松辽盆地南部梨树地区走滑-逆冲构造的成因——以小宽断裂带为例

doi:10.7623/syxb202009005

石油学报 ›› 2020, Vol. 41 ›› Issue (9): 1089-1099.DOI: 10.7623/syxb202009005

松辽盆地南部梨树地区走滑-逆冲构造的成因——以小宽断裂带为例

邓铭哲¹, 方成名¹, 邓棚¹, 张永², 朱建峰³

1. 中国石油化工股份有限公司石油勘探开发研究院无锡石油地质研究所江苏无锡 214126;
2. 中国石油化工股份有限公司石油勘探开发研究院西北勘探研究中心北京 100083;
3. 中国石油化工股份有限公司东北油气分公司吉林长春 130062

收稿日期:2019-06-21 修回日期:2020-04-26 出版日期:2020-09-25 发布日期:2020-09-29
通讯作者: 邓铭哲,男,1990年2月生,2012年获中国地质大学(北京)矿产普查与勘探(固体矿产)专业学士学位,2019年获中国地质大学(北京)矿产普查与勘探(油气)专业博士学位,现为中国石油化工股份有限公司石油勘探开发研究院无锡石油地质研究所博士后,主要从事含油气盆地分析方向的研究工作。
作者简介:邓铭哲,男,1990年2月生,2012年获中国地质大学(北京)矿产普查与勘探(固体矿产)专业学士学位,2019年获中国地质大学(北京)矿产普查与勘探(油气)专业博士学位,现为中国石油化工股份有限公司石油勘探开发研究院无锡石油地质研究所博士后,主要从事含油气盆地分析方向的研究工作。Email:dmz527214955@126.com
基金资助:
国家科技重大专项（2017ZX05005-001-004）资助。

Origin of strike-slip thrust structure in Lishu area, southern Songliao Basin: a case study of Xiaokuan fault belt

Deng Mingzhe¹, Fang Chengmin¹, Deng Peng¹, Zhang Yong², Zhu Jianfeng³

1. Wuxi Institute of Petroleum Geology, Sinopec Petroleum Exploration and Production Research Institute, Jiangsu Wuxi 214126, China;
2. Northwest Exploration and Development Research Center, Sinopec Petroleum Exploration and Production Research Institute, Beijing 100083, China;
3. Sinopec Northeast Oil and Gas Company, Jilin Changchun 130062, China

Received:2019-06-21 Revised:2020-04-26 Online:2020-09-25 Published:2020-09-29

摘要/Abstract

摘要：

多个构造带的复合叠加过程及其形成的地质结构是陆内构造变形研究的前沿问题。松辽盆地南部梨树断陷处于古亚洲洋构造域与太平洋构造域的交接位置，是研究这一问题的良好窗口。小宽断裂带是梨树断陷内具有代表性的构造单元，与区域内的油气藏关系密切，其地质结构和演化过程仍存在争议。研究通过开展三维地震数据解释和地震相干切片分析厘定了小宽断裂带的地质结构和演化过程；通过总结前人认识和区域大地构造演化背景分析了走滑-逆冲活动的成因机制及其油气地质意义。研究结果认为：①小宽断裂带整体向西倾，可分为南段、中段、北段3部分；②在早白垩世，小宽断裂带经历了早期伸展构造变形和末期左行走滑-逆冲构造变形，断裂带的走滑-逆冲构造活动导致梨树断陷中央构造带内形成多个背斜；③小宽断裂带形成于中国东北地区由古亚洲洋构造域主导向太平洋构造域主导的转换过程，受控于早白垩世晚期古太平洋板块的加速俯冲；④小宽断裂带走滑-逆冲构造活动所形成的背斜构造是梨树断陷中央构造带内油气富集的重要构造。小宽断裂带南段发育封闭性良好的背斜构造，生-储-盖条件较好，具有成为梨树断陷下一步勘探方向的潜力。

