AEM Greenland 1998 (1) - Airborne GEOTEM magnetic survey over Washington Land Daugaard Jensen Land in western North Greenland
The AEM Greenland 1998 (1) survey was conducted in Washington Land and Daugaard-Jensen Land in western North Greenland. Measurements included acquisition of controlled source electromagnetic data (GEOTEM -time domain EM ) and total field magnetic data. The survey (size of 3220 km2) was flown by Geot...
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GEUS Dataverse
2021
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Online Access: | https://dx.doi.org/10.22008/fk2/wp1tr3 https://dataverse01.geus.dk/citation?persistentId=doi:10.22008/FK2/WP1TR3 |
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DataCite Metadata Store (German National Library of Science and Technology) |
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The AEM Greenland 1998 (1) survey was conducted in Washington Land and Daugaard-Jensen Land in western North Greenland. Measurements included acquisition of controlled source electromagnetic data (GEOTEM -time domain EM ) and total field magnetic data. The survey (size of 3220 km2) was flown by Geoterrex-Dighem Ltd. and financed by the Government of Greenland. Two surveys were acquired. The main survey was flown with a flight line spacing of 400 metres between lines with a heading of NW23.5 deg and tie-lines at a direction of NE66.5 deg spaced 4 km apart. Within this area, a smaller survey in the eastern part directly over the mineralised sites was measured at 200 m line spacing (NE66.5 deg). During a GEUS geological reconnaissance campaign in eastern Washington Land in 1997, a Zn-Pb-Ag mineralisation was discovered in dolomitic boulders in the area. The discovery led to the selection of Washington Land and Daugaard-Jensen Land as one of the target areas in North Greenland for a combined airborne electromagnetic (GEOTEM) and magnetic survey. Lower Palaeozoic sedimentary deposits dominate the geology of Washington Land and Daugaard-Jensen Land. The sediments were deposited in the Franklinian Basin that has an extension of approximately 2000 km across North Greenland and Canada. Approximately 8 km of Lower Palaeozoic strata are exposed within the North Greenland part of the basin. In Washington Land and Daugaard-Jensen Land the depositional environment of the basin is reflected in shelf sediments located to the south and deep-water sequences further to the north. Exposed rocks in the survey area consist mainly of carbonates deposited on the former shelf with subordinate siliciclastic sediments and evaporites. The Zn-Pg-Ag mineralisation is found within the evaporite-rich part of the Lower Ordovician platform sediments. |
format |
Dataset |
author |
GEOTERREX-DIGHEM |
spellingShingle |
GEOTERREX-DIGHEM AEM Greenland 1998 (1) - Airborne GEOTEM magnetic survey over Washington Land Daugaard Jensen Land in western North Greenland |
author_facet |
GEOTERREX-DIGHEM |
author_sort |
GEOTERREX-DIGHEM |
title |
AEM Greenland 1998 (1) - Airborne GEOTEM magnetic survey over Washington Land Daugaard Jensen Land in western North Greenland |
title_short |
AEM Greenland 1998 (1) - Airborne GEOTEM magnetic survey over Washington Land Daugaard Jensen Land in western North Greenland |
title_full |
AEM Greenland 1998 (1) - Airborne GEOTEM magnetic survey over Washington Land Daugaard Jensen Land in western North Greenland |
title_fullStr |
AEM Greenland 1998 (1) - Airborne GEOTEM magnetic survey over Washington Land Daugaard Jensen Land in western North Greenland |
title_full_unstemmed |
AEM Greenland 1998 (1) - Airborne GEOTEM magnetic survey over Washington Land Daugaard Jensen Land in western North Greenland |
title_sort |
aem greenland 1998 (1) - airborne geotem magnetic survey over washington land daugaard jensen land in western north greenland |
publisher |
GEUS Dataverse |
publishDate |
2021 |
url |
https://dx.doi.org/10.22008/fk2/wp1tr3 https://dataverse01.geus.dk/citation?persistentId=doi:10.22008/FK2/WP1TR3 |
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ENVELOPE(-66.000,-66.000,80.250,80.250) |
geographic |
Canada Greenland Washington Land |
geographic_facet |
Canada Greenland Washington Land |
genre |
Greenland North Greenland Washington land |
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Greenland North Greenland Washington land |
