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      Data report: electrical properties of gabbroic and troctolitic rocks from IODP Hole U1309D, Atlantis Massif: Expedition 304/305

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      Proceedings of the IODP

      Integrated Ocean Drilling Program

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          Abstract

          In this report we present the results of laboratory measurements carried out to explore the electrical properties of gabbroic and troctolitic samples from Integrated Ocean Drilling Program (IODP) Hole U1309D in the Atlantis Massif, an oceanic core complex located at 30°N on the Mid-Atlantic Ridge. Oceanic core complexes are presumably localized in portions of heterogeneous oceanic crust that are relatively rich in igneous rocks and are the locus of significant hydrothermal activity. Electrical properties of igneous rocks are used to discuss the rocks’ porosity structure as a function of mineralogy, alteration processes, and deformation. Electrical properties of the gabbroic suites sampled during IODP Expedition 304/305 can contribute to the understanding of these processes in the Atlantis Massif. We present the full suite of electrical data together with density and porosity measurements on the same suite of samples.

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          Most cited references 20

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          A long in situ section of the lower ocean crust: results of ODP Leg 176 drilling at the Southwest Indian Ridge

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            Electrical Conductivities in Oil-Bearing Shaly Sands

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              Oceanic core complexes and crustal accretion at slow-spreading ridges

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                Author and article information

                Journal
                10.2204/iodp.proc.304305.2006
                Proceedings of the IODP
                Integrated Ocean Drilling Program
                1930-1014
                08 September 2009
                10.2204/iodp.proc.304305.204.2009

                This work is licensed under a Creative Commons Attribution 4.0 Unported License. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/

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                Self URI (journal page): http://publications.iodp.org/

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