Discovery and character of the Kunlun-Yellow River Movement

被引:31
作者
Cui, ZJ [1 ]
Wu, YQ
Liu, GN
机构
[1] Peking Univ, Dept Geog, Beijing 100871, Peoples R China
[2] State Educ Commiss, Open Res Lab Environm Changes & Nat Disaster, Beijing 100875, Peoples R China
[3] Sichuan Normal Univ, Dept Geog, Chengdu 610063, Peoples R China
来源
CHINESE SCIENCE BULLETIN | 1998年 / 43卷 / 10期
关键词
Kunlun Mountain Pass; 700; kaBP; tectonic movement;
D O I
10.1007/BF03182748
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 [理学]; 0710 [生物学]; 09 [农学];
摘要
Based on geomorphological, tectonic and sedimentary data, a Kunlun Yellow River Tectonic Movement has been recognized in 1.10-0.60 Ma B.P. This tectonic movement, which leads to uplift of the Qinghai-Xizang (Tibet) plateau from 1500 to 3000-3500 m, is periodic, abrupt and changeable in the movement rate of uplifting and slide slipping.
引用
收藏
页码:833 / 836
页数:4
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[3]
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[4]
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[5]
KIDD WSF, 1990, GEOLOGICAL EVOLUTION, P348