Effect of postglacial warming seen in high precision temperature log deep into the granites in NE Alberta
Recently reported new terrestrial heat flow density (referred further to as "heat flow") determination from a 2.36-km-deep well of opportunity (AOC Granite-Hunt well) drilled deep into some 2- to 2.4-Gyr-year old Precambrian basement rocks just west of Fort McMurray, Alberta, shows increas...
Published in: | International Journal of Earth Sciences |
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Online Access: | https://doi.org/10.1007/s00531-014-1075-9 http://hdl.handle.net/11104/0237405 |
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ftczacademyscien:oai:asep.lib.cas.cz:CavUnEpca/0433131 2024-02-04T10:00:27+01:00 Effect of postglacial warming seen in high precision temperature log deep into the granites in NE Alberta Majorowicz, J. Šafanda, J. (Jan) 2015 https://doi.org/10.1007/s00531-014-1075-9 http://hdl.handle.net/11104/0237405 eng eng doi:10.1007/s00531-014-1075-9 urn:pissn: 1437-3254 urn:eissn: 1437-3262 http://hdl.handle.net/11104/0237405 info:eu-repo/semantics/openAccess surface processes borehole temperatures climatic warming Ice Age heat flow info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2015 ftczacademyscien https://doi.org/10.1007/s00531-014-1075-9 2024-01-09T17:29:00Z Recently reported new terrestrial heat flow density (referred further to as "heat flow") determination from a 2.36-km-deep well of opportunity (AOC Granite-Hunt well) drilled deep into some 2- to 2.4-Gyr-year old Precambrian basement rocks just west of Fort McMurray, Alberta, shows increase of heat flow with depth. Cores were collected from granites, which are below 0.55 km and to the well bottom of 2.36 km. This borehole was logged in June 2011, and several years after, it was drilled in 1994 and deepened in 2003. Therefore, it is assumed to be in thermal equilibrium. Temperature versus depth shows a significant increase in the thermal gradient with increasing depth in the basement rocks. Article in Journal/Newspaper Fort McMurray The Czech Academy of Sciences: Publication Activity (ASEP) Fort McMurray International Journal of Earth Sciences 104 6 1563 1571 |
institution |
Open Polar |
collection |
The Czech Academy of Sciences: Publication Activity (ASEP) |
op_collection_id |
ftczacademyscien |
language |
English |
topic |
surface processes borehole temperatures climatic warming Ice Age heat flow |
spellingShingle |
surface processes borehole temperatures climatic warming Ice Age heat flow Majorowicz, J. Šafanda, J. (Jan) Effect of postglacial warming seen in high precision temperature log deep into the granites in NE Alberta |
topic_facet |
surface processes borehole temperatures climatic warming Ice Age heat flow |
description |
Recently reported new terrestrial heat flow density (referred further to as "heat flow") determination from a 2.36-km-deep well of opportunity (AOC Granite-Hunt well) drilled deep into some 2- to 2.4-Gyr-year old Precambrian basement rocks just west of Fort McMurray, Alberta, shows increase of heat flow with depth. Cores were collected from granites, which are below 0.55 km and to the well bottom of 2.36 km. This borehole was logged in June 2011, and several years after, it was drilled in 1994 and deepened in 2003. Therefore, it is assumed to be in thermal equilibrium. Temperature versus depth shows a significant increase in the thermal gradient with increasing depth in the basement rocks. |
format |
Article in Journal/Newspaper |
author |
Majorowicz, J. Šafanda, J. (Jan) |
author_facet |
Majorowicz, J. Šafanda, J. (Jan) |
author_sort |
Majorowicz, J. |
title |
Effect of postglacial warming seen in high precision temperature log deep into the granites in NE Alberta |
title_short |
Effect of postglacial warming seen in high precision temperature log deep into the granites in NE Alberta |
title_full |
Effect of postglacial warming seen in high precision temperature log deep into the granites in NE Alberta |
title_fullStr |
Effect of postglacial warming seen in high precision temperature log deep into the granites in NE Alberta |
title_full_unstemmed |
Effect of postglacial warming seen in high precision temperature log deep into the granites in NE Alberta |
title_sort |
effect of postglacial warming seen in high precision temperature log deep into the granites in ne alberta |
publishDate |
2015 |
url |
https://doi.org/10.1007/s00531-014-1075-9 http://hdl.handle.net/11104/0237405 |
geographic |
Fort McMurray |
geographic_facet |
Fort McMurray |
genre |
Fort McMurray |
genre_facet |
Fort McMurray |
op_relation |
doi:10.1007/s00531-014-1075-9 urn:pissn: 1437-3254 urn:eissn: 1437-3262 http://hdl.handle.net/11104/0237405 |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1007/s00531-014-1075-9 |
container_title |
International Journal of Earth Sciences |
container_volume |
104 |
container_issue |
6 |
container_start_page |
1563 |
op_container_end_page |
1571 |
_version_ |
1789965748250083328 |