Magnetotelluric imaging of anisotropic crust near Fort McMurray, Alberta: implications for engineered geothermal system development
Viability for the development of an engineered geothermal system (EGS) in the oilsands region near Fort McMurray, Alberta, is investigated by studying the structure of the Precambrian basement rocks with magnetotellurics (MT). MT data were collected at 94 broad-band stations on two east-west profile...
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Online Access: | https://doi.org/10.1093/gji/ggw089 http://hdl.handle.net/11104/0262911 |
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ftczacademyscien:oai:asep.lib.cas.cz:CavUnEpca/0463813 2024-02-04T10:00:27+01:00 Magnetotelluric imaging of anisotropic crust near Fort McMurray, Alberta: implications for engineered geothermal system development Liddell, M. Unsworth, M. Pek, J. (Josef) 2016 https://doi.org/10.1093/gji/ggw089 http://hdl.handle.net/11104/0262911 eng eng doi:10.1093/gji/ggw089 urn:pissn: 0956-540x urn:eissn: 1365-246x http://hdl.handle.net/11104/0262911 info:eu-repo/semantics/openAccess electrical anisotropy composition of the continental crust magnetotellurics North America info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2016 ftczacademyscien https://doi.org/10.1093/gji/ggw089 2024-01-09T17:36:18Z Viability for the development of an engineered geothermal system (EGS) in the oilsands region near Fort McMurray, Alberta, is investigated by studying the structure of the Precambrian basement rocks with magnetotellurics (MT). MT data were collected at 94 broad-band stations on two east-west profiles. Apparent resistivity and phase data showed little variation along each profile. The short period MT data detected a 1-D resistivity structure that could be identified as the shallow sedimentary basin underlain by crystalline basement rocks to a depth of 4-5 km. At lower frequencies a strong directional dependence, large phase splits, and regions of out-of-quadrant (OOQ) phase were detected. 2-D isotropic inversions of these data failed to produce a realistic resistivity model. A detailed dimensionality analysis found links between large phase tensor skews (similar to 15A degrees), azimuths, OOQ phases and tensor decomposition strike angles at periods greater than 1 s. Low magnitude induction vectors, as well as uniformity of phase splits and phase tensor character between the northern and southern profiles imply that a 3-D analysis is not necessary or appropriate. Therefore, 2-D anisotropic forward modelling was used to generate a resistivity model to interpret the MT data. The preferred model was based on geological observations of outcropping anisotropic mylonitic basement rocks of the Charles Lake shear zone, 150 km to the north, linked to the study area by aeromagnetic and core sample data. This model fits all four impedance tensor elements with an rms misfit of 2.82 on the southern profile, and 3.3 on the northern Article in Journal/Newspaper Fort McMurray The Czech Academy of Sciences: Publication Activity (ASEP) Fort McMurray Geophysical Journal International 205 3 1365 1381 |
institution |
Open Polar |
collection |
The Czech Academy of Sciences: Publication Activity (ASEP) |
op_collection_id |
ftczacademyscien |
language |
English |
topic |
electrical anisotropy composition of the continental crust magnetotellurics North America |
spellingShingle |
electrical anisotropy composition of the continental crust magnetotellurics North America Liddell, M. Unsworth, M. Pek, J. (Josef) Magnetotelluric imaging of anisotropic crust near Fort McMurray, Alberta: implications for engineered geothermal system development |
topic_facet |
electrical anisotropy composition of the continental crust magnetotellurics North America |
description |
Viability for the development of an engineered geothermal system (EGS) in the oilsands region near Fort McMurray, Alberta, is investigated by studying the structure of the Precambrian basement rocks with magnetotellurics (MT). MT data were collected at 94 broad-band stations on two east-west profiles. Apparent resistivity and phase data showed little variation along each profile. The short period MT data detected a 1-D resistivity structure that could be identified as the shallow sedimentary basin underlain by crystalline basement rocks to a depth of 4-5 km. At lower frequencies a strong directional dependence, large phase splits, and regions of out-of-quadrant (OOQ) phase were detected. 2-D isotropic inversions of these data failed to produce a realistic resistivity model. A detailed dimensionality analysis found links between large phase tensor skews (similar to 15A degrees), azimuths, OOQ phases and tensor decomposition strike angles at periods greater than 1 s. Low magnitude induction vectors, as well as uniformity of phase splits and phase tensor character between the northern and southern profiles imply that a 3-D analysis is not necessary or appropriate. Therefore, 2-D anisotropic forward modelling was used to generate a resistivity model to interpret the MT data. The preferred model was based on geological observations of outcropping anisotropic mylonitic basement rocks of the Charles Lake shear zone, 150 km to the north, linked to the study area by aeromagnetic and core sample data. This model fits all four impedance tensor elements with an rms misfit of 2.82 on the southern profile, and 3.3 on the northern |
format |
Article in Journal/Newspaper |
author |
Liddell, M. Unsworth, M. Pek, J. (Josef) |
author_facet |
Liddell, M. Unsworth, M. Pek, J. (Josef) |
author_sort |
Liddell, M. |
title |
Magnetotelluric imaging of anisotropic crust near Fort McMurray, Alberta: implications for engineered geothermal system development |
title_short |
Magnetotelluric imaging of anisotropic crust near Fort McMurray, Alberta: implications for engineered geothermal system development |
title_full |
Magnetotelluric imaging of anisotropic crust near Fort McMurray, Alberta: implications for engineered geothermal system development |
title_fullStr |
Magnetotelluric imaging of anisotropic crust near Fort McMurray, Alberta: implications for engineered geothermal system development |
title_full_unstemmed |
Magnetotelluric imaging of anisotropic crust near Fort McMurray, Alberta: implications for engineered geothermal system development |
title_sort |
magnetotelluric imaging of anisotropic crust near fort mcmurray, alberta: implications for engineered geothermal system development |
publishDate |
2016 |
url |
https://doi.org/10.1093/gji/ggw089 http://hdl.handle.net/11104/0262911 |
geographic |
Fort McMurray |
geographic_facet |
Fort McMurray |
genre |
Fort McMurray |
genre_facet |
Fort McMurray |
op_relation |
doi:10.1093/gji/ggw089 urn:pissn: 0956-540x urn:eissn: 1365-246x http://hdl.handle.net/11104/0262911 |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1093/gji/ggw089 |
container_title |
Geophysical Journal International |
container_volume |
205 |
container_issue |
3 |
container_start_page |
1365 |
op_container_end_page |
1381 |
_version_ |
1789965748062388224 |