Normal faulting and mass movement during ridge subduction inferred from porosity transition and zeolitization in the Costa Rica subduction zone-Reference-Cited by-同舟云学术

Normal faulting and mass movement during ridge subduction inferred from porosity transition and zeolitization in the Costa Rica subduction zone

Published:2017-07 Issue:7 Volume:18 Page:2601-2616
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Hamahashi Mari¹²³^ORCID,Screaton Elizabeth⁴^ORCID,Tanikawa Wataru⁵^ORCID,Hashimoto Yoshitaka⁶^ORCID,Martin Kylara⁷⁸^ORCID,Saito Saneatsu⁹^ORCID,Kimura Gaku¹¹⁰^ORCID

Affiliation:

1. Department of Earth and Planetary Science, Graduate School of Science; The University of Tokyo; Tokyo Japan

2. Geological Survey of Japan; National Institute of Advanced Industrial Science and Technology; Ibaraki Japan

3. Now at Earth Observatory of Singapore; Nanyang Technological University; Singapore

4. Department of Geological Sciences; University of Florida; Gainesville Florida USA

5. Kochi Institute for Core Sample Research, Japan Agency for Marine-Earth Science and Technology; Nankoku-shi Kochi Japan

6. Department of Applied Science, Faculty of Science; Kochi University; Kochi-shi Kochi Japan

7. Naval Research Laboratory; Stennis Space Center, Hancock County; Mississippi USA

8. Now at The University of Texas, Institute for Geophysics; Austin Texas USA

9. Research and Development Center for Ocean Drilling Science, Japan Agency for Marine-Earth Science and Technology; Yokohama-shi Kanagawa Japan

10. Now at Tokyo University of Marine Science and Technology; Minato-ku Tokyo Japan

Funder

JSPS Grants-in-Aid for Scientific Research Fellowship for Young Scientists

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/2016GC006577/fullpdf

Reference57 articles.

1. Polymorphismm and crystal-chemistry of heulandites and clinoptilolites;Alietti;Am. Mineral.,1972

2. The electrical resistivity log as an aid in determining some reservoir characteristics;Archie;Trans. AIME,1942

3. Interplate seismicity at the CRISP drilling site: The 2002 Mw 6.4 Osa Earthquake at the southeastern end of the Middle America Trench;Arroyo;Geochem. Geophys. Geosyst.,2014

4. Fluid accumulation along the Costa Rica subduction thrust and development of the seismogenic zone;Bangs;J. Geophys. Res. Solid Earth,2015

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