Volatile‐Rich Hydrothermal Plumes Over the Southern Central Indian Ridge, 24°49’S: Evidence for a New Hydrothermal Field Hosted by Ultramafic Rocks-Reference-Cited by-同舟云学术

Volatile‐Rich Hydrothermal Plumes Over the Southern Central Indian Ridge, 24°49’S: Evidence for a New Hydrothermal Field Hosted by Ultramafic Rocks

Published:2022-10 Issue:10 Volume:23 Page:
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem Geophys Geosyst

Author:

Surya Prakash L.¹^ORCID,John Kurian P.¹^ORCID,Resing J. A.²^ORCID,Tsunogai U.³^ORCID,Srinivas Rao A.¹,Sen K.¹^ORCID,Lupton J. E.⁴^ORCID,Baumberger T.⁴⁵^ORCID,Prajith A.¹^ORCID,Roy P.¹

Affiliation:

1. National Centre for Polar and Ocean Research Ministry of Earth Sciences Vasco‐da‐Gama India

2. Cooperative Institute for Climate Oceans and Ecosystem Studies‐University of Washington and NOAA‐PMEL Seattle WA USA

3. Graduate School of Environmental Studies Nagoya University Nagoya Japan

4. Cooperative Institute of Marine Resources Studies Oregon State University Newport OR USA

5. NOAA Pacific‐Marine Environmental Laboratory Newport OR USA

Funder

Earth System Sciences Organization, Ministry of Earth Sciences

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2022GC010452

Reference105 articles.

1. Hydrothermal cooling along the Eastern Lau Spreading Center: No evidence for discharge beyond the neovolcanic zone

2. Fluid composition of the sediment-influenced Loki’s Castle vent field at the ultra-slow spreading Arctic Mid-Ocean Ridge

3. Contrasted hydrothermal activity along the South-East Indian Ridge (130°E-140°E): From crustal to ultramafic circulation

4. Chemical controls on the composition of vent fluids at 13°-11°N and 21°N, East Pacific Rise

5. Structural analysis of the segmentation of the Central Indian Ridge between 20�30?S and 25�30?S (Rodriguez Triple Junction)

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