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Einaudi, F. et al. (2005): Electrical properties of slow-spreading ridge gabbros from ODP Hole 1105A, SW Indian Ridge
Leg/Site/Hole:
Related Expeditions:
ODP 179
ODP 179 1105
ODP 118 735
ODP 176 735
Identifier:
ID:
2006-008642
Type:
georefid
Creator:
Name:
Einaudi, F.
Affiliation:
Universitede Montpellier II, Laboratoire de Geophysique et d'Hydrodynamique en Forage, Montpellier, France
Role:
author
Name:
Pezard, Phillipe A.
Affiliation:
Universite de Montpellier II, France
Role:
author
Name:
Ildefonse, B.
Affiliation:
Russian Academy of Sciences, Russian Federation
Role:
author
Name:
Glover, P.
Affiliation:
Universite d'Aix Marseille III, France
Role:
author
Identification:
Title:
Electrical properties of slow-spreading ridge gabbros from ODP Hole 1105A, SW Indian Ridge
Year:
2005
Source:
In: Harvey, Peter K. (editor), Brewer, Tim S. (editor), Pezard, Phillipe A. (editor), Petrov, Vladislav A. (editor), Petrophysical properties of crystalline rocks
Publisher:
Geological Society of London, London, United Kingdom
Volume:
240
Issue:
Pages:
179-193
Abstract:
Physical properties of gabbroic samples from Ocean Drilling Program Hole 1105A were measured in the laboratory, with a particular emphasis on the analysis of electrical properties. This data-set includes the major lithologies sampled in ODP Hole 1105A: gabbros, olivine gabbros, oxide-rich gabbros, and, for all rock types, different ranges of alteration were sampled: from fresh to highly altered. All these lithologies correspond to the seismic Layer 3 layer of the oceanic crust, and large-scale geophysical data interpretation requires a complete understanding of the physical properties of rocks in this section. Electrical conductivities measured on brine-saturated gabbros reveal strong excess conductivity for samples rich in oxide minerals and, to a lesser extent, for altered samples. However, the classical models do not explain the excess conductivity reported in the oxide-rich samples when saturated with brine. The electrical conduction via electronic processes in metallic minerals has been taken into account in our analysis of the electrical properties. The oxide minerals' contribution has been independently estimated through measuring dry electrical resistivity. These measurements allowed quantification of the electronic conduction, which can reach 80% of the full conductivity for the most oxide-rich gabbros.
Language:
English
Genre:
Serial
Rights:
URL:
Coverage:
Geographic coordinates:
North:-32.4308
West:57.1557
East: 57.1639
South:-32.4327
Keywords:
Engineering geology; Applied geophysics; Atlantis II fracture zone; basement; body waves; conductivity; crust; downhole methods; elastic waves; electrical logging; electrical properties; fluid dynamics; Formation MicroScanner; gabbros; igneous rocks; in situ; Indian Ocean; Leg 179; magnetic properties; magnetic susceptibility; mid-ocean ridges; mineral composition; Ocean Drilling Program; ocean floors; oceanic crust; ODP Site 1105; ODP Site 735; oxides; P-waves; paleomagnetism; physical properties; plate tectonics; plutonic rocks; porosity; reservoir properties; resistivity; saturation; sea-floor spreading; seismic stratigraphy; seismic waves; Southwest Indian Ridge; spreading centers; velocity; well-logging;
.
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