Preferential Formation of Chlorite Over Talc During Si‐Metasomatism of Ultramafic Rocks in Subduction Zones-Reference-Cited by-同舟云学术

Preferential Formation of Chlorite Over Talc During Si‐Metasomatism of Ultramafic Rocks in Subduction Zones

Published:2022-10-07 Issue:19 Volume:49 Page:
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophysical Research Letters

Author:

Codillo E. A.¹²^ORCID,Klein F.³^ORCID,Marschall H. R.²⁴^ORCID

Affiliation:

1. Massachusetts Institute of Technology/Woods Hole Oceanographic Institution Joint Program in Oceanography/Applied Ocean Science and Engineering Woods Hole MA USA

2. Department of Geology and Geophysics Woods Hole Oceanographic Institution Woods Hole MA USA

3. Department of Marine Chemistry and Geochemistry Woods Hole Oceanographic Institution Woods Hole MA USA

4. Institut für Geowissenschaften Goethe Universität Frankfurt Frankfurt am Main Germany

Funder

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2022GL100218

Reference89 articles.

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3. Models of permeability contrasts in subduction zone mélange: Implications for gradients in fluid fluxes, Syros and Tinos Islands, Greece

4. Teleseismic constraints on the geological environment of deep episodic slow earthquakes in subduction zone forearcs: A review

5. Exposed plate interface in the European Alps reveals fabric styles and gradients related to an ancient seismogenic coupling zone

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