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Joint 1-D inversion of TEM and MT resistivity data, comparison with mineral alteration and temperature in drillholes - case study : Krýsuvík area, SW-Iceland

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Titill: Joint 1-D inversion of TEM and MT resistivity data, comparison with mineral alteration and temperature in drillholes - case study : Krýsuvík area, SW-IcelandJoint 1-D inversion of TEM and MT resistivity data, comparison with mineral alteration and temperature in drillholes - case study : Krýsuvík area, SW-Iceland
Höfundur: Irabaruta, Constantin ; Jarðhitaskóli Háskóla Sameinuðu þjóðanna
URI: http://hdl.handle.net/10802/8243
Útgefandi: United Nations University; Orkustofnun
Útgáfa: 2011
Ritröð: United Nations University., UNU Geothermal Training Programme, Iceland. Report ; 2010 : 15
Efnisorð: Jarðhiti; Jarðeðlisfræði; Borholur; Krýsuvík
ISSN: 1670-7427
Tungumál: Enska
Tengd vefsíðuslóð: http://www.os.is/gogn/unu-gtp-report/UNU-GTP-2010-15.pdf
Tegund: Bók
Gegnir ID: 991010764129706886
Athugasemdir: Í: Geothermal training in Iceland 2010, s. 235-264Myndefni: myndir, kort, gröf
Útdráttur: In this work, the electrical resistivity of the subsurface is studied. Geophysical exploration methods to be used are discussed in some details. The joint 1-D inversion of TEM and MT data is performed. The static shift problem of MT data is solved by inverting jointly both TEM and MT data. The resistivity of the subsurface correlates with the alteration mineralogy studied in drillholes. The NW-SE profile of the Krýsuvík area appears to host a viable geothermal system. However, a discrepancy is raised between the formation and the alteration temperatures, which would mean a cooling geothermal system underneath the studied profile.


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