Fluid expulsion related to mud extrusion off Costa Rica—A window to the subducting slab
- 1 January 2004
- journal article
- Published by Geological Society of America in Geology
- Vol. 32 (3)
- https://doi.org/10.1130/g20119.1
Abstract
No abstract availableThis publication has 24 references indexed in Scilit:
- Control of sulfate pore-water profiles by sedimentary events and the significance of anaerobic oxidation of methane for the burial of sulfur in marine sedimentsGeochimica et Cosmochimica Acta, 2003
- Fluid–sediment interactions at Eastern Mediterranean mud volcanoes: a stable isotope study from ODP Leg 160Published by Elsevier ,2003
- Widespread fluid expulsion along the seafloor of the Costa Rica convergent marginTerra Nova, 2002
- Lithium isotopic compositions of pore fluids and sediments in the Costa Rica subduction zone: implications for fluid processes and sediment contribution to the arc volcanoesEarth and Planetary Science Letters, 2000
- Trinidad mud volcanoes: where do the expelled fluids come from?Geochimica et Cosmochimica Acta, 1999
- Mariana blueschist mud volcanism: Implications for conditions within the subduction zoneGeology, 1999
- The temperature dependence of hydrogen isotope fractionation between clay minerals and water: Evidence from a geopressured systemGeochimica et Cosmochimica Acta, 1992
- Oxygen-18 enrichment in the water of a clathrate hydrateGeochimica et Cosmochimica Acta, 1983
- Alteration of volcanic matter in deep sea sediments: evidence from the chemical composition of interstitial waters from deep sea drilling coresGeochimica et Cosmochimica Acta, 1981
- Geothermal gas equilibriaGeochimica et Cosmochimica Acta, 1980