A Review of the Geological Constraints on the Conductive Boundary Layer at the Base of the Hydrothermal System at Mid‐Ocean Ridges-Reference-Cited by-同舟云学术

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A Review of the Geological Constraints on the Conductive Boundary Layer at the Base of the Hydrothermal System at Mid‐Ocean Ridges

Published:2019-01 Issue:1 Volume:20 Page:67-83
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Gillis K. M.¹^ORCID,Coogan L. A.¹^ORCID

Affiliation:

1. School of Earth and Ocean SciencesUniversity of Victoria Victoria British Columbia Canada

Funder

Natural Sciences and Engineering Research Council of Canada

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018GC007878

Reference85 articles.

1. Subsurface structure of a submarine hydrothermal system in ocean crust formed at the East Pacific Rise, ODP/IODP Site 1256

2. QUILF: A pascal program to assess equilibria among FeMgMnTi oxides, pyroxenes, olivine, and quartz

3. Seismic evidence that black smoker heat flux is influenced by localized magma replenishment and associated increases in crustal permeability

4. How many vent fields? New estimates of vent field populations on ocean ridges from precise mapping of hydrothermal discharge locations

5. Dehydration Melting and Water-Saturated Melting of Basaltic and Andesitic Greenstones and Amphibolites at 1, 3, and 6. 9 kb

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5. Quantifying the Axial Magma Lens Dynamics at the Roof of Oceanic Magma Reservoirs (Dike/Gabbro Transition): Oman Drilling Project GT3 Site Survey;Journal of Geophysical Research: Solid Earth;2021-05

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