Gas hydrate destabilization: enhanced dewatering, benthic material turnover and large methane plumes at the Cascadia convergent margin-Reference-Cited by-同舟云学术

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Gas hydrate destabilization: enhanced dewatering, benthic material turnover and large methane plumes at the Cascadia convergent margin

Published:1999-06 Issue:1-2 Volume:170 Page:1-15
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Suess E.,Torres M.E.,Bohrmann G.,Collier R.W.,Greinert J.,Linke P.,Rehder G.,Trehu A.,Wallmann K.,Winckler G.,Zuleger E.

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference45 articles.

1. Landward vergence and oblique structural trends in the Oregon margin accretionary prism: implications and effect on fluid flow;MacKay;Earth Planet. Sci. Lett.,1992

2. Oregon subduction zone: venting, fauna, and carbonates;Kulm et al;Science,1986

3. B. Carson, G.K. Westbrook, Modern fluid flow in the Cascadia accretionary wedge: A synthesis, in: Carson, B., Westbrook, G.K., Musgrave, R.J., Suess, E. (Eds.), Proc. Ocean Drill. Program Sci. Results 146 (1995) 413–424.

4. M. Kastner, K.A. Kvenvolden, M.J. Whiticar, A. Camerlenghi, T.D. Lorenson, Relation between pore fluid chemistry and gas hydrates associated with bottom-simulating reflectors at the Cascadia margin, sites 889 and 892, in: Carson, B., Westbrook, G.K., Musgrave, R.J., Suess, E. (Eds.), Proc. Ocean Drill. Program Sci. Results 146 (1995) 175–187.

5. Methane hydrate stability in pore water: a simple theoretical approach for geophysical applications;Dickens;J. Geophys. Res.,1997

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