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Joint 1D inversion of MT and TEM resistivity data from the Theistareykir high-temperature geothermal area, NE-Iceland and comparison with alteration and temperature logs from boreholes

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Titill: Joint 1D inversion of MT and TEM resistivity data from the Theistareykir high-temperature geothermal area, NE-Iceland and comparison with alteration and temperature logs from boreholesJoint 1D inversion of MT and TEM resistivity data from the Theistareykir high-temperature geothermal area, NE-Iceland and comparison with alteration and temperature logs from boreholes
Höfundur: Suriyaarachchi, Nuwan Buddika ; Jarðhitaskóli Háskóla Sameinuðu þjóðanna
URI: http://hdl.handle.net/10802/8625
Útgefandi: United Nations University; Orkustofnun
Útgáfa: 2012
Ritröð: United Nations University., UNU Geothermal Training Programme, Iceland. Report ; 2012 : 32
Efnisorð: Jarðhiti; Borholur; Þeistareykir
ISSN: 1670-7427
Tungumál: Enska
Tengd vefsíðuslóð: http://www.os.is/gogn/unu-gtp-report/UNU-GTP-2012-32-1.pdf
http://www.os.is/gogn/unu-gtp-report/UNU-GTP-2012-32-2.pdf
Tegund: Bók
Gegnir ID: 991003331729706886
Athugasemdir: Í: Geothermal training in Iceland 2012, s. 793-822Two parts, report and appendicesSjá viðauka eingöngu rafrænt / appendices to the report only on pdf.Myndefni: myndir, gröf, töflur
Útdráttur: Due to future demands for energy, it is essential to identify and develop new geothermal fields. As a result of this situation, many exploration projects have been carried out. Magnetotelluric (MT) and Transient electromagnetic (TEM) soundings in Theistareykir area were carried out by Iceland Geo-Survey (ISOR). In this study 15 MT and 15 TEM soundings from Theistareykir were used to study the resistivity subsurface structure. Both 1D TEM inversion and MT-TEM joint 1D inversion were performed for each and every sounding site. Two resistivity profiles and a number of iso-resistivity maps were compiled. With the aid of Zstrike, T-strike analysis and alteration mineralogical data from neighbouring boreholes, the resistivity structure and possible heat sources were interpreted.


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UNU-GTP-2012-32-1.pdf 6.194Mb PDF Skoða/Opna Heildartexti - Report
UNU-GTP-2012-32-2.pdf 2.217Mb PDF Skoða/Opna Heildartexti - Appendices

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