(Q104540880)

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Discovery of ancient and active hydrothermal systems along the ultra-slow spreading Southwest Indian Ridge 10°-16°E

scientific article published in July 2002

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Discovery of ancient and active hydrothermal systems along the ultra-slow spreading Southwest Indian Ridge 10°-16°E (English)

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Wolfgang Bach

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Neil R. Banerjee

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2

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Henry J. B. Dick

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3

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Edward T. Baker

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4

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publication date

July 2002

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published in

G3: Geochemistry, Geophysics, Geosystems

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volume

3

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issue

7

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1-14

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Methane-hydrogen gas seeps, Zambales Ophiolite, Philippines: Deep or shallow origin?

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Hydrothermal plumes along segments of contrasting magmatic influence, 15°20′-18°30′N, East Pacific Rise: Influence of axial faulting

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Occurrence of Sepiolite in the Lizard Serpentines

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Thin crust, ultramafic exposures, and rugged faulting patterns at the Mid-Atlantic Ridge (22°–24°N)

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Ultramafic and gabbroic exposures at the Mid-Atlantic Ridge: geological mapping in the 15°N region

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The rainbow vent fluids (36°14′N, MAR): the influence of ultramafic rocks and phase separation on trace metal content in Mid-Atlantic Ridge hydrothermal fluids

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Hydrothermal activity along the southwest Indian ridge

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Hot spring deposits on the East Pacific Rise at 21°N: preliminary description of mineralogy and genesis

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Initial indications of abiotic formation of hydrocarbons in the Rainbow ultramafic hydrothermal system, Mid-Atlantic Ridge

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Abiogenic methane formation and isotopic fractionation under hydrothermal conditions

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The internal structure of an active sea-floor massive sulphide deposit

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An off-axis hydrothermal vent field near the Mid-Atlantic Ridge at 30 degrees N.

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Relationship between spreading rate and the seismic structure of mid-ocean ridges

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Mineralization, alteration, and hydrothermal metamorphism of the ophiolite-hosted Turner-Albright sulfide deposit, southwestern Oregon

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Discovery of ancient and active hydrothermal systems along the ultra-slow spreading Southwest Indian Ridge 10°-16°E

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