In situ electrical resistivity and bulk porosity of the oceanic crust Costa Rica Rift

Details In situ electrical resistivity and bulk porosity of the oceanic crust Costa Rica Rift In situ electrical resistivity and bulk porosity of the oceanic crust Costa Rica Rift

Dec 1982

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1982natur.300..594b&link_type=abstract

Nature, Volume 300, Issue 5893, pp. 594-598 (1982).

Physics

36

Scientific paper

In situ electrical resistivity was measured in DSDP Hole 504B to a depth of 1,013 m into oceanic basement. Apparent resistivities are about 10 Ω m in about 600 m of pillow lavas, sharply increasing to nearly 1,000 Ω m in the underlying dykes. Bulk porosities calculated from resistivities show a distinct layering, apparently corresponding to geophysical layers 2A, 2B and 2C.

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