Decoupled whole-rock and zircon Hf isotopes in young evolved post-collisional lavas from Dayingshan (SE Tibet): Evidence for open-system magmatic processes-Reference-Cited by-同舟云学术

Decoupled whole-rock and zircon Hf isotopes in young evolved post-collisional lavas from Dayingshan (SE Tibet): Evidence for open-system magmatic processes

Published:2021-11 Issue: Volume:400-401 Page:106393
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Guo Zipei,Zou Haibo

Funder

National Natural Science Foundation of China

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

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1. Hf-Nd isotope decoupling in S-type granitoids caused by disequilibrium melting of metasedimentary rocks: Evidence from the North Qinling Terrane, Central China;Lithos;2024-06

2. Reduced post-collisional magmas for Tengchong volcanoes, southeastern Tibetan Plateau;Journal of Asian Earth Sciences;2024-02

3. Temperature and Hf-O isotope correlations of young erupted zircons from Tengchong (SE Tibet): Assimilation fractional crystallization during monotonic cooling;Geoscience Frontiers;2023-01