Magnetostratigraphy of the Dahonggou section, northern Qaidam Basin and its bearing on Cenozoic tectonic evolution of the Qilian Shan and Altyn Tagh Fault
Magnetostratigraphy of the Dahonggou section, northern Qaidam Basin and its bearing on Cenozoic tectonic evolution of the Qilian Shan and Altyn Tagh Fault
复制标题
柴达木盆地北部大红沟剖面磁性地层及其对祁连山、阿尔金断裂新生代构造演化的影响
DOI：
10.1016/j.epsl.2009.10.016
复制
发表时间：
2009-11-15
影响因子：
5.3
通讯作者：
Xiong, Shangfa
中科院分区：
文献类型：
--
作者：
Lu, Haijian;Xiong, Shangfa
青藏高原隆升的时间对青藏高原和新生代全球气候变化的构造模型的发展起着核心作用。对柴达木盆地北部大红沟剖面的详细磁性地层学研究表明，该剖面的年龄为34~8.5 Ma，上干柴沟组、下油砂山组和上油砂山组的年龄分别为34~22~20 Ma、22~20~13 Ma和13~20 Ma
The timing of uplift of the Tibet Plateau has a central role in the development of tectonic models for the Tibet Plateau and Cenozoic global climate change. A detailed magnetostratigraphic study of the Dahonggou section, northern Qaidam Basin, reveal that the section spans from similar to 34 to similar to 8.5 Ma and the ages of the Shang Ganchaigou, Xia Youshashan and Shang Youshashan formations are from > 34 to 22-20 Ma, 22-20 to 13 Ma and 13 to