Tectonic framework, evolution and potential petroleum resources of the structural belt in the western margin of Songliao basin

WANG Yan; QIAN Cheng; ZHONG Hui; LI Chengli; QIN Tao; YANG Xiaoping; ZHAO Weijun

doi:10.12097/gbc.2023.03.011

2024 Vol. 43, No. 7

Article Contents

Article navigation > Geological Bulletin of China > 2024 > 43(7): 1073-1089

Next Article Previous Article

WANG Yan, QIAN Cheng, ZHONG Hui, LI Chengli, QIN Tao, YANG Xiaoping, ZHAO Weijun. 2024. Tectonic framework, evolution and potential petroleum resources of the structural belt in the western margin of Songliao basin. Geological Bulletin of China, 43(7): 1073-1089. doi: 10.12097/gbc.2023.03.011

Citation:

WANG Yan, QIAN Cheng, ZHONG Hui, LI Chengli, QIN Tao, YANG Xiaoping, ZHAO Weijun. 2024. Tectonic framework, evolution and potential petroleum resources of the structural belt in the western margin of Songliao basin. Geological Bulletin of China, 43(7): 1073-1089. doi: 10.12097/gbc.2023.03.011

Tectonic framework, evolution and potential petroleum resources of the structural belt in the western margin of Songliao basin

1.
Shenyang Center, China Geological Survey, Shenyang 110034, Liaoning, China
2.
Northeast Geological S&T Innovation Center of China Geological Survey, Shenyang 110034, Liaoning, China
3.
Military Civilian Integration Center of Geological Survey, China Geological Survey, Chengdu 610036, Sichuan, China

More Information

Corresponding author: ZHONG Hui, 2418734955@qq.com

Received Date: 06 March 2023

Revised Date: 22 June 2023

Publish Date: 15 July 2024

Abstract

Abstract

The structural belt in the western margin of the Songliao Basin is a key area for studying the formation and evolution of the Songliao basin. However, regarding the structural framework of this structural belt, the activity history and basin control characteristics are still unclear. This fine definition of deep material architecture and Meso-Cenozoic tectonic evolution in this structural belt provide a new evidence for solving this scientific problem. The Bouguer gravity anomaly and comprehensive geophysical profile characteristics indicate that the structural belt in the western margin of the Songliao basin manifests as a zonally distributed supercrustal deep structural belt. Through a comprehensive analysis encompassing the occurrence, nature and kinematics of the tectonic deformation zone, a "Bifurcated Dual Belt" structural framework is proposed. This framework divides into eastern and western zones, exhibiting opposing inclinations. According to the differences of basement background, tectonic pattern and geophysical characteristics of the structural belt development, a “four-stage” distribution framework is established for the north and south section. Additionally, considering the regional tectonic evolution, the structural analysis of deformation zones, and chronology data, the Meso−Cenozoic tectonic activity chronological framework of six periods is restored, including Late Triassic, Middle to Later Jurassic, middle Early Cretaceous, middle Late Cretaceous, Paleocene to Oligocene and Neogenic to Pleistocene. And combined with the basin-controlling influence of the structural belt, it is emphasized that the middle Jurassic and middle Early Cretaceous sedimentary basins, under the control of the exterior basin belt, hold paramount significance for the exploration, provided new basis for the exploration of petroleum reserves of new strata in northeastern China.
- Songliao basin /
- structural framework /
- chronological framwork /
- basin-controlling /
- potential petroleum resources /
- oil and gas exploration engineering

FullText(HTML)