关键词: 走滑构造, 太平洋板块, 松辽盆地, 梨树断陷, 小宽断裂带

Abstract:

The complex superposition process of multiple structural belts and their geological structures are the frontier issues in the study of intracontinental structural deformation. Lishu fault depression in the southern Songliao Basin is located at the junction of the Paleo-Asian Ocean tectonic domain and the Pacific tectonic domain, which is a good window for studying that issue. Xiaokuan fault belt is a representative structural unit in Lishu fault depression; it is closely related to the oil and gas reservoirs in this region, but there are still disputes on its geological structure and evolution process. This study determines the geological structure and evolution process of Xiaokuan fault belt by carrying out 3D seismic data interpretation and seismic coherence slice analysis. Through summarizing previous knowledge and the regional geotectonic evolution background, this paper analyzes the genetic mechanism of strike-slip thrust activity and its significance of petroleum geology. The study results show as follows. (1) Xiaokuan fault belt dips to the west as a whole and can be divided into three parts: the south, middle, and north sections. (2) In the Early Cretaceous, Xiaokuan fault belt experienced early extensional structural deformation and late sinistral strike-slip thrust deformation, and the strike-slip thrust tectonic activity of the fault belt led to the formation of multiple anticlines in the central tectonic belt of Lishu fault depression. (3) Xiaokuan fault belt formed in the transformation process from the Paleo-Asian Ocean tectonic domain dominant in northeastern China to the Pacific tectonic domain, which was controlled by the accelerated subduction of the Paleo-Pacific plate in the late Early Cretaceous. (4) The formation of anticline structure due to the strike-slip thrust tectonic activity of Xiaokuan fault belt is an important structural factor for forming hydrocarbon enrichment areas in the central tectonic belt of Lishu fault depression. The anticline structure with good sealing property developed in the southern section of Xiaokuan fault belt has good generation-reservoir-cap conditions, indicating the next exploration direction of Lishu fault depression.

Key words: strike-slip structure, Pacific plate, Songliao Basin, Lishu fault depression, Xiaokuan fault belt

中图分类号:

TE121.2

邓铭哲, 方成名, 邓棚, 张永, 朱建峰. 松辽盆地南部梨树地区走滑-逆冲构造的成因——以小宽断裂带为例[J]. 石油学报, 2020, 41(9): 1089-1099.

Deng Mingzhe, Fang Chengmin, Deng Peng, Zhang Yong, Zhu Jianfeng. Origin of strike-slip thrust structure in Lishu area, southern Songliao Basin: a case study of Xiaokuan fault belt[J]. Acta Petrolei Sinica, 2020, 41(9): 1089-1099.

