Evidence for Low‐Temperature Diffuse Venting at North Pond, Western Flank of the Mid‐Atlantic Ridge-Reference-Cited by-同舟云学术

Evidence for Low‐Temperature Diffuse Venting at North Pond, Western Flank of the Mid‐Atlantic Ridge

Published:2019-06 Issue:6 Volume:20 Page:2572-2584
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Villinger H. W.¹^ORCID,Müller P.¹^ORCID,Bach W.¹^ORCID,Becker K.²^ORCID,Orcutt B. N.³^ORCID,Kaul N.¹^ORCID,Wheat C. G.⁴^ORCID

Affiliation:

1. Department of Geosciences University of Bremen Bremen Germany

2. Department of Marine Geosciences, RSMAS University of Miami Miami FL USA

3. Bigelow Laboratory for Ocean Sciences East Boothbay ME USA

4. Global Undersea Research Unit University of Alaska Fairbanks Moss Landing CA USA

Funder

Deutsche Forschungsgemeinschaft

Office of the Director

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018GC008113

Reference47 articles.

1. Bach W. Edwards K. J. Girguis P. Glazer C. C. Hsieh B. Hulme S. Jaekel U. Lin H.‐T. Orcutt B. Thal J. Villinger H. Wheat C. G. Collasius A. Fernandez M. Hansen S. Hutchinson B. Kevis‐Stirling A. Pelowski J. Tradd B. Varnum J. &Verhein K.(2012).Borehole microbial observatory science in basaltic ocean crust: The North Pond area on the Western Mid‐Atlantic Ridge Flank at 23N Cruise No. MSM20/5 April 11–May 10 2012 Freeport (Bahamas)–St. John's (Canada).Bremen: Leitstelle Deutsche Forschungsschiffe Institut für Meereskunde der Universität Hamburg. https://doi.org/10.2312/cr_msm20_5

2. Exploring the ocean for hydrothermal venting: New techniques, new discoveries, new insights

3. Hydrothermal venting in magma deserts: The ultraslow-spreading Gakkel and Southwest Indian Ridges

4. Hydrothermal Plumes Over Spreading-Center Axes: Global Distributions and Geological Inferences

5. Idealised modelling of ocean circulation driven by conductive and hydrothermal fluxes at the seabed

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