): 1164-1178. doi: 10.11764/j.issn.1672-1926.2016.07.1164 李军, 胡东风, 邹华耀, 等. 四川盆地元坝——通南巴地区须家河组致密砂岩储层成岩-成藏耦合关系[J]. 天然气地球科学, 2016, 27(7): 1164-1178. doi:10.11764/j.issn.1672-1926.2016.07.1164
[13] CHEN Longbo, HE Dengfa, WANG Bei, et al. Dating the tectonic deformation since the middle Triassic for the Tongnanba Anticline in the northeastern Sichuan Basin and its geological implications[J]. Geotectonica et Metallogenia, 2017, 41(3): 433-445. doi: 10.16539/j.ddgzyckx.2017.03.001 陈龙博, 何登发, 王贝, 等. 川东北地区通南巴背斜中三叠世以来构造变形时间厘定及其地质意义[J]. 大地构造与成矿学, 2017, 41(3): 433-445. doi:10.16539/j.ddgzyckx.2017.03.001
[14] LIU Shu, REN Xingguo, YAO Shengxian, et al. Relationship between gas reservoir distribution and structural system of Upper Triassic Xujiahe Formation in the Sichuan Basin[J]. Natural Gas Industry, 2018, 38(11): 1-14. doi: 10.3787/j.issn.1000-0976.2018.11.001 刘殊, 任兴国, 姚声贤, 等. 四川盆地上三叠统须家河组气藏分布与构造体系的关系[J]. 天然气工业, 2018, 38(11): 1-14. doi:10.3787/j.issn.1000-0976.2018.11.001
[15] ENKELMANN E, RATSCHBACHER L, JONCKHEERE R, et al. Cenozoic exhumation and deformation of northeastern Tibet and the Qinling: Is Tibetan lower crustal flow diverging around the Sichuan Basin?[J]. Geological Society of America Bulletin, 2006, 118(5-6): 651-671. doi: 10.1130/B25805.1
[16] YIN An, HARRISON T M. Geologic evolution of the Himalayan–Tibetan Orogen[J]. Annual Review of Earth and Planetary Sciences, 2000, 28: 211-280. doi: 10.1146/annurev.earth.28.1.211
[17] TIAN Yuntao, KOHN B P, ZHU Chuanqing, et al. Post-orogenic evolution of the Mesozoic Micangshan Foreland Basin system, central China[J]. Basin Research, 2012, 24(1): 70-90. doi: 10.1111/j.1365-2117.2011.00516.x
[18] TIAN Yuntao, QIU Nansheng, KOHN B P, et al. Detrital zircon(U–Th)/He thermochronometry of the Mesozoic Dabashan Foreland Basin, central China: Evidence for timing of post-orogenic denudation[J]. Tectonophysics, 2012, (570-571): 65-77. doi: 10.1016/j.tecto.2012.08.010
[19] TAN Lei, LIU Hong, TANG Yuzhe, et al. Characteristics and Mechanism of Upper Permian reef reservoirs in the Eastern Longgang Area, northeastern Sichuan Basin, China[J]. Petroleum, 2020, 6(2): 130-137. doi: 10.1016/j.petlm.2019.06.008
[20] ZHANG Feng. Study on sequence-lithofacies paleogeography of the Xujiahe Formation of Upper Triassic in northeast of Sichuan Basin[D]. Chengdu: Chengdu University of Technology, 2011. 张峰. 川东北地区上三叠统须家河组层序岩相古地理研究[D]. 成都: 成都理工大学, 2011.
[21] ZHAO Zongju, ZHU Yan, LI Dacheng, et al. Control affect of tectonic deformation to oil-gas pools in southern China[J]. Oil and Gas Geology, 2002, 23(1): 19-25. 赵宗举, 朱琰, 李大成, 等. 中国南方构造形变对油气藏的控制作用[J]. 石油与天然气地质, 2002, 23(1): 19-25.
[22] TAN X, XIA Q, CHEN J, et al. Basin-scale sand deposition in the Upper Triassic Xujiahe Formation of the Sichuan Basin, southwest China: Sedimentary framework and conceptual model[J]. Journal of Earth Science, 2013, 24(1): 89-103. doi: 10.1007/s12583-013-0312-7
[23] LI Jingrong, LI Yu, CHENG Hongliang, et al. Sedimentary characteristics of the third Member of Xujiahe Formation in Yuanba Area[J]. Journal of Xi'an Shiyou University (Natural Science Edition), 2013, 28(5): 43-50. doi: 10.3969/j.issn.1673-064X.2013.05.008 黎静容, 李毓, 程洪亮, 等. 元坝地区须三段沉积特征[J]. 西安石油大学学报(自然科学版), 2013, 28(5): 43-50. doi:10.3969/j.issn.1673-064X.2013.05.008
[24] HAO Jingyu. Subtile sediment and sequence character in northeastern Sichuan Basin[D]. Wuhan: Yangtze University, 2012. 郝景宇. 川东北地区须家河组沉积与层序特征精细研究[D]. 武汉: 长江大学, 2012.
[25] ZENG Tao. Sedimentary fades and depositional evolution of Member 3 of Upper Triassic Xujiahe Formation in Yuanba Area of northeast Sichuan, China[J]. Journal of Chengdu University of Technology (Science and Technology Edition), 2014, 41(4): 468-475. doi: 10.3969/j.issn.1671-9727.2014.04.09 曾韬. 川东北元坝地区须三段沉积相及沉积演化[J]. 成都理工大学学报(自然科学版), 2014, 41(4): 468-475. doi:10.3969/j.issn.1671-9727.2014.04.09
[26] MORAD S, ALDAHAN A A. Diagenetic chloritization of feldspars in sandstones[J]. Sedimentary Geology, 1987, 51(3-4): 155-164. doi: 10.1016/0037-0738(87)90046-7

