Fluid metasomatism of subducted continental crust: Insights from Si isotope compositions of metasomatic rocks from the Western and Eastern Alps-Reference-Cited by-同舟云学术

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Fluid metasomatism of subducted continental crust: Insights from Si isotope compositions of metasomatic rocks from the Western and Eastern Alps

Published:2024-04 Issue: Volume:470-471 Page:107503
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Yu Hui-Min,Shi Zhen,Chen Yi-Xiang,Schertl Hans-Peter,Wang Bao-Liang,Huang Fang

Funder

National Natural Science Foundation of China

Chinese Academy of Sciences

Natural Science Foundation of Anhui Province

West Light Foundation, Chinese Academy of Sciences

Publisher

Elsevier BV

Reference77 articles.

1. The role of serpentinites in cycling of carbon and sulfur: Seafloor serpentinization and subduction metamorphism;Alt;Lithos,2013

2. Early continental crust generated by reworking of basalts variably silicified by seawater;André;Nat. Geosci.,2019

3. Interactions between serpentinite devolatilization, metasomatism and strike-slip strain localization during deep-crustal shearing in the Eastern Alps;Barnes;J. Metamorph. Geol.,2004

4. The silicon isotopic composition of fine-grained river sediments and its relation to climate and lithology;Bayon;Geochim. Cosmochim. Acta,2018

5. Very-high pressure metamorphism of the Brossasco coronite metagranite, southern Dora Maira Massif, Western Alps;Biino;Schweiz. Mineral. Petrogr. Mitt.,1992

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