scholarly journals Neogene sedimentary evolution of the Guide Basin and its implications on uplift of the NE Tibetan Plateau, China

1970 ◽  
Vol 5 (7) ◽  
pp. 154
Author(s):  
Chunhui Song ◽  
Qingquan Meng ◽  
Xiaomin Fang ◽  
Shuang Dai ◽  
Junping Gao

DOI = 10.3126/hjs.v5i7.1333 Himalayan Journal of Sciences Vol.5(7) (Special Issue) 2008 p.154

2005 ◽  
Vol 117 (9) ◽  
pp. 1208 ◽  
Author(s):  
Xiaomin Fang ◽  
Maodu Yan ◽  
Rob Van der Voo ◽  
David K. Rea ◽  
Chunhui Song ◽  
...  

2019 ◽  
Vol 131 (9-10) ◽  
pp. 1744-1760 ◽  
Author(s):  
Xiaofei Hu ◽  
Dianbao Chen ◽  
Baotian Pan ◽  
Jinjun Chen ◽  
Jian Zhang ◽  
...  

AbstractWe studied the magnetostratigraphy and sedimentary facies of a 550-m-long drill core from the Jiudong Basin in the NE Tibetan Plateau. Our aims were to reconstruct the late Cenozoic sedimentary evolution of this foreland basin, and to determine the spatiotemporal pattern of growth of the Qilian Shan. The magnetostratigraphy indicates that the sedimentary sequence was deposited during ca. 7–0 Ma. From ca. 6.7–3.0 Ma, the sediment accumulation rate increased gradually from ∼30 mm/k.y. to 120 mm/k.y., which was associated with the gradual evolution of sedimentary facies from a shallow lake/delta front to braided rivers. The progradation of the depositional system from 7 Ma to 3 Ma probably reflects the growth of the relief of the Qilian Shan caused by tectonic uplift. The occurrence of a continuous braided river environment from 3 Ma to the present suggests that the high relief of the Qilian Shan developed before 3 Ma. An abrupt decrease of the sedimentation rate to ∼46 mm/k.y. during 3.0–1.8 Ma, and the deposition of coarse-grained sediments, indicates the uplift of the basin center. We interpret this to reflect the propagation of the thrust system of the Qilian Shan into the basin along a southward-dipping décollement from ca. 3 Ma. Climatic changes may have influenced the sedimentary sequence by introducing long-distance-transported thin coarse sand/gravel layers which are sandwiched within the sequence, and likely were a response to cooling events or climatic transitions. The widespread occurrence of deformation within the basin region in the NE Tibetan Plateau at ca. 3 Ma indicates that this date marks the basinward growth of the deformation system.


2017 ◽  
Vol 478 ◽  
pp. 66-75 ◽  
Author(s):  
Zhouchuan Huang ◽  
Frederik Tilmann ◽  
Mingjie Xu ◽  
Liangshu Wang ◽  
Zhifeng Ding ◽  
...  

Lithos ◽  
2019 ◽  
Vol 344-345 ◽  
pp. 374-392 ◽  
Author(s):  
Jun-Qiang Hu ◽  
Xiao-Wei Li ◽  
Ji-Feng Xu ◽  
Xuan-Xue Mo ◽  
Fang-Yue Wang ◽  
...  

2015 ◽  
Vol 37 (1) ◽  
pp. i ◽  
Author(s):  
Shikui Dong ◽  
Ruth Sherman

This special issue covers a wide range of topics on the protection and sustainable management of alpine rangelands on the Qinghai-Tibetan Plateau (QTP), including Indigenous knowledge of sustainable rangeland management, science-policy interface for alpine rangeland biodiversity conservation, adaptations of local people to social and environmental changes and policy design for managing coupled human-natural systems of alpine rangelands.


2021 ◽  
Vol 252 ◽  
pp. 106736
Author(s):  
Dada Yan ◽  
Bernd Wünnemann ◽  
Georg Stauch ◽  
Yongzhan Zhang ◽  
Hao Long

2021 ◽  
Vol 37 (8) ◽  
pp. 2401-2418
Author(s):  
FU ChangLei ◽  
◽  
YAN Zhen ◽  
XIAO WenJiao ◽  
WANG BingZhang ◽  
...  

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