AEM Greenland 1994 - Airborne GEOTEM electromagnetic survey over Inglefield Land, Greenland ...
The area for the AEM Greenland 1994 project is located in Inglefield Land, North-West Greenland. The measurements included acquisition of controlled source electromagnetic data (GEOTEM - time domain EM) and total field magnetic data. The survey across the ice-free onshore area (size of 6493 km2) is...
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2021
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Online Access: | https://dx.doi.org/10.22008/fk2/0lhvq6 https://dataverse.geus.dk/citation?persistentId=doi:10.22008/FK2/0LHVQ6 |
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ftdatacite:10.22008/fk2/0lhvq6 2023-06-11T04:12:01+02:00 AEM Greenland 1994 - Airborne GEOTEM electromagnetic survey over Inglefield Land, Greenland ... GEOTERREX 2021 https://dx.doi.org/10.22008/fk2/0lhvq6 https://dataverse.geus.dk/citation?persistentId=doi:10.22008/FK2/0LHVQ6 unknown GEUS Dataverse https://dx.doi.org/10.22008/fk2/0lhvq6/x54qku https://dx.doi.org/10.22008/fk2/0lhvq6/i92qdb https://dx.doi.org/10.22008/fk2/0lhvq6/mozyhr https://dx.doi.org/10.22008/fk2/0lhvq6/wndc4k https://dx.doi.org/10.22008/fk2/0lhvq6/ozzdzk https://dx.doi.org/10.22008/fk2/0lhvq6/xinvsh https://dx.doi.org/10.22008/fk2/0lhvq6/xmqeho https://dx.doi.org/10.22008/fk2/0lhvq6/xeznwc https://dx.doi.org/10.22008/fk2/0lhvq6/5tsgkr https://dx.doi.org/10.22008/fk2/0lhvq6/mdk57z https://dx.doi.org/10.22008/fk2/0lhvq6/x6xeb7 https://dx.doi.org/10.22008/fk2/0lhvq6/pjmqwy https://dx.doi.org/10.22008/fk2/0lhvq6/wd6baz https://dx.doi.org/10.22008/fk2/0lhvq6/90vrgf https://dx.doi.org/10.22008/fk2/0lhvq6/kolxj1 https://dx.doi.org/10.22008/fk2/0lhvq6/luwqqq https://dx.doi.org/10.22008/fk2/0lhvq6/g61054 https://dx.doi.org/10.22008/fk2/0lhvq6/ijyneq https://dx.doi.org/10.22008/fk2/0lhvq6/aheu9q https://dx.doi.org/10.22008/fk2/0lhvq6/in7q4g Dataset dataset 2021 ftdatacite https://doi.org/10.22008/fk2/0lhvq610.22008/fk2/0lhvq6/x54qku10.22008/fk2/0lhvq6/i92qdb10.22008/fk2/0lhvq6/mozyhr10.22008/fk2/0lhvq6/wndc4k10.22008/fk2/0lhvq6/ozzdzk10.22008/fk2/0lhvq6/xinvsh10.22008/fk2/0lhvq6/xmqeho10.22008/fk2/0lhvq6/xeznwc10.22008/fk2 2023-06-01T11:22:48Z The area for the AEM Greenland 1994 project is located in Inglefield Land, North-West Greenland. The measurements included acquisition of controlled source electromagnetic data (GEOTEM - time domain EM) and total field magnetic data. The survey across the ice-free onshore area (size of 6493 km2) is collected by Geoterrex Ltd. and financed by the Government of Greenland. The main flight lines are oriented north-south and spaced at 400 metres intervals with a set of orthogonal tie-lines at 4000 metre intervals. The area is underlain by an Early Proterozoic (and possibly Archaean) crystalline basement which traditionally has been subdivided into three main units: - Etah group of metasedimentary supracrustal rocks - Etah meta-igneous complex - Variable gneisses The basement is overlain by a succession of younger platform strata (Proterozoic to Cambrian age) in a number of coastal regions ... Dataset Greenland Inglefield land DataCite Metadata Store (German National Library of Science and Technology) Etah ENVELOPE(-72.585,-72.585,78.314,78.314) Greenland Inglefield Land ENVELOPE(-69.987,-69.987,78.637,78.637) |
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DataCite Metadata Store (German National Library of Science and Technology) |
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ftdatacite |
language |
unknown |
