Late Eocene clay boron-derived paleosalinity in the Qaidam Basin and its implications for regional tectonics and climate
Abstract The Qaidam Basin, located on the northeastern Tibetan Plateau and containing
Cenozoic sediments with a maximum thickness of~ 12,000 m, is an ideal place to study the
phased uplift of the NE Tibetan Plateau and regional climate change. The estimation of the
paleosalinity of sedimentary environments not only helps to evaluate the evolution of lakes
in this region but offers insights into contemporaneous climate change. We present detailed
geochemical and mineralogical investigations from the lacustrine interval of the Hongliugou …
Cenozoic sediments with a maximum thickness of~ 12,000 m, is an ideal place to study the
phased uplift of the NE Tibetan Plateau and regional climate change. The estimation of the
paleosalinity of sedimentary environments not only helps to evaluate the evolution of lakes
in this region but offers insights into contemporaneous climate change. We present detailed
geochemical and mineralogical investigations from the lacustrine interval of the Hongliugou …
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