In the Kunlun Mountains Pass area, all the landform, structure, sedimentary facies and assembladge of organisms show that a violent tectonic movement occurred between 1.1-0.7 MaB.P. The movement leads to a large-scale uplifting first, and then fault-block rising and fault depression occurred suddenly in the northern Plateau. In the late period of this movement, sudden and tremendous uplifting raised this area over the critical elevation of 3 000 m and caused the appearance of the maximum glaciation in Quaternary. This uplifting is perhaps the driving terce of the tremendous environmental change of tectonic-climatic circulation at the break of the early and middle Pleistocene in China.Geosciences, MultidisciplinarySCI(E)EI21ARTICLE6592-6004
A new division of Middle and Late Pleistocene alluvial sequence in the north piedmont of the Chinese...
Abstract The Qaidam Basin in Northern Tibet is one of the largest hyper-arid intermontane basins on ...
Forming the western branches of the East Kunlun Mountains,the bow-like Qimen Tagh Mountains separate...
Based on geomorphological, tectonic and sedimentary data, a Kunlun Yellow River Tectonic Movement ha...
There is a set of Late Cenozoic sediments in the Kunlun Pass area, Tibetan Plateau, China. Paleomagn...
The Kunlun Pass Basin, located in the middle of the eastern Kunlun Mountains, received relatively co...
The Taiyuan Graben and the Linfen Graben are two fault-controlled grabens in the Fen River basin, no...
Fieldwork south of the city of Gaotai (Gansu province, China) shows that active shortening of surfac...
The Shanxi Graben System is composed of a series of normal fault-controlled basins which are arrange...
Late Pleistocene glaciation was restricted to only a few high mountains in eastern China.The Gongwan...
The geomorphological evolution of the Northeastern Tibetan Plateau (NETP) could provide valuable inf...
In the Kunlun Pass area of northern Tibet, glacial landforms and sediments provide evidence for thre...
Coming by way of the great desert corridors which run along the northern borders of Tibet, thick aeo...
The timing of crustal shortening and strike-slip faulting along the East Kunlun Shan provides insigh...
cn) Abstract The Quaternary Tailan River fault has been found in the Tianshan foothills area, the Xi...
A new division of Middle and Late Pleistocene alluvial sequence in the north piedmont of the Chinese...
Abstract The Qaidam Basin in Northern Tibet is one of the largest hyper-arid intermontane basins on ...
Forming the western branches of the East Kunlun Mountains,the bow-like Qimen Tagh Mountains separate...
Based on geomorphological, tectonic and sedimentary data, a Kunlun Yellow River Tectonic Movement ha...
There is a set of Late Cenozoic sediments in the Kunlun Pass area, Tibetan Plateau, China. Paleomagn...
The Kunlun Pass Basin, located in the middle of the eastern Kunlun Mountains, received relatively co...
The Taiyuan Graben and the Linfen Graben are two fault-controlled grabens in the Fen River basin, no...
Fieldwork south of the city of Gaotai (Gansu province, China) shows that active shortening of surfac...
The Shanxi Graben System is composed of a series of normal fault-controlled basins which are arrange...
Late Pleistocene glaciation was restricted to only a few high mountains in eastern China.The Gongwan...
The geomorphological evolution of the Northeastern Tibetan Plateau (NETP) could provide valuable inf...
In the Kunlun Pass area of northern Tibet, glacial landforms and sediments provide evidence for thre...
Coming by way of the great desert corridors which run along the northern borders of Tibet, thick aeo...
The timing of crustal shortening and strike-slip faulting along the East Kunlun Shan provides insigh...
cn) Abstract The Quaternary Tailan River fault has been found in the Tianshan foothills area, the Xi...
A new division of Middle and Late Pleistocene alluvial sequence in the north piedmont of the Chinese...
Abstract The Qaidam Basin in Northern Tibet is one of the largest hyper-arid intermontane basins on ...
Forming the western branches of the East Kunlun Mountains,the bow-like Qimen Tagh Mountains separate...