参考文献

[1] 张国伟,郭安林,董云鹏,等.大陆地质与大陆构造和大陆动力学[J].地学前缘,2011,18(3):1-12.
ZHANG Guowei,GUO Anlin,DONG Yunpeng,et al.Continental geology,tectonics and dynamics[J].Earth Science Frontiers,2011,18(3):1-12.
[2] 国家自然科学基金委员会,中国科学院.中国学科发展战略:板块构造与大陆动力学[M].北京:科学出版社,2017.
National Natural Science Foundation of China,Chinese Academy of Sciences.Discipline development strategy in China:plate tectonics and continental dynamics[M].Beijing:Science Press,2017.
[3] 潘桂棠,肖庆辉,陆松年,等.中国大地构造单元划分[J].中国地质,2009,36(1):1-29.
PAN Guitang,XIAO Qinghui,LU Songnian,et al.Subdivision of tectonic units in China[J].Geology in China,2009,36(1):1-29.
[4] 周建波,张兴洲,马志红,等.中国东北地区的构造格局与盆地演化[J].石油与天然气地质,2009,30(5):530-538.
ZHOU Jianbo,ZHANG Xingzhou,MA Zhihong,et al.Tectonic framework and basin evolution in Northeast China[J].Oil & Gas Geology,2009,30(5):530-538.
[5] 孟凡超,刘嘉麒,崔岩,等.中国东北地区中生代构造体制的转变:来自火山岩时空分布与岩石组合的制约[J].岩石学报,2014,30(12):3569-3586.
MENG Fanchao,LIU Jiaqi,CUI Yan,et al.Mesozoic tectonic regimes transition in the Northeast China:constriants from temporal-spatial distribution and associations of volcanic rocks[J].Acta Petrologica Sinica,2014,30(12):3569-3586.
[6] 刘永江,张兴洲,金巍,等.东北地区晚古生代区域构造演化[J].中国地质,2010,37(4):943-951.
LIU Yongjiang,ZHANG Xingzhou,JIN Wei,et al.Late Paleozoic tectonic evolution in Northeast China[J].Geology in China,2010,37(4):943-951.
[7] 任战利,崔军平,史政,等.中国东北地区晚古生代构造演化及后期改造[J].石油与天然气地质,2010,31(6):734-742.
REN Zhanli,CUI Junping,SHI Zheng,et al.The Late Paleozoic tectonic evolution and later transformation in Northeast China[J].Oil & Gas Geology,2010,31(6):734-742.
[8] 徐备,赵盼,鲍庆中,等.兴蒙造山带前中生代构造单元划分初探[J].岩石学报,2014,30(7):1841-1857.
XU Bei,ZHAO Pan,BAO Qingzhong,et al.Preliminary study on the Pre-Mesozoic tectonic unit division of the Xing-Meng orogenic belt (XMOB)[J].Acta Petrologica Sinica,2014,30(7):1841-1857.
[9] 唐杰,许文良,王枫.东北亚早中生代火成岩组合的时空变异:对古太平洋板块俯冲开始时间的制约[J].矿物岩石地球化学通报,2016,35(6):1181-1194.
TANG Jie,XU Wenliang,WANG Feng.Rock associations and their spatial-temporal variations of the Early Mesozoic igneous rocks in the NE Asia:constraints on the initial subduction timing of the Paleo-Pacific plate[J].Bulletin of Mineralogy,Petrology and Geochemistry,2016,35(6):1181-1194.
[10] WANG Yu,ZHOU Liyun,LIU Shaofeng,et al.Post-cratonization deformation processes and tectonic evolution of the North China craton[J].Earth-Science Reviews,2018,177:320-365.
[11] 张晋瑞,魏春景,初航.兴蒙造山带构造演化的新模式:来自内蒙古中部四期不同类型变质作用的证据[J].岩石学报,2018,34(10):2857-2872.
ZHANG Jinrui,WEI Chunjing,CHU Hang.New model for the tectonic evolution of Xing'an-Inner Mongolia orogenic belt:evidence from four different phases of metamorphism in central Inner Mongolia[J].Acta Petrologica Sinica,2018,34(10):2857-2872.
