| 青藏高原东西向伸展及其地质意义 |
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| 引用本文： | 张进江,丁林.青藏高原东西向伸展及其地质意义[J].地质科学,2003,38(2):179-189. |
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| 作者姓名： | 张进江 丁林 |
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| 作者单位： | 1. 北京大学地球与空间科学学院, 北京100871;2. 中国科学院地质与地球物理研究所, 北京100029 |
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| 基金项目： | 高等学校全国优秀博士学位论文作者专项资金项目 ( 2 0 0 0 2 2 )，国家自然科学基金项目 ( 4980 2 0 2 0 )，国家973青藏高原研究项目 (G19980 4 0 80 0 )研究成果。 |
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| 摘 要： | 东西和南北向伸展是青藏高原最显著的地质特征之一。南北向伸展形成的东西走向伸展构造,主要包括藏南拆离系(STDS),和沿喀喇昆仑—嘉黎断裂带(KJFZ)发育的正断层体系。东西向伸展形成数目众多的南北走向伸展构造,它们切割青藏高原几乎所有的东西走向构造单元,包括羌塘地块、KJFZ和STDS等,说明东西向伸展以整体形式发生并同时波及整个青藏高原,而不是由以KJFZ和STDS为边界的不同地块的不均匀挤出所致。南北走向伸展构造在地表呈之字形,为南北向挤压形成的追踪张断裂;剖面上表现为被后期高角度正断层叠加的拆离断层,拆离断层形成于中-晚中新世而高角度正断层形成于上新世及以后。导致拆离断层的东西向伸展可能是南北向挤压的变形分解,后期高角度正断层作用可能是高原隆升后的垮塌所致。东西向伸展是控制青藏高原新生代浅色花岗岩和盆地形成的主要因素。
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| 关 键 词： | 青藏高原 伸展构造 形成机制 变形分解 浅色花岗岩 盆地 |
| 收稿时间： | 2001-09-11 |
| 修稿时间： | 2001年9月11日 |
EAST-WEST EXTENSION IN TIBETAN PLATEAU AND ITS SIGNIFICANCE TO TECTONIC EVOLUTION |
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| Zhang Jinjiang,Ding Lin.EAST-WEST EXTENSION IN TIBETAN PLATEAU AND ITS SIGNIFICANCE TO TECTONIC EVOLUTION[J].Chinese Journal of Geology,2003,38(2):179-189. |
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| Authors: | Zhang Jinjiang Ding Lin |
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| Institution: | 1. School of Earth and Space Science, Peking University, Beijing 100871;2. Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029 |
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| Abstract: | One of the most striking geological features in Tibet was widespread distribution extensional structures formed by north south and east west extension. Besides the southern Tibetan detachment system (STDS), another large scale E W trending structure formed by north south extension was the normal faults along the Karakorum Jiali Fault zone (KJFZ). East west extension resulted in a great quantity of north south trending structures. These N S trending extensional structures cut most of the east west trending tectonic units of Tibet including Qiangtang block, KJFZ and STDS, indicating that the east west extension took place as a uniform tectonics involving almost the whole plateau simultaneously, which was unlike the supposition that the extension was caused by the heterogeneous extrusion of different blocks along KJFZ and STDS. The N S trending extensional faults took the zigzag shapes on earth surface, expressing the characters of tensional faults tracing conjugate faults formed by N S contraction. In sections, these structures showed features of detachment faults superposed by later high angle normal faulting. The detachment faults formed in Mid Late Miocene whereas the high angle faulting took place during and after Pliocene. The east west extension resulting in the detachment faults was probably caused by the deformation partition of the north south compression while the late high angle faulting was possibly caused by the collapse of the Plateau after its uplift. The east west extension was one of most important tectonic factors controlling the formation of Cenozoic leucogranite and basins in Tibet. |
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| Keywords: | The Tibetan Plateau Extension Formation mechanism Deformation partition Leucogranite The basins |
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