| 滇西北剑川-虎跳峡大规模东向西逆冲推覆构造——兼论滇西扬子陆块区与西藏-三江造山系界线 |
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| 引用本文： | 沙绍礼,曾普胜,苟瑞涛,代艳娟,张子雄.滇西北剑川-虎跳峡大规模东向西逆冲推覆构造——兼论滇西扬子陆块区与西藏-三江造山系界线[J].地质力学学报,2015,21(3):438-445. |
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| 作者姓名： | 沙绍礼 曾普胜 苟瑞涛 代艳娟 张子雄 |
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| 作者单位： | 云南省地质矿产勘查开发局第三地质大队, 云南 大理 671000;国家地质实验测试中心, 北京 100037;国家地质实验测试中心, 北京 100037;中国地质大学地球科学与资源学院, 北京 100083;国家地质实验测试中心, 北京 100037;昆明理工大学国土资源工程学院, 昆明 650000;云南省地质科学研究所, 昆明 650000 |
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| 基金项目： | 国土资源大调查项目(12120113002500);国家自然科学基金项目(41072073);国土资源部公益性行业科研专项(201211078) |
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| 摘 要： | 基于剑川至虎跳峡一带的野外区域地质调查资料,论述剑川-虎跳峡断裂的性质,进而探讨扬子-华南陆块区与西藏-三江造山系的界线。野外观察显示,该区存在大规模自东向西的逆冲推覆构造,从剑川开始,经丽江白汉场—汝寒坪、忠义村,至香格里拉县的虎跳峡镇(下桥头)等地,多条剖面可见上扬子稳定型的古生代及中生代三叠纪地层自东向西逆冲推覆在西藏-三江造山系地层层序之上,推覆距离大于50 km。因此,剑川—虎跳峡断裂不是两大板块的边界,而是一条狭长的构造窗。两大板块的界线应是大理-剑川-丽江-木里断裂,南段接红河断裂。
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| 关 键 词： | 逆冲推覆构造 构造窗 木里-丽江断裂 分界线 西藏-三江造山系 扬子陆块区 |
| 收稿时间： | 2015/1/26 0:00:00 |
LARGE-SCALE E-W THRUST NAPPES IN JIANCHUAN-HUTIAOXIA AREA, NW YUNNAN, CHINA: A DISCUSSION ON THE BOUNDARY OF THE YANGTZE CRATON AND TIBET-SANJIANG OROGENIC SYSTEM |
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| SHA Shao-li,ZENG Pu-sheng,GOU Rui-tao,DAI Yan-juan and ZHANG Zi-xiong.LARGE-SCALE E-W THRUST NAPPES IN JIANCHUAN-HUTIAOXIA AREA, NW YUNNAN, CHINA: A DISCUSSION ON THE BOUNDARY OF THE YANGTZE CRATON AND TIBET-SANJIANG OROGENIC SYSTEM[J].Journal of Geomechanics,2015,21(3):438-445. |
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| Authors: | SHA Shao-li ZENG Pu-sheng GOU Rui-tao DAI Yan-juan and ZHANG Zi-xiong |
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| Institution: | The No.3 Geological Brigade, Yunnan Bureau of Geoexploration and Development of Mineral Resources, Dali 671000, China;National Research Center for Geoanlysis, Beijing 100037, China;National Research Center for Geoanlysis, Beijing 100037, China;School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China;National Research Center for Geoanlysis, Beijing 100037, China;Engineering Institute of Land and Resources, Kunming University of Science and Technology, Kunming 650000, China;Yunnan Institute of Geological Sciences, Kunming 650000, China |
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| Abstract: | Based on the regional geological survey, the characteristics of the faults in Jianchuan-Hutiaoxia area and the boundary of the Yangtze Craton and Tibet-Sanjiang Orogenic System were discussed. The results show that there exist EW trending large-scale thrust nappe structures in this region. Through the observation of several sections which started from Jianchuan to Baihanchang-Ruhanping and Zhongyi Village in Lijiang, and ended in Hutiaoxia town (Xiatiaotou) in Shangri-La,it is revealed that the stable sequences including Paleozoic and Mesozoic Triassic strata of Yangtze craton are thrust nappes, overlying westward on the strata sequences of the Tibetan-Sanjiang orogenic system, with the thrusting distance over 50 km. Therefore the Jianchuan-Hutiaoxia fault is a narrow tectonic window instead of the boundary of the Yantze Craton and the Sanjiang orogenic system. The Erhai-Jianchuan-Lijiang-Muli fault is suggested as the boundary of the two plates, extending southward to the Red River fault. |
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| Keywords: | thrust nappe structure tectonic window Erhai-Jianchuan-Lijiang-Muli fault Tibet-Sanjiang Orogenic System Boundary Yangtze Craton |
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