supported by grants from the China Geological Survey(Grant Nos.1212010610102,DD20190065).
The Tibetan Plateau is an important area for studying global climate change,but the answers to many scientific problems remain unknown.Here,we present new information from the lacustrine sedimentary record in the west...
supported by the National Natural Science Foundation of China (Grant Nos. 41902190 and 42003044);the Geological Survey Project of China (Grant No. DD20221913);the Qinghai Geological Exploration Fund (Grant No. 2020021068kc035)。
The Quaternary was the main evaporite deposition period in the Qaidam Basin(QB), but the correlation between the evaporite deposition period and the glacial period is still unclear. In this study, the research objects...
supported by the China Geological Survey(grant Nos.DD20160048-04 and DD20179402-01 DD20179402-02);the National Natural Science Foundation of China(grant No.41702032)
Objective Northeast China is located in a cold region with high latitude. In the mid-low mountain areas, the existence of Quaternary glacier as well as its range and nature are always controversial. The glacial paleo...
How to effectively identify glacial sediments, especially Quaternary moraine, has been in dispute for decades. The traditional methods, e.g., sedimentary and geomorphologic ones, are facing challenge in eastern China ...
The detailed geological mapping, conducted in the Damxung-Yangbajain basin, shows that there are many types of deposits formed since the Pliocene. The oldest sediments are formed during the Pliocene. The most prominen...