Tectonic erosion and deep subduction in Central Tibet: Evidence from the discovery of retrograde eclogites in the Amdo microcontinent

Name: Tectonic erosion and deep subduction in Central Tibet: Evidence from the discovery of retrograde eclogites in the Amdo microcontinent
Creator: Yinbiao Peng
Published: 2022-06-29T14:12:26.077Z
Keywords: Metamorphic Geology

Peng, Yinbiao; Yu, Shengyao; Li, Sanzhong; Liu, Yongjiang; Santosh, M.; Lv, Pei; Li, Yunshuai; Li, Chuanzhi; Liu, Yiming

doi:10.17632/gtrd856zg8.1

Tectonic erosion and deep subduction in Central Tibet: Evidence from the discovery of retrograde eclogites in the Amdo microcontinent

Published: 29 June 2022| Version 1 | DOI: 10.17632/gtrd856zg8.1

Contributors:

Yinbiao Peng, Shengyao Yu, Sanzhong Li, Yongjiang Liu, M. Santosh, Pei Lv, Yunshuai Li, Chuanzhi Li, Yiming Liu

Description

This data shows the composition of representative minerals and geochemical data from the retrograde eclogites in Amdo microcontinent, wchic can be used to constrain the P-T conditions of eclogite. This data also shows the isotopic data of zircon and rutile, which can be used to constrain the metamorphism age of Amdo eclogite.

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Ocean University of China

Tectonic erosion and deep subduction in Central Tibet: Evidence from the discovery of retrograde eclogites in the Amdo microcontinent

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