References

[1]	Meng Q R. 2003. What drove late Mesozoic extension of the northern China–Mongoliatract?[J]. Tectonophysics, 369: 155−174. doi: 10.1016/S0040-1951(03)00195-1 CrossRef Google Scholar
[2]	Pang Y M, Guo X W, Zhang X H, et al. 2020. Late Mesozoic and Cenozoic tectono−thermal history and geodynamic implications of the Great Xing’an Range, NE China[J]. Journal of Asian Earth Sciences, 189: 104−155. Google Scholar
[3]	Wang T, Zheng Y, Zhang J, et al. 2011. Pattern and kinematic polarity of late Mesozoic extension in continental NE Asia: Perspectives from metamorphic core complexes[J]. Tectonics, 30(6): 119−145. Google Scholar
[4]	陈洪洲, 余中元, 许晓艳, 等. 2004. 嫩江断裂构造及其与地震活动的关系[J]. 东北地震研究, 4: 43−49. Google Scholar
[5]	陈印, 朱光, 姜大志, 等. 2013. 四合堂剪切带活动时代及其对燕山运动B幕时间的限定[J]. 地质学报, 87(3): 295−310. Google Scholar
[6]	陈树旺, 丁秋红, 郑月娟, 等. 2013. 松辽盆地外围新区、新层系——油气基础地质调查进展与认识[J]. 地质通报, 32(8): 1147−1158. Google Scholar
[7]	邓晋福, 苏尚国, 赵国春, 等. 2004. 华北燕山造山带构造要素组合[J]. 高校地质学报, 10(3): 315−323. Google Scholar
[8]	方曙, 朱洪森, 朱慧忠, 等. 2001. 华北地台北缘喀喇沁断隆隆升机制[J]. 中国地质, (3): 5−11. Google Scholar
[9]	方石, 张志强, 刘招君, 等. 2007. 松辽盆地新生代热演化及地层定年[J]. 吉林大学学报(地球科学版), 37(5): 923−928. Google Scholar
[10]	方石, 刘招君, 黄湘通, 等. 2008. 大兴安岭东南坡新生代隆升及地貌演化的裂变径迹研究[J]. 吉林大学学报(地球科学版), 5(2): 771−794. Google Scholar
[11]	傅维洲, 杨宝俊, 刘财, 等. 1998. 中国满洲里−绥芬河地学断面地震学研究[J]. 长春科技大学学报, 28(2): 206−212. Google Scholar
[12]	傅维洲, 贺日政. 1999. 松辽盆地及周边地带地震构造特征[J]. 世界地质, 18(2): 95−100. Google Scholar
[13]	郭孟习, 孙炜, 尹国义, 等. 2000. 郯庐断裂系的北延及地质−地球物理特征[J]. 吉林地质, 19: 35−44. Google Scholar
[14]	韩国卿, 刘永江, 温泉波, 等. 2009. 嫩江−八里罕断裂带岭下韧性剪切带变形特征[J]. 吉林大学学报(地球科学版), 39(3): 398−405. Google Scholar
[15]	韩国卿, 刘永江, Franz Neubauer, 等. 2012. 松辽盆地西缘边界断裂带中南段走滑性质、时间及其位移量[J]. 中国科学: 地球科学, 42(4): 471−482. Google Scholar
[16]	韩国卿, 刘永江, Franz Neubauer, 等. 2014. 松辽盆地西缘边界断裂带中北段尼尔基L型构造岩构造年代学及其构造意义[J]. 岩石学报, 30(7): 1922−1934. Google Scholar