[12] ZHOU Jianbo,WILDE S A,ZHANG Xingzhou,et al.The onset of Pacific margin accretion in NE China:evidence from the Heilongjiang high-pressure metamorphic belt[J].Tectonophysics,2009,478(3/4):230-246.
[13] 李三忠,张国伟,周立宏,等.中、新生代超级汇聚背景下的陆内差异变形:华北伸展裂解和华南挤压逆冲[J].地学前缘,2011,18(3):79-107.
LI Sanzhong,ZHANG Guowei,ZHOU Lihong,et al.The opposite Meso-Cenozoic intracontinental deformations under the superconvergence:rifting and extension in the North China craton and shortening and thrusting in the South China craton[J].Earth Science Frontiers,2011,18(3):79-107.
[14] 索艳慧,李三忠,曹现志,等.中国东部中新生代反转构造及其记录的大洋板块俯冲过程[J].地学前缘,2017,24(4):249-267.
SUO Yanhui,LI Sanzhong,CAO Xianzhi,et al.Mesozoic-Cenozoic inversion tectonics of East China and its implications for the subduction process of the oceanic plate[J].Earth Science Frontiers,2017,24(4):249-267.
[15] 罗群.中国东北地区断裂系统及其控藏特征[J].石油实验地质,2010,32(3):205-210.
LUO Qun.Fault systems and characteristics of their controlling reservoir formation in the Northeast China[J].Petroleum Geology & Experiment,2010,32(3):205-210.
[16] 陈东旭,章凤奇,陈汉林,等.新生代辉绿岩岩体识别及油气地质意义——以中国东北地区方正断陷为例[J].石油学报,2016,37(6):757-767.
CHEN Dongxu,ZHANG Fengqi,CHEN Hanlin,et al.Identification and hydrocarbon geological significance of Cenozoic diabase rock:a case study of Fangzheng faulted sag,NE China[J].Acta Petrolei Sinica,2016,37(6):757-767.
[17] 余一欣,周心怀,徐长贵,等.渤海辽东湾坳陷走滑断裂差异变形特征[J].石油与天然气地质,2014,35(5):632-638.
YU Yixin,ZHOU Xinhuai,XU Changgui,et al.Differential deformation of strike slip faults in the Liaodongwan depression,offshore Bohai Bay Basin[J].Oil & Gas Geology,2014,35(5):632-638.
[18] 郑华,金宝强,杨志成,等.走滑断裂控制下渤海中深层复杂断块油藏潜力判别及滚动开发——以辽中凹陷W油田东块为例[J].中国海上油气,2015,27(5):76-81.
ZHENG Hua,JIN Baoqiang,YANG Zhicheng,et al.Potential discrimination and progressive development of Bohai mid-deep complex fault block reservoir controlled by strike-slip fault:a case study of east block of W oilfield in Liaozhong sag[J].China Offshore Oil and Gas,2015,27(5):76-81.
[19] 黄雷,刘池洋.张扭断裂带内复合花状构造的成因与意义[J].石油学报,2019,40(12):1460-1469.
HUANG Lei,LIU Chiyang.Genesis and significance of hybrid flower structure in a transtensional fault zone[J].Acta Petrolei Sinica,2019,40(12):1460-1469.
[20] 周新源,吕修祥,杨海军,等.塔中北斜坡走滑断裂对碳酸盐岩油气差异富集的影响[J].石油学报,2013,34(4):628-637.
ZHOU Xinyuan,LV Xiuxiang,YANG Haijun,et al.Effects of strike-slip faults on the differential enrichment of hydrocarbons in the northern slope of Tazhong area[J].Acta Petrolei Sinica,2013,34(4):628-637.
[21] 张新超,孙赞东,赵俊省,等.塔中北斜坡走滑断裂断距对碳酸盐岩油气藏的影响[J].现代地质,2014,28(5):1017-1022.
ZHANG Xinchao,SUN Zandong,ZHAO Junsheng,et al.Study on the influence of strike-slip fault displacement on reservoir in northern slope,Tazhong area[J].Geoscience,2014,28(5):1017-1022.
[22] 李映涛,漆立新,张哨楠,等.塔里木盆地顺北地区中-下奥陶统断溶体储层特征及发育模式[J].石油学报,2019,40(12):1470-1484.
