Hydration of a Mantle Shear Zone Beyond Serpentine Stability: A Possible Link to Microseismicity Along Ultraslow Spreading Ridges?-Reference-Cited by-同舟云学术

Hydration of a Mantle Shear Zone Beyond Serpentine Stability: A Possible Link to Microseismicity Along Ultraslow Spreading Ridges?

Published:2020-10 Issue:10 Volume:125 Page:
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res. Solid Earth

Author:

Vieira Duarte J. F.¹²^ORCID,Kaczmarek M.‐A.¹³^ORCID,Vonlanthen P.¹^ORCID,Putlitz B.¹,Müntener O.¹^ORCID

Affiliation:

1. Institute of Earth Sciences, UNIL‐Mouline University of Lausanne Lausanne Switzerland

2. Institute of Geological Sciences University of Bern Bern Switzerland

3. Géosciences Environnement Toulouse (GET) CNRS‐CNES‐IRD‐Université de Toulouse III, Observatoire Midi Pyrénées Toulouse France

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020JB019509

Reference119 articles.

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3. O and H stable isotope compositions of oceanic crust and upper mantle rocks exposed in the Hess Deep near the Galapagos Triple Junction

4. Metasomatic hydrous fluids in amphibole peridotites from Zabargad Island (Red Sea)

5. Hydrothermal alteration of the peridotites cored at the ocean/continent boundary of the Iberian Margin: Petrologic and stable isotope evidence;Agrinier P.;Proceeding of the Ocean Drilling Program, Scientific Results,1988

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