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

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

Abstract Water column physico‐chemical studies were conducted over the southern Central Indian Ridge between 24°44’S and 25°52’S to identify and chemically characterize seafloor hydrothermal activity. High turbidity values were observed between 2300 and 2700 m with two distinct layers, between water...

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Bibliographic Details
Main Authors: L. Surya Prakash, P. John Kurian, J. A. Resing, U. Tsunogai, A. Srinivas Rao, K. Sen, J. E. Lupton, T. Baumberger, A. Prajith, P. Roy
Format: Article
Language:English
Published: Wiley 2022-10-01
Series:Geochemistry, Geophysics, Geosystems
Subjects:
southern Central Indian Ridge
hydrothermal plumes
dissolved trace metals
helium
methane
ultramafics
Online Access:https://doi.org/10.1029/2022GC010452

Internet

https://doi.org/10.1029/2022GC010452

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