Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
1742442 | Geothermics | 2014 | 11 Pages |
Abstract
The stratigraphy, alteration mineralogy and temperature conditions in well IDDP-1 were established through drill cutting analyses and geophysical logs. The stratigraphy comprises basaltic lava and hyaloclastite sequences extending to 1362 m succeeded by an intrusive complex. Intrusions comprise basaltic dykes, dolerites and below 2020 m, granophyre and felsites. Rhyolitic magma was intersected below 2100 m. Alteration reflects cooling in the upper â¼1500 m of the reservoir. Below 1600 m temperature follows the boiling-point-depth curve. Alteration minerals are scarce in vicinity to the feed zone at 2035-2080 m correlating with a superheated steam zone above the magma, but estimated bottom-hole temperature is â¼500 °C.
Keywords
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Geochemistry and Petrology
Authors
A.K. Mortensen, Ã. Egilson, B. Gautason, S. Árnadóttir, Á. Guðmundsson,