High-resolution magnetostratigraphic study of the Paleogene-Neogene strata in the Northern Qaidam Basin: Implications for the growth of the Northeastern Tibetan Plateau

2017 ◽  
Vol 46 ◽  
pp. 141-155 ◽  
Author(s):  
Junliang Ji ◽  
Kexin Zhang ◽  
Peter D. Clift ◽  
Guangsheng Zhuang ◽  
Bowen Song ◽  
...  
Keyword(s):  
High Resolution ◽  
Tibetan Plateau ◽  
Qaidam Basin ◽  
Northeastern Tibetan Plateau

scholarly journals High‐Resolution Eocene Magnetostratigraphy of the Xijigou Section: Implications for the Infilling Process of Xining Basin, Northeastern Tibetan Plateau

2019 ◽  
Vol 124 (8) ◽  
pp. 7588-7603 ◽  
Author(s):  
Fan Yang ◽  
Zhengtang Guo ◽  
Chunxia Zhang ◽  
Sayem Abu Sadat Md ◽  
Zhilin He ◽  
...  
Keyword(s):  
High Resolution ◽  
Tibetan Plateau ◽  
Northeastern Tibetan Plateau ◽  
Xining Basin

A new growth model of the northeastern Tibetan Plateau from high-resolution seismic imaging by improved double-difference tomography

2021 ◽  
Vol 798 ◽  
pp. 228699
Author(s):  
Quan Sun ◽  
Shunping Pei ◽  
Zhongxiong Cui ◽  
Y. John Chen ◽  
Yanbing Liu ◽  
...  
Keyword(s):  
High Resolution ◽  
Tibetan Plateau ◽  
Growth Model ◽  
Seismic Imaging ◽  
Double Difference ◽  
Northeastern Tibetan Plateau

scholarly journals An Early Miocene Lowland on the Northeastern Tibetan Plateau

2021 ◽  
Vol 9 ◽  
Author(s):  
Qian Tian ◽  
Xiaomin Fang ◽  
Yan Bai ◽  
Chihao Chen ◽  
Juzhi Hou ◽  
...  
Keyword(s):  
Tibetan Plateau ◽  
Sea Level ◽  
Late Miocene ◽  
Qaidam Basin ◽  
Early Miocene ◽  
Annual Average ◽  
Northeastern Tibetan Plateau ◽  
The Mean ◽  
First Time ◽  
Glycerol Dialkyl Glycerol Tetraethers

The northeastern Tibetan Plateau (NE TP) has long been thought to be the last part of the Plateau to be raised, but this assumption has been challenged by recent analyses of fossil leaf energy, which have pointed to the possibility that the present surface altitude of ∼3,000 m above sea level (asl) in the Qaidam Basin (QB) was attained during the Oligocene. Here, for the first time, we present a record of glycerol dialkyl glycerol tetraethers (GDGTs) from a well-dated Cenozoic section in the QB. This record appears to demonstrate that the mean annual average paleotemperature of the QB was 28.4 ± 2.9°C at ∼18.0 Ma. This would suggest that the paleoelevation of the QB was only ∼1,488 m asl at that time and that a ∼1,500 m uplift was attained afterwards, in agreement with the massive shortening of the QB and the rapid drying of inland Asia since the late Miocene.

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