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| 柴达木盆地新生代演化及其构造重建——基于地震剖面的解释 | |
| 引用本文： | 尹安,党玉琪,陈宣华,汪立群,蒋武明,蒋荣宝,王小凤,周苏平,刘明德,马立协.柴达木盆地新生代演化及其构造重建——基于地震剖面的解释[J].地质力学学报,2007,13(3):193-211. |
| 作者姓名： | 尹安 党玉琪 陈宣华 汪立群 蒋武明 蒋荣宝 王小凤 周苏平 刘明德 马立协 |
| 作者单位： | 1. Department of Earth and Space Sciences,University of California,Los Angeles,California 90095-1567,USA 2. 中国石油青海油田公司,甘肃敦煌,736202 3. 中国地质科学院地质力学研究所,北京,100081 |
| 基金项目： | 国土资源大调查全国油气资源战略评价专项 , 青海油田公司项目资助 |
| 摘 要： | 柴达木盆地是青藏高原内部最大的坳陷。柴达木盆地构造成因的研究,可以揭示青藏高原形成机制和生长历史。本文分析了柴达木盆地区域地震勘探剖面,得到如下认识:柴达木盆地一级构造为新生代宽缓复向斜,其振幅和半波长分别从柴西的>16km和~170km变化为柴东的<4km和~50km。褶皱首先在柴西贴近阿尔金断裂附近形成(65~50.5Ma),并向柴东扩展(23.3Ma)。复向斜的形成与较老的柴北缘逆冲断层系(65~50.5Ma)和较年轻的柴南缘逆冲断层系(35.5~23.3Ma)有关。盆地内部新生代上地壳缩短作用,由柴西的>48%,向柴东减小到<1%,说明在柴西和柴东之间,存在地壳加厚机制的渐进转换:柴西主要为上地壳缩短,柴东主要为下地壳缩短。 |
| 关 键 词： | 地震反射剖面 构造重建 新生代 柴达木盆地 |
| 文章编号： | 1006-6616（2007）03-0193-19 |
| 收稿时间： | 2007-08-27 |
| 修稿时间： | 2007年8月27日 |
CENOZOIC EVOLUTION AND TECTONIC RECONSTRUCTION OF THE QAIDAM BASIN: EVIDENCE FROM SEISMIC PROFILES |
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| YIN An,DANG Yu-qi,CHEN Xuan-hu,WANG Li-qun,JIANG Wu-ming,JIANG Rong-bao,WANG Xiao-feng,ZHOU Su-ping,LIU Ming-de,MA Li-xie.CENOZOIC EVOLUTION AND TECTONIC RECONSTRUCTION OF THE QAIDAM BASIN: EVIDENCE FROM SEISMIC PROFILES[J].Journal of Geomechanics,2007,13(3):193-211. | |
| Authors: | YIN An DANG Yu-qi CHEN Xuan-hu WANG Li-qun JIANG Wu-ming JIANG Rong-bao WANG Xiao-feng ZHOU Su-ping LIU Ming-de MA Li-xie |
| Institution: | Department of Earth and Space Sciences and Institute of Geophysics and Planetary Physics, University of California, Los Angeles, CA 90095-1567, USA,Petroleum Research Institute of Qinghai Oilfield Company, PetroChina, Dunhuang, Gansu 736202, China,Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China,Petroleum Research Institute of Qinghai Oilfield Company, PetroChina, Dunhuang, Gansu 736202, China,Petroleum Research Institute of Qinghai Oilfield Company, PetroChina, Dunhuang, Gansu 736202, China,Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China,Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China,Petroleum Research Institute of Qinghai Oilfield Company, PetroChina, Dunhuang, Gansu 736202, China,Petroleum Research Institute of Qinghai Oilfield Company, PetroChina, Dunhuang, Gansu 736202, China and Petroleum Research Institute of Qinghai Oilfield Company, PetroChina, Dunhuang, Gansu 736202, China |
| Abstract: | The Qaidam basin is the largest topographic depression inside the Tibetan plateau. Understanding the tectonic origin of the Qaidam basin has important implications for unraveling the formation mechanism and growth history of the Tibetan plateau.In this paper, the authors analyze regional seismic-reflection profiles across the basin.The first-order structure of the basin is a broad Cenozoic synclinorium, with an amplitude ranging from > 16 km in the west to < 4 km in the east.The fold axis propagated from the western Qaidam basin against the Altyn Tagh fault at 65-50.5Ma to the eastern basin at 23.3Ma;its half-wavelength changes from ~170 km in the west to ~50 km in the east. The formation of the synclinorium was induced by an older thrust system initiated at ~65-50.5Ma at the northern margin and a younger thrust system initiated at 35.5-23.3Ma at the southern margin.Cenozoic upper-crustal shortening decreases across the basin from > 48% in the west to < 1% in the east, suggesting a progressive shift in crustal thickening mechanisms across the Qaidam basin, from dominantly upper-crustal shortening in the west to dominantly lower-crustal shortening in the east. |
| Keywords: | seismic reflection profile tectonic reconstruction Cenozoic Qaidam basin |
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