Barium isotope behavior during interaction between serpentinite-derived fluids and metamorphic rocks in the continental subduction zone

Author:

Chen Anxia,Chen Yi-XiangORCID,Gu Xiaofeng,Zeng ZhenORCID,Xiao ZicongORCID,Schertl Hans-PeterORCID,Han XiqiuORCID,Zhao Zi-Fu,Huang FangORCID

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference112 articles.

1. Exhumation of oceanic blueschists and eclogites in subduction zones: Timing and mechanisms;Agard;Earth-Sci. Rev.,2009

2. Carbon dioxide released from subduction zones by fluid mediated reactions;Ague;Nat. Geosci.,2014

3. Variant across-forearc compositions of slab-fluids recorded by serpentinites: Implications on the mobilization of FMEs from an active subduction zone (Mariana forearc);Albers;Lithos,2020

4. Recycling of water, carbon, and sulfur during subduction of serpentinites: A stable isotope study of Cerro del Almirez, Spain;Alt;Earth Planet. Sci. Lett.,2012

5. Channelized fluid flow and eclogite-facies metasomatism along the subduction shear zone;Angiboust;J. Petrol.,2014

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