LI Yingtao,QI Lixin,ZHANG Shaonan,et al.Characteristics and development mode of the Middle and Lower Ordovician fault-karst reservoir in Shunbei area,Tarim Basin[J].Acta Petrolei Sinica,2019,40(12):1470-1484.
[23] 韩剑发,苏洲,陈利新,等.塔里木盆地台盆区走滑断裂控储控藏作用及勘探潜力[J].石油学报,2019,40(11):1296-1310.
HAN Jianfa,SU Zhou,CHEN Lixin,et al.Reservoir-controlling and accumulation-controlling of strike-slip faults and exploration potential in the platform of Tarim Basin[J].Acta Petrolei Sinica,2019,40(11):1296-1310.
[24] 刘志宏,孙理难,王超,等.松辽盆地伏龙泉断陷构造特征及演化[J].吉林大学学报:地球科学版,2015,45(3):663-673.
LIU Zhihong,SUN Li'nan,WANG Chao,et al.Structural features and evolution of the Fulongquan sag in Songliao Basin[J].Journal of Jilin University:Earth Science Edition,2015,45(3):663-673.
[25] 李增玉,冯晓辉,陈光宇.松辽盆地南部深层断陷结构与构造特征分析[J].吉林地质,2017,36(2):1-4.
LI Zengyu,FENG Xiaohui,CHEN Guangyu.The analysis of southern Songliao Basin deep rift structure and features[J].Jilin Geology,2017,36(2):1-4.
[26] 刘玉虎,李瑞磊,赵洪伟,等.深大断裂特征及其对天然气成藏的影响——以松辽盆地德惠断陷万金塔地区为例[J].天然气勘探与开发,2017,40(1):23-31.
LIU Yuhu,LI Ruilei,ZHAO Hongwei,et al.Characteristics of deep large fault and its effects on gas accumulation:a case study on Wanjinta area in Dehui fault depression of the Songliao Basin[J].Natural gas Exploration and Development,2017,40(1):23-31.
[27] 张庆龙,王良书,解国爱,等.郯庐断裂带北延及中新生代构造体制转换问题的探讨[J].高校地质学报,2005,11(4):577-584.
ZHANG Qinglong,WANG Liangshu,XIE Guoai,et al.Discussion on northward extension of the tanlu fault zone and its tectonic regime transformation[J].Geological Journal of China Universities,2005,11(4):577-584.
[28] 曲少东.松辽盆地梨树断陷构造演化及区域动力学背景[D].西安:西北大学,2013:1-165.
QU Shaodong.Tectonic evolution and regional dynamics background of Lishu subbasin,Songliao Basin[D].Xi'an:Northwestern University,2013:1-165.
[29] 曲少东,刘池阳,宋立军,等.梨树断陷小宽断裂带构造特征及演化[J].西北大学学报:自然科学版,2013,43(4):612-616.
QU Shaodong,LIU Chiyang,SONG Lijun,et al.The structural characteristics and evolution of Xiaokuan fracture zone in Lishu rift[J].Journal of Northwest University:Natural Science Edition,2013,43(4):612-616.
[30] 王铣慧,魏柯佳,宋立军,等.梨树断陷断陷期小宽断裂带构造应力场数值模拟[J].海洋地质前沿,2019,35(3):40-47.
WANG Xianhui,WEI Kejia,SONG Lijun,et al.Numerical sumulation of tectonic stress field of the Xiaokuan fault zone during the fault depression period of the Lishu fault depression[J].Marine Geology Frontiers,2019,35(3):40-47.
[31] 徐红波.梨树断陷构造特征及构造样式分析[D].大庆:东北石油大学,2013.
XU Hongbo.The analysis of structural characteristics and tectonic style in Lishu fault depression[D].Daqing:Northeast Petroleum University,2013.
[32] 柯钦,郭波,王玉柱,等.梨树断陷边界控陷断裂活动特征及油气地质意义[J].复杂油气藏,2018,11(3):17-21.
KE Qin,GUO Bo,WANG Yuzhu,et al.Active characteristics and petroleum geological significance of boundary fault controlled by Lishu fault depression[J].Complex Hydrocarbon Reservoirs,2018,11(3):17-21.
