Mantle refertilization at high-pressure conditions of continental subduction channel: Evidence from orogenic peridotites in the Sulu UHP terrane, eastern China-Reference-Cited by-同舟云学术

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Mantle refertilization at high-pressure conditions of continental subduction channel: Evidence from orogenic peridotites in the Sulu UHP terrane, eastern China

Published:2023-11 Issue: Volume:456-457 Page:107300
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Ren Aiqing,Wang Zaicong,Zong Keqing,Hu Zhaochu,Cheng Huai,Wang Xiang,Zhang Wen,Chen Weijun

Funder

National Natural Science Foundation of China

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference78 articles.

1. Metamorphic chemical geodynamics of subduction zones;Bebout;Earth Planet. Sci. Lett.,2007

2. 3.4 - Orogenic, ophiolitic, and abyssal peridotites;Bodinier,2014

3. Origin of pyroxenite–peridotite veined mantle by refertilization reactions: evidence from the ronda peridotite (Southern Spain);Bodinier;J. Petrol.,2008

4. Composition of the Siberian cratonic mantle: evidence from Udachnaya peridotite xenoliths;Boyd;Contrib. Mineral. Petrol.,1997

5. Geothermobarometry in four-phase Lherzolites II. New thermobarometers, and practical assessment of existing thermobarometers;Brey;J. Petrol.,1990

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1. Continental subduction-triggered carbonate metasomatism of the lithospheric mantle: Implications for the deep carbon cycle;Chemical Geology;2024-08

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