Diagenetic, metamorphic, and hydrogeologic consequences of hydrothermal circulation in subducting crust-Reference-Cited by-同舟云学术

Diagenetic, metamorphic, and hydrogeologic consequences of hydrothermal circulation in subducting crust

Published:2018-10-24 Issue:6 Volume:14 Page:2337-2354
ISSN:1553-040X
Container-title:Geosphere
language:en
Short-container-title:

Author:

Spinelli Glenn¹,Wada Ikuko²,Wang Kelin³,He Jiangheng³,Harris Robert⁴,Underwood Michael¹

Affiliation:

1. Department of Earth & Environmental Science, New Mexico Tech, 801 Leroy Place, Socorro, New Mexico 87801, USA

2. Department of Earth Sciences, University of Minnesota, 116 Church Street SE, Minneapolis, Minnesota 55455, USA

3. Pacific Geoscience Centre, Geological Survey of Canada, Sidney, British Columbia V8L 4B2, Canada

4. College of Earth, Ocean, and Atmospheric Sciences (CEOAS), Oregon State University, 104 CEOAS Administration Building, Corvallis, Oregon 97331-5503, USA

Publisher

Geological Society of America

Subject

Stratigraphy,Geology

Link

https://pubs.geoscienceworld.org/gsa/geosphere/article-pdf/14/6/2337/4578757/2337.pdf

Reference159 articles.

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3. The cold and relatively dry nature of mantle forearcs in subduction zones;Abers;Nature Geoscience,2017

4. Hydrothermal alteration of a 1 km section through the upper oceanic crust, Deep Sea Drilling Project Hole 504B: Mineralogy, chemistry and evolution of seawater-basalt interactions;Alt;Journal of Geophysical Research,1986

5. Field-Based Evidence for Devolatilization in Subduction Zones: Implications for Arc Magmatism;Bebout;Science,1991

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