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Journal ArticleDOI

Carbon dioxide released from subduction zones by fluid-mediated reactions

TLDR
In this paper, the balance between carbonate subduction into the deep Earth and CO2 release through degassing at volcanoes is critical for the carbon cycle, and fluid-mediated reactions could liberate significant amounts of carbon from the subducting slab for later release at arc volcanoes.
Abstract
The balance between carbonate subduction into the deep Earth and CO2 release through degassing at volcanoes is critical for the carbon cycle. Geochemical analyses of an exhumed subduction zone complex in Greece show that fluid-mediated reactions could liberate significant amounts of carbon from the subducting slab for later release at arc volcanoes.

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Citations
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Reevaluating carbon fluxes in subduction zones, what goes down, mostly comes up.

TL;DR: Carbon fluxes in subduction zones can be better constrained by including new estimates of carbon concentration in subducting mantle peridotites, consideration of carbonate solubility in aqueous fluid along subduction geotherms, and diapirism of carbon-bearing metasediments.
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Slab melting as a barrier to deep carbon subduction

TL;DR: It is shown that the majority of slab geotherms will intersect a deep depression along the melting curve of carbonated oceanic crust at depths of approximately 300 to 700 kilometres, creating a barrier to direct carbonate recycling into the deep mantle.
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The Global Range of Subduction Zone Thermal Structures from Exhumed Blueschists and Eclogites: Rocks Are Hotter than Models

TL;DR: In this article, the authors compare the maximum pressure P-T conditions of exhumed subduction-related metamorphic rocks with those predicted by computational thermal models of subduction systems.
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Fluid and mass transfer at subduction interfaces-The field metamorphic record

TL;DR: In this article, the authors consider records of fluid and mass transfer at localities representing various depths and structural expressions of evolving paleo-interfaces, ranging widely in structural character, the rock types involved, and the rheology of these rocks.
References
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Journal ArticleDOI

An internally consistent thermodynamic data set for phases of petrological interest

TL;DR: In this paper, the thermodynamic properties of 154 mineral endmembers, 13 silicate liquid end-members and 22 aqueous fluid species are presented in a revised and updated data set.
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The chemical composition of subducting sediment and its consequences for the crust and mantle

TL;DR: This article evaluated subducting sediments on a global basis in order to better define their chemical systematics and to determine both regional and global average compositions, and then used these compositions to assess the importance of sediments to arc volcanism and crust-mantle recycling, and to re-evaluate the chemical composition of the continental crust.
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Computation of phase equilibria by linear programming: A tool for geodynamic modeling and its application to subduction zone decarbonation

TL;DR: In this article, an algorithm for the construction of phase diagram sections is formulated that is well suited for geodynamic problems in which it is necessary to assess the influence of phase transitions on rock properties or the evolution and migration of fluids.
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The global range of subduction zone thermal models

TL;DR: In this article, a suite of thermal models for the global subduction system is presented, where the authors model 56 segments of subduction zones using kinematically defined slabs based on updated geometries from Syracuse and Abers (2006).
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The deep carbon cycle and melting in Earth's interior

TL;DR: Carbon geochemistry of mantle-derived samples suggests that the fluxes and reservoir sizes associated with deep cycle are in the order of 1012−13−g−C/yr and 1022−23−g C, respectively.
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