多期次构造运动对不同物源成分砂岩控制作用

Controls of Multi-stage Tectonic Movement on Sandstones with Different Provenances

RichHTML

PDF (PC)

可视化

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 15

编辑推荐

Metrics

本文评价

[1]	冉清昌, 钟安宁, 周翔, 王超, 杨丹丹. 沙河子组致密砂砾岩成岩相及孔隙演化分析[J]. 西南石油大学学报(自然科学版), 2022, 44(1): 13-26.
[2]	邹敏, 夏东领, 夏冬冬, 庞雯. 致密砂岩储层非均质成因研究[J]. 西南石油大学学报(自然科学版), 2022, 44(1): 41-52.
[3]	吴承美, 许长福, 陈依伟, 谭强, 徐田录. 吉木萨尔页岩油水平井开采实践[J]. 西南石油大学学报(自然科学版), 2021, 43(5): 33-41.
[4]	吴锦伟, 李勇仁, 曹军, 吕栋梁. 渭北长₃裂缝性致密储层渗流特征及产能研究[J]. 西南石油大学学报(自然科学版), 2021, 43(3): 136-145.
[5]	程乐利, 白林坤, 韦少校, 熊亭, 印森林. 北羌塘拗陷巴贡组致密砂岩储层特征及控制因素[J]. 西南石油大学学报(自然科学版), 2021, 43(2): 10-22.
[6]	江同文, 张辉, 徐珂, 王志民, 王海应. 克深气田储层地质力学特征及其对开发的影响[J]. 西南石油大学学报(自然科学版), 2020, 42(4): 1-12.
[7]	马帅, 张风波, 王雯娟, 查玉强, 王彦利. 高压低渗气井产能二项式改进与求解[J]. 西南石油大学学报(自然科学版), 2020, 42(4): 121-126.
[8]	于学亮, 胥云, 翁定为, 蒋豪, 段瑶瑶. 页岩油藏“密切割”体积改造产能影响因素分析[J]. 西南石油大学学报(自然科学版), 2020, 42(3): 132-143.
[9]	李鹏, 范倩倩, 霍明会, 郑腊年, 岳君. 苏里格气田气井配产与递减率关系研究及应用[J]. 西南石油大学学报(自然科学版), 2020, 42(1): 126-132.
[10]	程小伟, 张高寅, 马志超, 李斌, 辜涛. 页岩气水平井油井水泥的原位增韧技术研究[J]. 西南石油大学学报(自然科学版), 2019, 41(6): 68-74.
[11]	李勇明, 骆昂, 吴磊, 伊向艺. 考虑应力敏感和水力裂缝方位角的页岩产能模型[J]. 西南石油大学学报(自然科学版), 2019, 41(6): 117-123.
[12]	白慧, 田敏, 冯敏, 刘鹏程, 王海涛. 低渗气藏多级压裂水平井产能模型及影响因素[J]. 西南石油大学学报(自然科学版), 2019, 41(3): 113-120.
[13]	杨树坤, 郭宏峰, 赵广渊, 季公明, 张博. 致密砂岩油藏注热水降压增注实验研究[J]. 西南石油大学学报(自然科学版), 2019, 41(1): 102-110.
[14]	夏鹏, 曾凡桂, 吴婧, 王晋, 冯绍盛. 中煤阶煤层气井排采阶段划分及渗透率变化[J]. 西南石油大学学报(自然科学版), 2018, 40(6): 115-123.
[15]	雷强, 唐洪明, 张烈辉, 朱柏宇. 钻井液在致密砂岩中裂缝的侵入深度模型[J]. 西南石油大学学报(自然科学版), 2018, 40(4): 97-104.