In situ electrical resistivity and bulk porosity of the oceanic crust costa rica rift


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ABSTRACT _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


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AFFILIATIONS * Deep Sea Drilling Project A-031, Scripps Institution of Oceanography, La Jolla, California, 92093, USA Keir Becker * Woods Hole Oceanographic Institution, Woods Hole,


Massachusetts, 02542, USA R. P. Von Herzen & M. J. Mottl * Institute of Oceanographic Sciences, Wormley, Godalming, Surrey, GU8 5UB, UK T. J. G. Francis * Lamont-Doherty Geological


Observatory, Palisades, New York, 10964, USA R. N. Anderson & R. L. Newmark * Division of Marine Geology and Geophysics, University of Miami, Miami, Florida, 33149, USA J. Honnorez &


 J. C. Alt * Department of Geology, The University, Newcastle upon Tyne, Newcastle, NE1 7RU, UK A. C. Adamson * Mineralogisch-Petrologisches Institut, University of Giessen, 63, Giessen, FRG


R. Emmermann * Department of Geological Sciences, Southern Methodist University, Dallas, Texas, 75275, USA P. D. Kempton * Faculty of Sciences, Chiba University, Yayoi-Cho, Chiba, Japan H.


Kinoshita * Laboratoire de Géologic, Université de l'Océan Indien, Réunion, France C. Laverne Authors * Keir Becker View author publications You can also search for this author inPubMed


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Von Herzen, R., Francis, T. _et al._ _In situ_ electrical resistivity and bulk porosity of the oceanic crust Costa Rica Rift. _Nature_ 300, 594–598 (1982). https://doi.org/10.1038/300594a0


Download citation * Received: 21 June 1982 * Accepted: 16 September 1982 * Issue Date: 16 December 1982 * DOI: https://doi.org/10.1038/300594a0 SHARE THIS ARTICLE Anyone you share the


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