[17]	核工业二四三大队. 2019. 内蒙古1∶5 万工农屯、扎鲁特旗、五道井子、鱼泡子牧场、包郎格艾勒、查布嘎吐幅区域地质调查报告[R]. Google Scholar
[18]	黄汲清. 1960. 中国地质构造基本特征的初步总结[J]. 地质学报, 40: 1237. Google Scholar
[19]	黄薇, 王建功, 赵应成, 等. 2007. 松辽盆地拗陷期坡折带特征[J]. 石油学报, 28(4): 31−35. Google Scholar
[20]	李佳桐. 2021. 松辽盆地西部斜坡区青山口组−嫩江组沉积体系研究[D]. 吉林大学硕士学位论文: 22−53. Google Scholar
[21]	李英康, 高锐, 姚聿涛, 等. 2014. 大兴安岭造山带及两侧盆地的地壳速度结构[J]. 地球物理学进展, 29(1): 73−83. Google Scholar
[22]	梁琛岳, 刘永江, 李伟, 等. 2012. 黑龙江省嫩江地区科洛杂岩隆升时代[J]. 地质科学, 47(2): 360−375. Google Scholar
[23]	刘勃然, 李伟, 贾杰, 等. 2014. 大兴安岭北段嘎拉山伸展滑脱构造[J]. 吉林大学学报(地球科学版), 44(4): 1142−1152. Google Scholar
[24]	刘财, 杨宝俊, 王兆国, 等. 2011. 松辽盆地西边界带深部构造: 地电学证据[J]. 地球物理学报, 54(2): 401−406. Google Scholar
[25]	刘桂珍, 鲍志东, 王英民. 2008. 松辽盆地西斜坡古沟谷−坡折带特征及其对储层分布的控制[J]. 中国石油大学学报(自然科学版), 32(6): 12−16. Google Scholar
[26]	刘伟, 杨进辉, 李潮峰. 2003. 内蒙赤峰地区若干主干断裂的构造热年代学[J]. 岩石学报, 19(4): 717−728. Google Scholar
[27]	鹿林, 张宫博, 刘财, 等. 2019. 地球物理剖面揭示大兴安岭域壳幔结构及其地质意义[J]. 地球物理学报, 62(11): 4401−4416. Google Scholar
[28]	马寅生, 吴满路, 曾庆利. 2002. 燕山及临区中新生代挤压与伸展的转换和成矿作用[J]. 地球学报, 23(2): 115−122. Google Scholar
[29]	内蒙古自治区地质调查院. 2019. 内蒙古1: 5 万沙巴尔吐、巴达尔湖社、两家子、团发屯六村、前联合屯、白音浩特幅区域地质调查报告[R]. Google Scholar
[30]	钱程, 崔天日, 李林川, 等. 2013. ASTER−GDEM数据在大兴安岭北段地貌形态分析中的应用[J]. 地质力学学报, 19(1): 82−92. Google Scholar
[31]	钱程, 陆露, 秦涛, 等. 2018. 大兴安岭北段雅鲁河断裂晚更新世活动记录[J]. 地质通报, 37(9): 1748−1754. Google Scholar
[32]	钱程, 汪岩, 秦涛, 等. 2022. 内蒙古扎兰屯地区晚三叠世韧性剪切变形的激光⁴⁰Ar/³⁹Ar年龄证据[J]. 中国地质, 49(1): 1990−1991. Google Scholar
[33]	裘善文. 2008. 中国东北地貌第四纪研究与应用[M]. 长春: 吉林科学出版社. Google Scholar
[34]	邵济安, 张履桥, 贾文, 等. 2001. 内蒙古喀喇沁变质核杂岩及其隆升机制探讨[J]. 岩石学报, 17(2): 283−290. Google Scholar
[35]	王东星, 贺宏云, 赵磊, 等. 2018. 内蒙古乌兰浩特地区早白垩世韧性变形对嫩江−八里罕断裂的响应[J]. 地质通报, 37(9): 1704−1709. Google Scholar
[36]	王璞珺, 赵然磊, 蒙启安, 等. 2015. 白垩纪松辽盆地: 从火山裂谷到陆内拗陷的动力学环境[J]. 地学前缘, 22(3): 99−117. Google Scholar
[37]	王新社, 郑亚东. 2005. 楼子店变质核杂岩韧性变形作用的⁴⁰Ar−³⁹Ar年代学约束[J]. 地质论评, 51(5): 574−582. Google Scholar
