The permeability of young oceanic crust east of Juan de Fuca Ridge Determined using borehole thermal measurements
Author:
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
http://www.agu.org/journals/gl/v024/i011/97GL01286/97GL01286.pdf
Reference20 articles.
1. Permeability, underpressures and convection in the oceanic crust near the Costa Rica Rift, eastern equatorial Pacific;Anderson;J. Geophys. Res.,1982
2. Becker , K. Permeability measurements in Hole 896A and implications for the lateral variability of upper crustal permeability at Sites 504 and 896 Proc. ODP., Sci. Res. J. C. Alt H. Kinoshita L. Stokking 353 363 Ocean Drilling Program College Station, TX 1996
3. Becker , K. M. G. Langseth R. D. Hyndman Temperature measurements in Hole 395A, Leg 78B Init. Rep. DSDP R. Hyndman M. Salisbury 689 698 U. S. Govt. Printing Office Washington, D. C. 1984
4. Becker , K. M. G. Langseth R. P. Von Herzen Deep crustal geothermal measurements, Hole 504B, Deep Sea Drilling Project Legs 69 and 70 Init. Rep. DSDP J. in Cann M. G. Langseth 223 236 U. S. Govt. Printing Office Washington, D. C. 1983
5. Davis , E. E. A. T. Fisher J. Firth Proceedings of the Ocean Drilling Program Init. Repts. 168 Ocean Drilling Program College Station, TX 1997
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