Hydrothermal venting in magma deserts: The ultraslow-spreading Gakkel and Southwest Indian Ridges (Q104540876)

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Charles H. Langmuir

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object named as

Charles H. Langmuir

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author name string

Edward T. Baker

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Henrietta N. Edmonds

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Henry J. B. Dick

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Jonathan E. Snow

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Sharon L. Walker

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Neil R. Banerjee

G3: Geochemistry, Geophysics, Geosystems

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publication date

August 2004

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published in

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volume

5

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issue

8

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cites work

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

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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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Geochemistry of high H2 and CH4 vent fluids issuing from ultramafic rocks at the Rainbow hydrothermal field (36°14′N, MAR)

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An ultraslow-spreading class of ocean ridge

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Hydrothermal activity along the southwest Indian ridge

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Geophysical evidence for reduced melt production on the Arctic ultraslow Gakkel mid-ocean ridge.

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

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Larval dispersal potential of the tubeworm Riftia pachyptila at deep-sea hydrothermal vents

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Magmatic and amagmatic seafloor generation at the ultraslow-spreading Gakkel ridge, Arctic Ocean.

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Melt Generation at Very Slow-Spreading Oceanic Ridges: Constraints from Geochemical and Geophysical Data

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