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ftdatacite:10.22008/fk2/wp1tr3 2023-05-15T16:24:19+02:00 AEM Greenland 1998 (1) - Airborne GEOTEM magnetic survey over Washington Land Daugaard Jensen Land in western North Greenland GEOTERREX-DIGHEM 2021 https://dx.doi.org/10.22008/fk2/wp1tr3 https://dataverse01.geus.dk/citation?persistentId=doi:10.22008/FK2/WP1TR3 unknown GEUS Dataverse https://dx.doi.org/10.22008/fk2/wp1tr3/ybqoak https://dx.doi.org/10.22008/fk2/wp1tr3/excgqf https://dx.doi.org/10.22008/fk2/wp1tr3/xsfeq1 https://dx.doi.org/10.22008/fk2/wp1tr3/yjgssc https://dx.doi.org/10.22008/fk2/wp1tr3/xvyqae https://dx.doi.org/10.22008/fk2/wp1tr3/nfssub https://dx.doi.org/10.22008/fk2/wp1tr3/zmrbnc https://dx.doi.org/10.22008/fk2/wp1tr3/mniyld https://dx.doi.org/10.22008/fk2/wp1tr3/gzgqms https://dx.doi.org/10.22008/fk2/wp1tr3/zwg0hu https://dx.doi.org/10.22008/fk2/wp1tr3/vzkeev https://dx.doi.org/10.22008/fk2/wp1tr3/3k2qe6 https://dx.doi.org/10.22008/fk2/wp1tr3/cqocxo https://dx.doi.org/10.22008/fk2/wp1tr3/azqmli https://dx.doi.org/10.22008/fk2/wp1tr3/as0kmq https://dx.doi.org/10.22008/fk2/wp1tr3/segobp https://dx.doi.org/10.22008/fk2/wp1tr3/2es7uy https://dx.doi.org/10.22008/fk2/wp1tr3/nsvm1b https://dx.doi.org/10.22008/fk2/wp1tr3/eudqhm https://dx.doi.org/10.22008/fk2/wp1tr3/2nrx3d https://dx.doi.org/10.22008/fk2/wp1tr3/odj5gq https://dx.doi.org/10.22008/fk2/wp1tr3/gv5ykj https://dx.doi.org/10.22008/fk2/wp1tr3/ndais3 https://dx.doi.org/10.22008/fk2/wp1tr3/kz11tt https://dx.doi.org/10.22008/fk2/wp1tr3/tl6xbe https://dx.doi.org/10.22008/fk2/wp1tr3/bvlta6 https://dx.doi.org/10.22008/fk2/wp1tr3/pqwjrh https://dx.doi.org/10.22008/fk2/wp1tr3/wjnvjb https://dx.doi.org/10.22008/fk2/wp1tr3/bkmusw https://dx.doi.org/10.22008/fk2/wp1tr3/aj524w https://dx.doi.org/10.22008/fk2/wp1tr3/srk6ad https://dx.doi.org/10.22008/fk2/wp1tr3/kf17ya https://dx.doi.org/10.22008/fk2/wp1tr3/dodc3m https://dx.doi.org/10.22008/fk2/wp1tr3/2bx2vl https://dx.doi.org/10.22008/fk2/wp1tr3/7ugy6m https://dx.doi.org/10.22008/fk2/wp1tr3/40vsmk https://dx.doi.org/10.22008/fk2/wp1tr3/vfubd0 https://dx.doi.org/10.22008/fk2/wp1tr3/uf3lid https://dx.doi.org/10.22008/fk2/wp1tr3/1j43wu https://dx.doi.org/10.22008/fk2/wp1tr3/j4yqpx https://dx.doi.org/10.22008/fk2/wp1tr3/z8nle1 https://dx.doi.org/10.22008/fk2/wp1tr3/e5magb https://dx.doi.org/10.22008/fk2/wp1tr3/v6llet https://dx.doi.org/10.22008/fk2/wp1tr3/ot3ko9 https://dx.doi.org/10.22008/fk2/wp1tr3/3vn6rr https://dx.doi.org/10.22008/fk2/wp1tr3/xu8nyc https://dx.doi.org/10.22008/fk2/wp1tr3/vthgny https://dx.doi.org/10.22008/fk2/wp1tr3/hxy1fd https://dx.doi.org/10.22008/fk2/wp1tr3/idpkcs https://dx.doi.org/10.22008/fk2/wp1tr3/ohfgxz dataset Dataset 2021 ftdatacite https://doi.org/10.22008/fk2/wp1tr3 https://doi.org/10.22008/fk2/wp1tr3/ybqoak https://doi.org/10.22008/fk2/wp1tr3/excgqf https://doi.org/10.22008/fk2/wp1tr3/xsfeq1 https://doi.org/10.22008/fk2/wp1tr3/yjgssc https://doi.org/10.22008/fk2/wp1tr3/x 2021-11-05T12:55:41Z The AEM Greenland 1998 (1) survey was conducted in Washington Land and Daugaard-Jensen Land in western North Greenland. Measurements included acquisition of controlled source electromagnetic data (GEOTEM -time domain EM ) and total field magnetic data. The survey (size of 3220 km2) was flown by Geoterrex-Dighem Ltd. and financed by the Government of Greenland. Two surveys were acquired. The main survey was flown with a flight line spacing of 400 metres between lines with a heading of NW23.5 deg and tie-lines at a direction of NE66.5 deg spaced 4 km apart. Within this area, a smaller survey in the eastern part directly over the mineralised sites was measured at 200 m line spacing (NE66.5 deg). During a GEUS geological reconnaissance campaign in eastern Washington Land in 1997, a Zn-Pb-Ag mineralisation was discovered in dolomitic boulders in the area. The discovery led to the selection of Washington Land and Daugaard-Jensen Land as one of the target areas in North Greenland for a combined airborne electromagnetic (GEOTEM) and magnetic survey. Lower Palaeozoic sedimentary deposits dominate the geology of Washington Land and Daugaard-Jensen Land. The sediments were deposited in the Franklinian Basin that has an extension of approximately 2000 km across North Greenland and Canada. Approximately 8 km of Lower Palaeozoic strata are exposed within the North Greenland part of the basin. In Washington Land and Daugaard-Jensen Land the depositional environment of the basin is reflected in shelf sediments located to the south and deep-water sequences further to the north. Exposed rocks in the survey area consist mainly of carbonates deposited on the former shelf with subordinate siliciclastic sediments and evaporites. The Zn-Pg-Ag mineralisation is found within the evaporite-rich part of the Lower Ordovician platform sediments. Dataset Greenland North Greenland Washington land DataCite Metadata Store (German National Library of Science and Technology) Canada Greenland Washington Land ENVELOPE(-66.000,-66.000,80.250,80.250) |