Geochemical and geothermal evidence for fluid migration in the Barbados Accretionary Prism (ODP leg 110)
- 1 May 1991
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 18 (5), 947-950
- https://doi.org/10.1029/91gl00913
Abstract
No abstract availableThis publication has 14 references indexed in Scilit:
- Heat flow, tectonics, and fluid circulation at the toe of the Barbados Ridge Accretionary PrismJournal of Geophysical Research, 1990
- Transient fluid flow through the toe of the Barbados Accretionary Complex: Constraints from ocean Drilling Program Leg 110 heat row studies and simple modelsJournal of Geophysical Research, 1990
- Contrasting geothermal regimes of the Barbados Ridge Accretionary ComplexJournal of Geophysical Research, 1990
- Hydrogeochemistry of the Northern Barbados Accretionary Complex Transect: Ocean Drilling Project Leg 110Journal of Geophysical Research, 1990
- Interstitial Water Chemistry—Major ConstituentsPublished by International Ocean Discovery Program (IODP) ,1990
- Expulsion of fluids from depth along a subduction-zone decollement horizonNature, 1987
- Constraints on water transport and alteration in the oceanic crust from the isotopic composition of pore waterJournal of Geophysical Research, 1981
- Clay Diagenesis in Wilcox Sandstones of Southwest Texas: Implications of Smectite Diagenesis on Sandstone CementationJournal of Sedimentary Research, 1979
- An analysis of the variation of ocean floor bathymetry and heat flow with ageJournal of Geophysical Research, 1977
- Diagenesis of Gulf Coast Clayey Sediments and Its Possible Relation to Petroleum MigrationAAPG Bulletin, 1969