[33] 甘学启,秦启荣,苏培东,等.左旋走滑对十屋油田构造形态的影响及石油地质意义[J].岩性油气藏,2011,23(3):40-43.
GAN Xueqi,QIN Qirong,SU Peidong,et al.Influence of left-lateral slip on structural form in Shiwu oilfield and it's petroleum geological significance[J].Lithologic Reservoirs,2011,23(3):40-43.
[34] 喻顺,吕修祥,柳广弟,等.松辽盆地十屋断陷天然气来源及成藏分析[J].地质科技情报,2011,30(1):90-95.
YU Shun,LV Xiuxiang,LIU Guangdi,et al.Natural gas resource and accumulation in the Shiwu fault depression,Songliao Basin[J].Geological Science and Technology Information,2011,30(1):90-95.
[35] 袁红军,刘民,王振升,等.十屋断陷小宽断裂带的走滑特征研究及其勘探前景分析[J].石油物探,2009,48(6):596-600.
YUAN Hongjun,LIU Min,WANG Zhensheng,et al.Study on strike-slip structural features of Xiaokuan faulted zone in Shiwu fault depression and analysis on its exploration perspective[J].Geophysical Prospecting for Petroleum,2009,48(6):596-600.
[36] 任纪舜,赵磊,徐芹芹,等.中国的全球构造位置和地球动力系统[J].地质学报,2016,90(9):2100-2108.
REN Jishun,ZHAO Lei,XU Qinqin,et al.Global tectonic position and geodynamic system of China[J].Acta Geologica Sinica,2016,90(9):2100-2108.
[37] 张欲清,张长厚,侯丽玉,等.内蒙古东南部西拉木伦缝合带两侧二叠纪以来的叠加褶皱变形:对同碰撞和碰撞后变形的启示[J].地学前缘,2019,26(2):264-280.
ZHANG Yuqing,ZHANG Changhou,HOU Liyu,et al.Superposed folding since the Permian on both sides of the Xar Moron suture,southeastern Inner Mongolia:implications for syn- and post- collision geodynamic process[J].Earth Science Frontiers,2019,26(2):264-280.
[38] REN Jianye,TAMAKI K,Li Sitian,et al.Late Mesozoic and Cenozoic rifting and its dynamic setting in Eastern China and adjacent areas[J].Tectonophysics,2002,344(3/4):175-205.
[39] 林伟,王军,刘飞,等.华北克拉通及邻区晚中生代伸展构造及其动力学背景的讨论[J].岩石学报,2013,29(5):1791-1810.
LIN Wei,WANG Jun,LIU Fei,et al.Late Mesozoic extension structures on the North China craton and adjacent regions and its geodynamics[J]. Acta Petrologica Sinica,2013,29(5):1791-1810.
[40] 宋鹰,任建业,阳怀忠,等.松辽盆地北部姚家组底界面特征及其动力学背景[J].石油学报,2010,31(2):187-195.
SONG Ying,REN Jianye,YANG Huaizhong,et al.Characteristics and dynamic background of bottom boundary in Yaojia Formation of the northern Songliao Basin[J].Acta Petrolei Sinica,2010,31(2):187-195.
[41] RICHARD P D,NAYLOR M A,KOOPMAN A.Experimental models of strike-slip tectonics[J].Petroleum Geoscience,1995,1(1):71-80.
[42] 许文良,孙德有.满洲里-绥芬河地学断面岩浆作用与地壳结构[M].北京:地质出版社,1994.
XU Wenliang,SUN Deyou.Manzhouli-Suifenhe geoscience transect:magmatism and crustal structure[M].Beijing:Geological Publishing House,1994.
[43] 李双林,欧阳自远.兴蒙造山带及邻区的构造格局与构造演化[J].海洋地质与第四纪地质,1998,18(3):45-54.
LI Shuanglin,OUYANG Ziyuan.Tectonic framework and evolution of Xing'anling Mongolian orogenic belt (XMOB)and its adjacent region[J].Marine Geology & Quaternary Geology,1998,18(3):45-54.
[44] 孔凡梅,李旭平,李守军,等.黑龙江杂岩带的形成演化及地质意义[J].地质论评,2011,57(5):623-631.
