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- W2094609570 abstract "The results from magnetotelluric sounding experiments at three sites in Iceland are discussed. Two sites were in the neovolcanic zone (Askja, Burfellshraun); the third was in an adjacent area of older volcanics (Sulendur). Apparent resistivities were estimated using a series of digital band-pass filters having a selectivity of 0.3 and center periods of 50, 100, 200, 400, 800 and 1600 seconds. This method of analysis allowed the stability with time of the apparent resistivity to be considered. The sounding data show very little difference between the three stations over this range of periods, thus suggesting similar electrical structures under all the stations. The results indicate an almost constant value of about 30 ohm-meters for the apparent resistivity over the entire range of periods. On the assumption of a two-layer model, the depth to the conductive, 30 ohm-meter layer must be less than 25 km. The resistivity is a factor of two or three too high for molten lava, but may indicate a temperature enhancement in basalt or gabbro of 300 to 400°K." @default.
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- W2094609570 date "1968-08-01" @default.
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- W2094609570 title "Magnetotelluric deep-sounding experiments in Iceland" @default.
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- W2094609570 doi "https://doi.org/10.1016/0012-821x(68)90026-5" @default.
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