Permeability versus depth in the upper oceanic crust: In situ measurements in DSDP hole 504B, eastern equatorial Pacific
- 10 April 1985
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 90 (B5) , 3659-3669
- https://doi.org/10.1029/jb090ib05p03659
Abstract
No abstract availableKeywords
This publication has 16 references indexed in Scilit:
- Deep crustal geothermal measurements, hole 504B, Costa Rica RiftJournal of Geophysical Research, 1983
- Numerical models for the hydrothermal field at the Galapagos Spreading CenterJournal of Geophysical Research, 1983
- In situ electrical resistivity and bulk porosity of the oceanic crust Costa Rica RiftNature, 1982
- DSDP Hole 504B, the first reference section over 1 km through Layer 2 of the oceanic crustNature, 1982
- Permeability, underpressures, and convection in the oceanic crust near the Costa Rica Rift, eastern equatorial PacificJournal of Geophysical Research, 1982
- A method for determining the hydraulic properties of tight formationsWater Resources Research, 1980
- Geothermal Convection Through Oceanic Crust and Sediments in the Indian OceanScience, 1979
- Convective heat transfer analysis by the finite element methodComputer Methods in Applied Mechanics and Engineering, 1977
- The mechanisms of heat transfer through the floor of the Indian OceanJournal of Geophysical Research, 1977
- Response of a finite‐diameter well to an instantaneous charge of waterWater Resources Research, 1967