Convection in the oceanic crust: Simulation of observations from deep sea drilling project hole 504B, Costa Rica Rift
Abstract
Three-dimensional modeling of convection in the oceanic crust at Deep Sea Drilling Project site 504B using an integral finite difference model reasonably duplicates underpressures, surface heat flow, downhole temperature profiles, and fluid drawdown rates observed by in situ measurements in the borehole. The major constraint to produce such good fits is the permeability versus depth functions, a quantity which was actually measured in the borehole.
- Authors:
- Publication Date:
- Research Org.:
- Earth Sciences Division, Lawrence Berkeley Laboratory, Berkeley, California
- OSTI Identifier:
- 5718286
- Resource Type:
- Journal Article
- Journal Name:
- J. Geophys. Res.; (United States)
- Additional Journal Information:
- Journal Volume: 91:B5
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 58 GEOSCIENCES; OCEANIC CRUST; CONVECTION; PACIFIC OCEAN; BOREHOLES; GEOTHERMAL GRADIENTS; HEAT FLUX; NUMERICAL SOLUTION; PERMEABILITY; SENSITIVITY ANALYSIS; THERMAL CONDUCTIVITY; THREE-DIMENSIONAL CALCULATIONS; CAVITIES; EARTH CRUST; ENERGY TRANSFER; HEAT TRANSFER; MASS TRANSFER; PHYSICAL PROPERTIES; SEAS; SURFACE WATERS; TEMPERATURE GRADIENTS; THERMODYNAMIC PROPERTIES; 580200* - Geophysics- (-1989)
Citation Formats
Williams, C F, Narasimhan, T N, Anderson, R N, Zoback, M D, and Becker, K. Convection in the oceanic crust: Simulation of observations from deep sea drilling project hole 504B, Costa Rica Rift. United States: N. p., 1986.
Web. doi:10.1029/JB091iB05p04877.
Williams, C F, Narasimhan, T N, Anderson, R N, Zoback, M D, & Becker, K. Convection in the oceanic crust: Simulation of observations from deep sea drilling project hole 504B, Costa Rica Rift. United States. https://doi.org/10.1029/JB091iB05p04877
Williams, C F, Narasimhan, T N, Anderson, R N, Zoback, M D, and Becker, K. 1986.
"Convection in the oceanic crust: Simulation of observations from deep sea drilling project hole 504B, Costa Rica Rift". United States. https://doi.org/10.1029/JB091iB05p04877.
@article{osti_5718286,
title = {Convection in the oceanic crust: Simulation of observations from deep sea drilling project hole 504B, Costa Rica Rift},
author = {Williams, C F and Narasimhan, T N and Anderson, R N and Zoback, M D and Becker, K},
abstractNote = {Three-dimensional modeling of convection in the oceanic crust at Deep Sea Drilling Project site 504B using an integral finite difference model reasonably duplicates underpressures, surface heat flow, downhole temperature profiles, and fluid drawdown rates observed by in situ measurements in the borehole. The major constraint to produce such good fits is the permeability versus depth functions, a quantity which was actually measured in the borehole.},
doi = {10.1029/JB091iB05p04877},
url = {https://www.osti.gov/biblio/5718286},
journal = {J. Geophys. Res.; (United States)},
number = ,
volume = 91:B5,
place = {United States},
year = {Thu Apr 10 00:00:00 EST 1986},
month = {Thu Apr 10 00:00:00 EST 1986}
}
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