| 塔里木盆地库车坳陷西秋古隆起的形成及其演化 |
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| 引用本文： | 余海波,漆家福,师骏,张玮,曹淑娟,范绳,孙统,杨向阳.塔里木盆地库车坳陷西秋古隆起的形成及其演化[J].地质科学,2015,50(2):524-535. |
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| 作者姓名： | 余海波 漆家福 师骏 张玮 曹淑娟 范绳 孙统 杨向阳 |
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| 作者单位： | 1. 中国石油大学(北京)油气资源与探测国家重点实验室 北京 102249;
2. 中国石油大学(北京) 地球科学学院 北京 102249;
3. 中国石油塔里木油田公司研究院 新疆库尔勒 841000 |
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| 基金项目： | 国家科技重大专项的企业配套项目 |
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| 摘 要： | 重力异常资料显示,库车坳陷南缘西秋构造带深层发育有基底隆起。本文通过地震资料解释确认了西秋构造带深层占隆起的结构,分析了占隆起的形成和演化过程。西秋构造带南侧边缘存在一条区域性基底断裂,断裂北侧新生界下伏中生界、古生界明显减薄或地层缺失,总体上表现为断背斜形态的古隆起构造。结合区域构造演化分析认为,泥盆纪~石炭纪(D-C)塔里木克拉通边缘隆升、二叠纪-三叠纪(P-T)受南天山负荷影响产生的克拉通边缘压陷的构造演化过程中,西秋构造带处于"跷跷板"式地壳升降运动的"支点"部位,发育古隆起和基底卷入高角度断层,晚期南天山隆升向南斜向推挤的挤压剪切应力场使古隆起边界断层复活,基底断裂活动并在新生界之下形成冲断隆起。
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| 关 键 词： | 塔里木盆地 库车坳陷 西秋古隆起 构造演化 |
| 收稿时间： | 2014-09-10 |
| 修稿时间： | 2014-09-10; |
Paleo-uplift formation and evolution in the Xiqiu structural belt of the Kuqa depression,Tarim Basin |
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| Yu Haibo;Qi Jiafu;Shi Jun;Zhang Wei;Cao Shujuan;Fan Sheng;Sun Tong;Yang Xiangyang.Paleo-uplift formation and evolution in the Xiqiu structural belt of the Kuqa depression,Tarim Basin[J].Chinese Journal of Geology,2015,50(2):524-535. |
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| Authors: | Yu Haibo;Qi Jiafu;Shi Jun;Zhang Wei;Cao Shujuan;Fan Sheng;Sun Tong;Yang Xiangyang |
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| Institution: | 1. State Key Laboratory of Petroleum Resource and Prospecting, China University of Petroleum, Beijing 102249;
2. Department of Geology, China University of Petroleum, Beijing 102249;
3. Tarim Oil Company of PetroChina, Korla, Xinjiang 841000 |
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| Abstract: | Gravity anomaly data show that the Xiqiu tectonic belt in the southern margin of the Kuqa depression has developed as a basement uplift tectonic belt. The seismic data confirms the formation structure of the Xiqiu tectonic belt, and analyzes the processes of the formation and evolution of the ancient uplift. There are a regional basement-involved faults in the south edge of the Xiqiu tectonic belt, with obvious thinning of Paleozoic and Mesozoic thickness. The Paleozoic and Mesozoic strata have missed in the north edge of the faults, the whole ancient uplift performanced for faulted anticline structure. Combined with the regional tectonic evolution analysis, the edge of the Tarim Cratonic Basin has uplifted in Devonian and Carboniferous, the tectonic evolution process has been affected by the south of the Tianshan loading to form cratonic edge sag in Permian-Triassic. The Xiqiu tectonicbelt underwent tilting of crustal elevation and subsidence movement, has developed ancient uplift and high angle of basement-involved faults. The late transpressional stress field south of the Tianshan uplift due to oblique extrusion resulted in fault reactivation in the south of ancient uplift boundary, activities of the basement-involved faults resulted in the thrusting and uplifting under the Cenozoic strata. |
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| Keywords: | Tarim Basin Kuqa depression Xiqiu paleo-uplift Tectonic evolution |
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