The role of smectites in the electrical conductivity of active hydrothermal systems: electrical properties of core samples from Krafla volcano, Iceland

Author:

Lévy L123,Gibert B4,Sigmundsson F2,Flóvenz ÓG3,Hersir GP3,Briole P1,Pezard PA4

Affiliation:

1. Laboratoire de Géologie, Ecole Normale Supérieure - PSL Research University, CNRS, UMR 8538, Paris, France

2. Nordic Volcanological Center, Institute of Earth Sciences, University of Iceland, 101 Reykjavík, Iceland

3. ÍSOR-Iceland GeoSurvey, Grensásvegur 9, 108 Reykjavík, Iceland

4. Géosciences Montpellier, Université de Montpellier, Montpellier, France

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

Reference63 articles.

1. Hydrothermal alteration of a 1 km section through the upper oceanic crust, Deep Sea Drilling Project Hole 504B: mineralogy, chemistry and evolution of seawater‐basalt interactions;Alt;J. geophys. Res.,1986

2. Cation exchange properties of wairakite and analcime;Ames;Am. Mineral.,1966

3. The electrical resistivity log as an aid in determining some reservoir characteristics;Archie;Trans. AIME,1942

4. Joint 1D inversion of TEM and MT data and 3D inversion of MT data in the Hengill area, SW Iceland;Árnason;Geothermics,2010

5. The resistivity structure of high-temperature geothermal systems in Iceland;Árnason,2000

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