Neotectonic subsidence along the Cenozoic Kunlun fault (Tibetan Plateau)

Published: 21 September 2021| Version 1 | DOI: 10.17632/5839k8vdzx.1
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Description

Data refer to grain size and LOI data against calibrated ages

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Steps to reproduce

The data were retrieved from a sediment core with 1 cm resolution in the centre of the lake. Ages were retrieved by 14C AMS dating and Bayesian statistics

Categories

Tectonics Structure

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