Rupture of wet mantle wedge by self-promoting carbonation

Abstract More than one teramole of carbon per year is subducted as carbonate or carbonaceous material. However, the influence of carbonation/decarbonation reactions on seismic activity within subduction zones is poorly understood. Here we present field and microstructural observations, including sta...

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Published inCommunications earth & environment Vol. 2; no. 1; pp. 1 - 10
Main Authors Okamoto, Atsushi, Oyanagi, Ryosuke, Yoshida, Kazuki, Uno, Masaoki, Shimizu, Hiroyuki, Satish-Kumar, Madhusoodhan
Format Journal Article
LanguageEnglish
Published London Nature Publishing Group 03.08.2021
Nature Portfolio
Subjects
Brittle fracture
Carbonaceous materials
Carbonates
Carbonation
Computational fluid dynamics
Contraction
Decarbonation
Dehydration
Ductile fracture
Ductile-brittle transition
Isotopes
Lava
Magnesium
Minerals
Organic materials
Overpressure
Oxygen isotopes
Seismic activity
Seismicity
Stable isotopes
Subduction (geology)
Japan
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Abstract Abstract More than one teramole of carbon per year is subducted as carbonate or carbonaceous material. However, the influence of carbonation/decarbonation reactions on seismic activity within subduction zones is poorly understood. Here we present field and microstructural observations, including stable isotope analyses, of carbonate veins within the Higuchi serpentinite body, Japan. We find that the carbon and oxygen isotope compositions of carbonate veins indicate that carbonic fluids originated from organic materials in metasediments. Thermodynamic calculations reveal that carbonation of serpentinite was accompanied by a solid volume decrease, dehydration, and high magnesium mobility. We propose that carbonation of the mantle wedge occurs episodically in a self-promoting way and is controlled by a solid volume contraction and fluid overpressure. In our conceptual model, brittle fracturing and carbonate precipitation were followed by ductile flow of carbonates and hydrous minerals; this might explain the occurrence of episodic tremor and slip in the serpentinized mantle wedge.
AbstractList More than one teramole of carbon per year is subducted as carbonate or carbonaceous material. However, the influence of carbonation/decarbonation reactions on seismic activity within subduction zones is poorly understood. Here we present field and microstructural observations, including stable isotope analyses, of carbonate veins within the Higuchi serpentinite body, Japan. We find that the carbon and oxygen isotope compositions of carbonate veins indicate that carbonic fluids originated from organic materials in metasediments. Thermodynamic calculations reveal that carbonation of serpentinite was accompanied by a solid volume decrease, dehydration, and high magnesium mobility. We propose that carbonation of the mantle wedge occurs episodically in a self-promoting way and is controlled by a solid volume contraction and fluid overpressure. In our conceptual model, brittle fracturing and carbonate precipitation were followed by ductile flow of carbonates and hydrous minerals; this might explain the occurrence of episodic tremor and slip in the serpentinized mantle wedge.Carbonation of a serpentinized mantle wedge is associated with volume reduction and fluid over-pressurization which drives brittle fracture and seismicity, according to chemical analyses of carbonate veins from the Sanbagawa belt Japan and thermodynamic calculations.
Abstract More than one teramole of carbon per year is subducted as carbonate or carbonaceous material. However, the influence of carbonation/decarbonation reactions on seismic activity within subduction zones is poorly understood. Here we present field and microstructural observations, including stable isotope analyses, of carbonate veins within the Higuchi serpentinite body, Japan. We find that the carbon and oxygen isotope compositions of carbonate veins indicate that carbonic fluids originated from organic materials in metasediments. Thermodynamic calculations reveal that carbonation of serpentinite was accompanied by a solid volume decrease, dehydration, and high magnesium mobility. We propose that carbonation of the mantle wedge occurs episodically in a self-promoting way and is controlled by a solid volume contraction and fluid overpressure. In our conceptual model, brittle fracturing and carbonate precipitation were followed by ductile flow of carbonates and hydrous minerals; this might explain the occurrence of episodic tremor and slip in the serpentinized mantle wedge.
Carbonation of a serpentinized mantle wedge is associated with volume reduction and fluid over-pressurization which drives brittle fracture and seismicity, according to chemical analyses of carbonate veins from the Sanbagawa belt Japan and thermodynamic calculations.
ArticleNumber 151
Author Uno, Masaoki
Oyanagi, Ryosuke
Shimizu, Hiroyuki
Yoshida, Kazuki
Satish-Kumar, Madhusoodhan
Okamoto, Atsushi
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Snippet Abstract More than one teramole of carbon per year is subducted as carbonate or carbonaceous material. However, the influence of carbonation/decarbonation...
More than one teramole of carbon per year is subducted as carbonate or carbonaceous material. However, the influence of carbonation/decarbonation reactions on...
Carbonation of a serpentinized mantle wedge is associated with volume reduction and fluid over-pressurization which drives brittle fracture and seismicity,...
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StartPage 1
SubjectTerms Brittle fracture
Carbonaceous materials
Carbonates
Carbonation
Computational fluid dynamics
Contraction
Decarbonation
Dehydration
Ductile fracture
Ductile-brittle transition
Isotopes
Lava
Magnesium
Minerals
Organic materials
Overpressure
Oxygen isotopes
Seismic activity
Seismicity
Stable isotopes
Subduction (geology)
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Title Rupture of wet mantle wedge by self-promoting carbonation
URI https://www.proquest.com/docview/2557673340/abstract/
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