Effect of the size statistics in studying the uplift of the Tibetan plateau

LI Zeng; WANG Yun-bin; LIANG Ming-hong; XU Jingi-ming; LIU Tu-gai; WANG Qi-hang

Northwestern Geology > 2005 > 38(3): 16-20.

LI Zeng, WANG Yun-bin, LIANG Ming-hong, et al. Effect of the size statistics in studying the uplift of the Tibetan plateau[J]. Northwestern Geology, 2005, 38(3): 16-20.

Citation:

LI Zeng, WANG Yun-bin, LIANG Ming-hong, et al. Effect of the size statistics in studying the uplift of the Tibetan plateau[J]. Northwestern Geology, 2005, 38(3): 16-20.

Citation:

LI Zeng, WANG Yun-bin, LIANG Ming-hong, et al. Effect of the size statistics in studying the uplift of the Tibetan plateau[J]. Northwestern Geology, 2005, 38(3): 16-20.

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Effect of the size statistics in studying the uplift of the Tibetan plateau

1.
Gansu Institute of Geological Survey, Lanzhou 730000, China
2.
College of Earth Sciences and Land Resources, Chang'an University 710054, China
3.
No.3 Institute of Geology and Mineral Exploration, Gansu Provincial Bureau of Geology and Mineral Exploration and Development, Lanzhou 730050, China

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Received Date: April 03, 2005
Revised Date: June 13, 2005
Published Date: September 04, 2005

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After being studied by size statistics in Changma diluvial fan, the conclusion that sediments sizes were largened 7 times from Early Pleistocence was drawn. That is to say, the north-eastern margin of the Tibetan plateau has uplifted 7 times. The same conclusion also had been drawn by analysising the sediments of basin and active fault and the river terraces. They have the same active times with the Tibetan plateau uplift in sera. So, the size statistics given a new methed to study the diluvial.
- size statistics,
- 7 times events of size largened,
- Changma diluvial fan,
- Tibetan plateau uplift

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崔之久,等.泥石流沉积与环境[M].北京:海洋出版社,1996.

于庆文,李长安.等青藏高原区东北缘新生代隆升-沉积-气候演化玉其耦合——区域地质调查方法实践,中国地质调查局地质调查专报H6[M].北京:中国地质大学出版社.

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