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- W304265382 abstract "Application of electromagnetic geothermometer has enabled the construction of the 3-D temperature model of the Hengill geothermal area (Iceland) up to the depth of 20 km. Its analysis showed that the background temperature of the Icelandic crust above 20 km does not exceed 400°C. It is overlapped by a network of interconnected high-temperature low resistive channels, which braid through the crust mainly at a level of 10–15 km and root to a depth below 20 km. Joint analysis of the temperature and resistivity models taking into account the Bouguer gravity anomalies enables to suggest a new self-consistent conceptual model of the Icelandic crust, which agrees with previous geophysical results and provides an explanation for the facts the previous models failed to explain." @default.
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- W304265382 date "2015-01-01" @default.
- W304265382 modified "2023-09-25" @default.
- W304265382 title "A New Conceptual Model of the Icelandic Crust: Hengill Case Study" @default.
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- W304265382 doi "https://doi.org/10.1016/b978-0-12-802210-8.00008-3" @default.
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