Changing Brine Inputs Into Hydrothermal Fluids: Southern Cleft Segment, Juan de Fuca Ridge-Reference-Cited by-同舟云学术

Changing Brine Inputs Into Hydrothermal Fluids: Southern Cleft Segment, Juan de Fuca Ridge

Published:2020-10-31 Issue:11 Volume:21 Page:
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Wheat C. Geoffrey¹^ORCID,Zierenberg Robert A.²^ORCID,Paduan Jennifer B.³^ORCID,Caress David W.³^ORCID,Clague David A.³^ORCID,Chadwick William W.⁴^ORCID

Affiliation:

1. Institute of Marine Sciences College of Fisheries and Ocean Sciences University of Alaska Fairbanks Moss Landing CA USA

2. Department of Earth and Planetary Sciences University of California Davis Davis CA USA

3. Monterey Bay Aquarium Research Institute Moss Landing CA USA

4. Cooperative Institute for Marine Resources Studies (CIMRS) Hatfield Marine Science Center Oregon State University Newport OR USA

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020GC009360

Reference83 articles.

1. A simple predictive model of quartz solubility in water–salt–CO2 systems at temperatures up to 1000°C and pressures up to 1000MPa

2. Cataclysmic hydrothermal venting on the Juan de Fuca Ridge

3. Hydrothermal event plumes from the coaxial seafloor eruption site, Juan de Fuca Ridge

4. Geothermal energy and ore-forming potential of 600 °C mid-ocean-ridge hydrothermal fluids

5. An empirical equation of state for hydrothermal seawater (3.2 percent NaCl)

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