Data for: Paleolake salinity evolution in the Qaidam Basin (NE Tibetan Plateau) in ~42-29 Ma: Links to global cooling and Paratethys retreat

Published: 19-10-2020| Version 1 | DOI: 10.17632/dmj66h9xyx.1
Contributor:
Yibo Yang

Description

This dataset provides a quantitative boron-derived paleosalinity (~42-29 Ma) in the Hongliugou section in the Qaidam Basin.

Files