| 川渝地区构造动力学演化与盆岭-盆山耦合构造分析 |
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| 引用本文： | 李忠权,麻成斗,应丹琳,李洪奎,李应,万双双,席云飞.川渝地区构造动力学演化与盆岭-盆山耦合构造分析[J].岩石学报,2014,30(3):631-640. |
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| 作者姓名： | 李忠权 麻成斗 应丹琳 李洪奎 李应 万双双 席云飞 |
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| 作者单位： | 油气藏地质及开发工程国家重点实验室 成都理工大学, 成都 610059;国土资源部构造成矿成藏重点实验室 成都理工大学, 成都 610059;油气藏地质及开发工程国家重点实验室 成都理工大学, 成都 610059;中石油西南油气田分公司, 成都 610051;油气藏地质及开发工程国家重点实验室 成都理工大学, 成都 610059;国土资源部构造成矿成藏重点实验室 成都理工大学, 成都 610059;中国地质大学能源学院, 北京 100083;密苏里科技大学, 密苏里州 615401;油气藏地质及开发工程国家重点实验室 成都理工大学, 成都 610059;国土资源部构造成矿成藏重点实验室 成都理工大学, 成都 610059;油气藏地质及开发工程国家重点实验室 成都理工大学, 成都 610059;国土资源部构造成矿成藏重点实验室 成都理工大学, 成都 610059 |
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| 基金项目： | 本文受国家自然科学基金重点项目（41030426）、国家自然科学主任基金（41340004）、国家重大专项（2011ZX05004-005-01）和四川省省属高校科研创新团队（13TD0007）联合资助. |
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| 摘 要： | 以构造动力学演化为主线,从拉张与挤压的辩证关系出发,提出了川渝地区构造动力学演化经历了挤压-区域拉张-陆隆伸展-再挤压的构造动力学演化过程;川渝地区在T3-J2期间为盆岭耦合构造格局,在当时山岭与盆地之间过渡的斜坡带前缘(大致相当于理县至都江堰地域),出现印支、燕山期滑覆构造,表现为山岭斜坡前缘逆冲叠瓦状断层与紧闭甚至倒转、平卧褶皱的出现;J3以来,构造动力学背景由伸展转变为挤压,形成基底卷入的厚皮构造,龙门山迅速崛起,四川盆地最终定型,形成现今见到的松潘甘孜高原-龙门山-四川盆地构成的盆山耦合构造格局。
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| 关 键 词： | 松潘高原 龙门山 四川盆地 盆岭耦合 盆山耦合 西南盆地 |
| 收稿时间： | 7/7/2013 12:00:00 AM |
| 修稿时间： | 2013/12/26 0:00:00 |
Tectonic dynamic evolution and analysis of basin-range coupling and basin-mountain coupling in Sichuan-Chongqing region, China |
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| LI ZhongQuan,MA ChengDou,YING DanLin,LI HongKui,LI Ying,WAN ShuangShuang and XI YunFei.Tectonic dynamic evolution and analysis of basin-range coupling and basin-mountain coupling in Sichuan-Chongqing region, China[J].Acta Petrologica Sinica,2014,30(3):631-640. |
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| Authors: | LI ZhongQuan MA ChengDou YING DanLin LI HongKui LI Ying WAN ShuangShuang and XI YunFei |
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| Institution: | State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, China;Key Laboratory of Tectonic Controls on Mineralization and Hydrocarbon Accumulation, Ministry of Land and Resources, Chengdu University of Technology, Chengdu 610059, China;State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, China;Southwest Oil and Gas Field Company of Petrochina, Chengdu 610051, China;State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, China;Key Laboratory of Tectonic Controls on Mineralization and Hydrocarbon Accumulation, Ministry of Land and Resources, Chengdu University of Technology, Chengdu 610059, China;School of Energy Resources, China University of Geosciences, Beijing 100083, China;Missouri University of Science and Technology, Missouri 615401, USA;State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, China;Key Laboratory of Tectonic Controls on Mineralization and Hydrocarbon Accumulation, Ministry of Land and Resources, Chengdu University of Technology, Chengdu 610059, China;State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, China;Key Laboratory of Tectonic Controls on Mineralization and Hydrocarbon Accumulation, Ministry of Land and Resources, Chengdu University of Technology, Chengdu 610059, China |
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| Abstract: | From the dialectical perspective of extension and compression, this paper proposes that the Sichuan-Chongqing region has experienced a geodynamic evolution. The dynamic evolution of the main line began with compression, then regional extension, followed by uplift and stretching of the land, and finally by another stage of compression. The Sichuan-Chongqing region has experienced a geodynamic tectonic background of basin-range coupling between the Late Triassic to Middle Jurassic. During that period, sliding nappes of Indosinian and Yanshanian tectonic plates were found in the foreslope, an area roughly equivalent to the Dujiangyan-Lixian area serving as the transition zone between the range and the basin. The sliding of the Indosinian and Yanshanian results in the formation of imbricate thrusting faults, tight folds, and even the emergence of overturned and recumbent folds. Since the Late Jurassic, the shifting geodynamic tectonic background has resulted in the formation of many of the present day geologic landmarks in the Sichuan-Chongqing region after the Late Jurassic compression events gave way to the formation of the thick-skinned and basement-involved structure. After the basement structure formed after the Late Jurassic, many present day formations such as the Longmen Mountain rapidly rose, the Sichuan basin formed, and the basin-mountain coupling structure pattern consisting of the Songpan-Ganzi plateau-Longmen Mountain-Sichuan basin formed. |
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| Keywords: | Songpan-Ganzi plateau Longmen Mountain Sichuan basin Basin-range coupling Basin-mountain coupling Southwest basin |
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