Complex flow patterns through Hydrate Ridge and their impact on seep biota
- 15 July 2001
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 28 (14) , 2863-2866
- https://doi.org/10.1029/2000gl012566
Abstract
No abstract availableThis publication has 17 references indexed in Scilit:
- Authigenic carbonates from the Cascadia subduction zone and their relation to gas hydrate stabilityGeology, 1998
- The influence of pore‐water chemistry and physiology on the distribution of vesicomyid clams at cold seeps in Monterey Bay: Implications for patterns of chemosynthetic community organizationLimnology and Oceanography, 1997
- The Impact of Fluid and Gas Venting on Bacterial Populations and Processes in Sediments from the Cascadia Margin Accretionary System (Sites 888–892) and the Geochemical ConsequencesPublished by International Ocean Discovery Program (IODP) ,1995
- Long-Term Observations of Pressure and Temperature in Hole 892B, Cascadia Accretionary PrismPublished by International Ocean Discovery Program (IODP) ,1995
- Gas seep induced interstitial water circulation: observations and environmental implicationsContinental Shelf Research, 1995
- Gas hydrates—geological perspective and global changeReviews of Geophysics, 1993
- Interpretation of temperature measurements from the Kaiko-Nankai cruise: Modeling of fluid flow in clam coloniesEarth and Planetary Science Letters, 1992
- Landward vergence and oblique structural trends in the Oregon margin accretionary prism: Implications and effect on fluid flowEarth and Planetary Science Letters, 1992
- Fluid flow and mass flux determinations at vent sites on the Cascadia Margin Accretionary PrismJournal of Geophysical Research, 1990
- Oregon Subduction Zone: Venting, Fauna, and CarbonatesScience, 1986