Record Details

Feeding methane vents and gas hydrate deposits at south Hydrate Ridge

ScholarsArchive at Oregon State University

Field Value
Title Feeding methane vents and gas hydrate deposits at south Hydrate Ridge
Names Tréhu, Anne Martine (creator)
Flemings, Peter B. (creator)
Bangs, Nathan Lawrence Bailey (creator)
Chevallier, Johanna (creator)
Gracia, Eulalia (creator)
Johnson, Joel E. (creator)
Liu, C. S. (creator)
Liu, Xiaoli (creator)
Riedel, Michael (creator)
Torres, Marta E. (creator)
Date Issued 2004-12-14 (iso8601)
Note Copyrighted by American Geophysical Union.
Abstract Log and core data document gas saturations as high as
90% in a coarse-grained turbidite sequence beneath the gas
hydrate stability zone (GHSZ) at south Hydrate Ridge, in the
Cascadia accretionary complex. The geometry of this gas-saturated
bed is defined by a strong, negative-polarity
reflection in 3D seismic data. Because of the gas buoyancy,
gas pressure equals or exceeds the overburden stress
immediately beneath the GHSZ at the summit. We
conclude that gas is focused into the coarse-grained
sequence from a large volume of the accretionary complex
and is trapped until high gas pressure forces the gas to migrate
through the GHSZ to seafloor vents. This focused flow
provides methane to the GHSZ in excess of its proportion in
gas hydrate, thus providing a mechanism to explain the
observed coexistence of massive gas hydrate, saline pore
water and free gas near the summit.
Genre Article
Identifier Tre´hu, A. M., P. B. Flemings, N. L. Bangs, J. Chevallier, E. Gra`cia, J. E. Johnson, C.-S. Liu, X. Liu, M. Riedel, and M. E. Torres (2004), Feeding methane vents and gas hydrate deposits at south Hydrate Ridge, Geophys. Res. Lett., 31, L23310.

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