Trinidad mud volcanoes: where do the expelled fluids come from?
Authors:
- A.N DiaADA.N Dia
- M Castrec-RouelleMCM Castrec-Rouelle
- J BoulègueJBJ Boulègue
- P ComeauPCP Comeau
- 1 April 1999
- journal article
- Published by Elsevier in Geochimica et Cosmochimica Acta
- Vol. 63 (7-8) , 1023-1038
Abstract
No abstract availableKeywords
This publication has 22 references indexed in Scilit:
- Hydrotectonic Models of Burial Diagenesis in Platform Carbonates Based on Formation Water Geochemistry in North American Sedimentary Basins1997
- Major- and trace-element and Sr isotope constraints on fluid circulation in the Barbados accretionary complex. Part II: circulation rates and fluxesEarth and Planetary Science Letters, 1996
- Major and trace element and Sr isotope constraints on fluid circulations in the Barbados accretionary complex. Part 1: Fluid originEarth and Planetary Science Letters, 1995
- Geochemical modelling of late diagenetic processes in the Brent Sandstone, Alwyn South area (East Shetland Basin, North Sea)Chemical Geology, 1993
- Structure and deformation history of the northern range of Trinidad and adjacent areasTectonics, 1993
- Hyperfiltration-osmosis effects in compacting sediments: Isotopic and chemical changes in pore watersChemical Geology, 1990
- Long decollements and mud volcanoes: Evidence from the Barbados Ridge Complex for the role of high pore-fluid pressure in the development of an accretionary complexGeology, 1983
- Reduction of water with zinc for hydrogen isotope analysisAnalytical Chemistry, 1982
- Ratios and late-stage dehydration of shales during burialGeochimica et Cosmochimica Acta, 1980
- VIOLENT MUD-VOLCANO ERUPTION OF LAKE CITY HOT SPRINGS, NORTHEASTERN CALIFORNIAGeological Society of America Bulletin, 1955