Recognition of tuffs in the middle-upper Dingqinghu Fm., Lunpola Basin, central Tibetan Plateau: Constraints on stratigraphic age and implications for paleoclimate
Ziqiang Mao(Chinese Academy of Sciences), Mengqi Tan(Chinese Academy of Sciences), Fuli Wu(Chinese Academy of Sciences), Qingquan Meng(Lanzhou University), Tao Zhang(Chinese Academy of Sciences), Yibo Yang(Chinese Academy of Sciences), Weilin Zhang(Chinese Academy of Sciences), Xiaomin Fang(Chinese Academy of Sciences), Jinbo Zan(Chinese Academy of Sciences)
Cited by 36
Related Papers
Paleomagnetic data bearing on the Mesozoic deformation of the Qiangtang Block: Implications for the evolution of the Paleo- and Meso-Tethys
|Gondwana Research|2016|152
The 3.6-Ma aridity and westerlies history over midlatitude Asia linked with global climatic cooling
|Proceedings of the National Academy of Sciences|2020|140
Cenozoic magnetostratigraphy of the Xining Basin, NE Tibetan Plateau, and its constraints on paleontological, sedimentological and tectonomorphological evolution
|Earth-Science Reviews|2019|138
Tectonosedimentary evolution model of an intracontinental flexural (foreland) basin for paleoclimatic research
|Global and Planetary Change|2016|110
Paleogeography control of Indian monsoon intensification and expansion at 41 Ma
|Science Bulletin|2021|96