[38]	王新社, 郑亚东, 刘玉琳, 等. 2006. 内蒙赤峰南部楼子店拆离断层系绿泥石化带的形成时代[J]. 自然科学进展, 16(7): 902−906. Google Scholar
[39]	汪岩, 钱程, 马永非, 等. 2019. 吉林白城岭下地区花岗质糜棱岩锆石U−Pb年代学与地球化学特征对松辽盆地西缘晚古生代以来的俯冲背景的制约[J]. 地质学报, 93(1): 117−137. Google Scholar
[40]	吴咏敬, 董平, 王良书, 等. 2012. 东北地区构造分区与深断裂研究——基于重力场小波尺度分解[J]. 地球物理学进展, 27(1): 45−57. Google Scholar
[41]	辛仁臣, 王英民. 2004. 松辽盆地北部青山口−姚家组西部坡折带成因及演化[J]. 地球科学, 29(5): 621−624. Google Scholar
[42]	杨承先, 王贵华, 陈健. 1984. 内蒙红山−八里罕断裂带地质特征及其地震活动性[J]. 地震研究, (4): 391−398. Google Scholar
[43]	张鹏辉, 张小博, 方慧, 等. 2020. 地球物理资料揭示的嫩江−八里罕断裂中段深浅构造特征[J]. 吉林大学学报(地球科学版), 50(1): 261−272. Google Scholar
[44]	张振法, 葛昌宝. 2000. 内蒙古东部区深部构造特征和大地构造问题浅议[J]. 内蒙古地质, 3(1): 6−18. Google Scholar
[45]	张晓辉, 李铁胜, 蒲志平, 等. 2002. 内蒙古赤峰娄子店−大城子韧性剪切带的⁴⁰Ar−³⁹Ar年龄及其构造意义[J]. 科学通报, 47(12): 951−956. Google Scholar
[46]	张兴洲, 马玉霞, 迟效国, 等. 2012. 东北及内蒙古东部地区显生宙构造演化的有关问题[J]. 吉林大学学报(地球科学版), 42(5): 1269−1285. Google Scholar
[47]	张岳桥, 董树文, 赵越, 等. 2007. 华北侏罗纪大地构造: 综评与新认识[J]. 地质学报, 81(11): 1462−1480. doi: 10.3321/j.issn:0001-5717.2007.11.002 CrossRef Google Scholar
[48]	赵文智, 李建忠. 2004. 基底断裂对松辽南部油气聚集的控制作用[J]. 石油学报, 25(4): 1−6. doi: 10.3321/j.issn:0253-2697.2004.04.001 CrossRef Google Scholar
[49]	赵越. 1990. 燕山地区中生代造山运动及构造演化[J]. 地质论评, 36(1): 1−12. doi: 10.3321/j.issn:0371-5736.1990.01.001 CrossRef Google Scholar
[50]	赵越, 崔盛芹, 郭涛, 等. 2002. 北京西山侏罗纪盆地演化及其构造意义[J]. 地质通报, 21(4/5): 211−217. Google Scholar
[51]	赵越, 徐刚, 张拴宏, 等. 2004. 燕山运动与东亚构造体制的转变[J]. 地学前缘, 11(3): 319−328. Google Scholar
[52]	赵越, 宋彪, 张拴宏, 等. 2006. 北京西山侏罗纪南大岭组玄武岩的继承锆石年代学及其含义[J]. 地学前缘, 13(2): 184−190. Google Scholar
[53]	郑常青, 金巍, 张兴洲. 2008. 中国东北松辽盆地西缘韧性断裂带的锆石SHRMIP和黑云母Ar−Ar年龄及其大地构造意义[C]//任收麦. 东北亚地区油气地质与矿产资源学术研讨会论文集. 长春, 吉林大学: 81–82. Google Scholar
[54]	郑常青, 李娟, 金巍, 等. 2015. 松辽盆地西缘构造带中花岗质糜棱岩的锆石SHRIMP 和云母氩−氩年龄及其构造意义[J]. 吉林大学学报(地球科学版), 45(2): 349−363. Google Scholar
[55]	中国地质调查局沈阳地质调查中心. 2019. 内蒙古1∶5万五家户、孟家沟、莫力根屯、扎赉特旗、巴彦高勒幅区域地质调查报告[R]. Google Scholar