Tracing Sediment Source from the Nangqian Basin in the Eastern Tibetan Plateau Using Detrital Zircons: Insight into River and Paleoclimate Evolution

Name: Tracing Sediment Source from the Nangqian Basin in the Eastern Tibetan Plateau Using Detrital Zircons: Insight into River and Paleoclimate Evolution
Creator: Chenghao Jia
Published: 2025-04-09T08:01:32.600Z
Keywords: Geochemistry, Zircon

Jia, Chenghao

doi:10.17632/zrc6jm2jsd.1

Tracing Sediment Source from the Nangqian Basin in the Eastern Tibetan Plateau Using Detrital Zircons: Insight into River and Paleoclimate Evolution

Published: 9 April 2025| Version 1 | DOI: 10.17632/zrc6jm2jsd.1

Contributor:

Chenghao Jia

Description

Table S1.The zircon U-Pb age data set is derived from detrital zircons within sediments of different periods in the Nangqian Basin, located in the upper reaches of the Mekong River.

Tracing Sediment Source from the Nangqian Basin in the Eastern Tibetan Plateau Using Detrital Zircons: Insight into River and Paleoclimate Evolution

Description

Files

Categories

Licence