Paleolake salinity evolution in the Qaidam Basin (NE Tibetan Plateau) between ~42 and 29 Ma: Links to global cooling and Paratethys sea incursions
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DOI: 10.1016/j.sedgeo.2020.105778
Abstract: Abstract Climate change in the Asian interior during the early Cenozoic remains poorly constrained due to difficulties in distinguishing the impacts of global cooling, the early uplift of the Tibetan Plateau and the retreat of… read more here.
Keywords: qaidam basin; global cooling; paleolake salinity; salinity ... See more keywords