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Multidimensional Inversion of MT data from Krýsuvík High Temperature Geothermal Field, SW Iceland

Y. L. Didana, G. P. Hersir & K. Árnason

Conference
Der Geothermiekongress
Year
2011
Language
English

Full text

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Abstract

Electromagnetic (EM) methods are frequently used in the exploration of geothermal resourcefor determining the spatial distribution of electrical conductivity. Of the various EM methods, magnetotelluric (MT) method was found to be the most effective in defining a conductive reservoir at a depth exceeding 1 km overlain by a larger and more conductive clay cap.

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