description |
The area for the AEM Greenland 1994 project is located in Inglefield Land, North-West Greenland. The measurements included acquisition of controlled source electromagnetic data (GEOTEM - time domain EM) and total field magnetic data. The survey across the ice-free onshore area (size of 6493 km2) is collected by Geoterrex Ltd. and financed by the Government of Greenland. The main flight lines are oriented north-south and spaced at 400 metres intervals with a set of orthogonal tie-lines at 4000 metre intervals. The area is underlain by an Early Proterozoic (and possibly Archaean) crystalline basement which traditionally has been subdivided into three main units: - Etah group of metasedimentary supracrustal rocks - Etah meta-igneous complex - Variable gneisses The basement is overlain by a succession of younger platform strata (Proterozoic to Cambrian age) in a number of coastal regions ... |
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Dataset |
author |
GEOTERREX |
spellingShingle |
GEOTERREX AEM Greenland 1994 - Airborne GEOTEM electromagnetic survey over Inglefield Land, Greenland ... |
author_facet |
GEOTERREX |
author_sort |
GEOTERREX |
title |
AEM Greenland 1994 - Airborne GEOTEM electromagnetic survey over Inglefield Land, Greenland ... |
title_short |
AEM Greenland 1994 - Airborne GEOTEM electromagnetic survey over Inglefield Land, Greenland ... |
title_full |
AEM Greenland 1994 - Airborne GEOTEM electromagnetic survey over Inglefield Land, Greenland ... |
title_fullStr |
AEM Greenland 1994 - Airborne GEOTEM electromagnetic survey over Inglefield Land, Greenland ... |
title_full_unstemmed |
AEM Greenland 1994 - Airborne GEOTEM electromagnetic survey over Inglefield Land, Greenland ... |
title_sort |
aem greenland 1994 - airborne geotem electromagnetic survey over inglefield land, greenland ... |
publisher |
GEUS Dataverse |
publishDate |
2021 |
url |
https://dx.doi.org/10.22008/fk2/0lhvq6 https://dataverse.geus.dk/citation?persistentId=doi:10.22008/FK2/0LHVQ6 |
long_lat |
ENVELOPE(-72.585,-72.585,78.314,78.314) ENVELOPE(-69.987,-69.987,78.637,78.637) |
geographic |
Etah Greenland Inglefield Land |
geographic_facet |
Etah Greenland Inglefield Land |
genre |
Greenland Inglefield land |
genre_facet |
Greenland Inglefield land |
op_relation |
https://dx.doi.org/10.22008/fk2/0lhvq6/x54qku https://dx.doi.org/10.22008/fk2/0lhvq6/i92qdb https://dx.doi.org/10.22008/fk2/0lhvq6/mozyhr https://dx.doi.org/10.22008/fk2/0lhvq6/wndc4k https://dx.doi.org/10.22008/fk2/0lhvq6/ozzdzk https://dx.doi.org/10.22008/fk2/0lhvq6/xinvsh https://dx.doi.org/10.22008/fk2/0lhvq6/xmqeho https://dx.doi.org/10.22008/fk2/0lhvq6/xeznwc https://dx.doi.org/10.22008/fk2/0lhvq6/5tsgkr https://dx.doi.org/10.22008/fk2/0lhvq6/mdk57z https://dx.doi.org/10.22008/fk2/0lhvq6/x6xeb7 https://dx.doi.org/10.22008/fk2/0lhvq6/pjmqwy https://dx.doi.org/10.22008/fk2/0lhvq6/wd6baz https://dx.doi.org/10.22008/fk2/0lhvq6/90vrgf https://dx.doi.org/10.22008/fk2/0lhvq6/kolxj1 https://dx.doi.org/10.22008/fk2/0lhvq6/luwqqq https://dx.doi.org/10.22008/fk2/0lhvq6/g61054 https://dx.doi.org/10.22008/fk2/0lhvq6/ijyneq https://dx.doi.org/10.22008/fk2/0lhvq6/aheu9q https://dx.doi.org/10.22008/fk2/0lhvq6/in7q4g |
op_doi |
https://doi.org/10.22008/fk2/0lhvq610.22008/fk2/0lhvq6/x54qku10.22008/fk2/0lhvq6/i92qdb10.22008/fk2/0lhvq6/mozyhr10.22008/fk2/0lhvq6/wndc4k10.22008/fk2/0lhvq6/ozzdzk10.22008/fk2/0lhvq6/xinvsh10.22008/fk2/0lhvq6/xmqeho10.22008/fk2/0lhvq6/xeznwc10.22008/fk2 |
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1768387568117743616 |