Tectonic transition from continental subduction to orogenic collapse recorded by ultrahigh-pressure to ultrahigh-temperature metamorphism-Reference-Cited by-同舟云学术

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Tectonic transition from continental subduction to orogenic collapse recorded by ultrahigh-pressure to ultrahigh-temperature metamorphism

Published:2024-07 Issue: Volume:638 Page:118743
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Dong Jie^ORCID,Wei Chunjing,Yin An,Han Bao-Fu^ORCID,Song Shuguang

Funder

China Postdoctoral Science Foundation

National Natural Science Foundation of China

Publisher

Elsevier BV

Reference70 articles.

1. Lithosphere structure in Europe from thermal isostasy;Artemieva;Earth-Sci. Rev.,2019

2. Zircon and monazite ages constraints on devonian magmatism and granulite-facies metamorphism in the southern qaidam block: implications for evolution of Proto-and Paleo-Tethys in East Asia;Ba;J. Earth Sci.,2018

3. HP–UHT granulites in the East Kunlun Orogen, NW China: constraints on the transition from compression to extension in an arc setting of the Proto-Tethys Ocean;Bi;J. Metamorph. Geol.,2021

4. UHP metamorphism recorded by coesite-bearing metapelite in the East Kunlun Orogen (NW China) UHP metamorphism recorded by coesite-bearing metapelite;Bi;Geol. Mag.,2020

5. HP–UHP eclogites in the East Kunlun Orogen, China: P–T evidence for asymmetric suturing of the Proto-Tethys Ocean;Bi;Gondwana Res.,2022

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