KONG Fanmei,LI Xuping,LI Shoujun,et al.Formation,evolution and geological significance of the Heilongjiang complex zone[J].Geological Review,2011,57(5):623-631.
[45] 辛玉莲,任军丽,彭玉鲸,等.中国东北兴蒙-吉黑造山带造山作用结束的标志——来自晚三叠世磨拉石(大地构造相)的证据[J].地质与资源,2011,20(6):413-419.
XIN Yulian,REN Junli,PENG Yujing,et al.Ending of the mountain-building movement of Xing'an-Mongolian-Ji-Hei orogenic belt in northeast China:evidence from Late Triassic molasse (geotectoinc phase)[J].Geology and Resources,2011,20(6):413-419.
[46] 臧兴运,赵华伟,马晶,等.吉林省吉黑造山带构造演化与成矿谱系[J].吉林地质,2018,37(4):1-13.
ZANG Xingyun,ZHAO Huawei,MA Jing,et al.Tectonic evolution and metallogenic pedigree of Jilin-Heilongjiang orogenic belt in Jilin Province[J].Jilin Geology,2018,37(4):1-13.
[47] REN Qiang,ZHANG Shihong,WU Huaichun,et al.Further paleomagnetic results from the ~155 Ma Tiaojishan Formation,Yanshan belt,North China,and their implications for the tectonic evolution of the Mongol-Okhotsk suture[J].Gondwana Research,2016,35:180-191.
[48] ENGEBRETSON D C,COX A,GORDON R.Relative motions between oceanic and continental plates in the Pacific Basin[M]Boulder,Colo:Geological Society of America,1985.
[49] SETON M,M? LLER R D,ZAHIROVIC S,et al.Global continental and ocean basin reconstructions since 200 Ma[J].Earth-Science Reviews,2012,113(3/4):212-270.
[50] 黄宝春,朱鸿,谭承泽.吉林省东部地区古地磁结果的大地构造意义[J].地球物理学报,1994,37(S2):304-315.
HUANG Baochun,ZHU Hong,TAN Chengze.Tectonic implications of paleomagnetic data from eastern area of Jilin Province,China[J].Acta Geophysica Sinica,1994,37(S2):304-315.
[51] PARK Y H,DOH S J,RYU I C,et al.A synthesis of cretaceous palaeomagnetic data from South Korea:tectonic implications in East Asia[J].Geophysical Journal International,2005,162(3):709-724.
[52] 唐杰,许文良,王枫,等.古太平洋板块在欧亚大陆下的俯冲历史:东北亚陆缘中生代-古近纪岩浆记录[J].中国科学:地球科学,2018,48(5):33-67.
TANG Jie,XU Wenliang,WANG Feng,et al.Subduction history of the Paleo-Pacific slab beneath Eurasian continent:Mesozoic-Paleogene magmatic records in Northeast Asia[J].Science China Earth Sciences,2018,61(5):527-559.
[53] 裴军令,杨振宇,赵越,等中国东北及邻区白垩纪古地磁分析与块体旋转运动动力学背景[J].地质学报,2009,83(5):617-627.
PEI Junling,YANG Zhengyu,ZHAO Yue,et al.Cretaceous paleomagnetism of the Northeast China and adjacent regions and the geodynamic setting of block rotations[J].Acta Geologica Sinica,2009,83(5):617-627.
[54] 马永生,何治亮,赵培荣,等.深层-超深层碳酸盐岩储层形成机理新进展[J].石油学报,2019,40(12):1415-1425.
MA Yongsheng,HE Zhiliang,ZHAO Peirong,et al.A new progress in formation mechanism of deep and ultra-deep carbonate reservoir[J].Acta Petrolei Sinica,2019,40(12):1415-1425.

松辽盆地南部梨树地区走滑-逆冲构造的成因——以小宽断裂带为例

Origin of strike-slip thrust structure in Lishu area, southern Songliao Basin: a case study of Xiaokuan fault belt

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