Relationship between carbonate deposits and fluid venting: Oregon Accretionary Prism-Reference-Cited by-同舟云学术

Relationship between carbonate deposits and fluid venting: Oregon Accretionary Prism

Published:1990 Issue:B6 Volume:95 Page:8899
ISSN:0148-0227
Container-title:Journal of Geophysical Research
language:en
Short-container-title:J. Geophys. Res.

Author:

Kulm LaVerne D.,Suess Erwin

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Link

http://www.agu.org/journals/jb/v095/iB06/JB095iB06p08899/JB095iB06p08899.pdf

Reference33 articles.

1. The Washington continental slope: Quaternary tectonics and sedimentation;Barnard;Mar. Geol.,1978

2. Nankai Trough, Japan Trench and Kuril Trench: Geochemistry of fluids sampled by submersible “Nautile”;Boulègue;Earth Planet. Sci. Lett.,1987

3. Deep-sea hydrocarbon seep communities: Evidence for energy and nutritional carbon sources;Brooks;Science,1987

4. Biology and ecology of shallow vents associated with the Oregon continental shelf edge;Carey;Global Venting, Midwater, and Benthic Ecological Processes,1988

5. Fluid flow and mass flux determinations at vent sites on the Cascadia margin accretionary prism;Carson;J. Geophys. Res.,1990

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