AEROMAG 1997 - Aeromagnetic survey - Disko Bay, Greenland
The Aeromag 1997 project was conducted over the Disko-Nuussuaq region of central West Greenland (size: 46 390 km²). The survey area was located both onshore and offshore. The data were collected and processed by Sanders Geophysics Ltd. and financed by the Greenlandic government. The regular line dir...
Main Authors: | , |
---|---|
Format: | Dataset |
Language: | unknown |
Published: |
GEUS Dataverse
2021
|
Subjects: | |
Online Access: | https://dx.doi.org/10.22008/fk2/oepn9z https://dataverse01.geus.dk/citation?persistentId=doi:10.22008/FK2/OEPN9Z |
id |
ftdatacite:10.22008/fk2/oepn9z |
---|---|
record_format |
openpolar |
spelling |
ftdatacite:10.22008/fk2/oepn9z 2023-05-15T16:01:04+02:00 AEROMAG 1997 - Aeromagnetic survey - Disko Bay, Greenland Feargal, Murphy Maurice, Coyle 2021 https://dx.doi.org/10.22008/fk2/oepn9z https://dataverse01.geus.dk/citation?persistentId=doi:10.22008/FK2/OEPN9Z unknown GEUS Dataverse https://dx.doi.org/10.22008/fk2/oepn9z/bkb71l https://dx.doi.org/10.22008/fk2/oepn9z/xxrdul https://dx.doi.org/10.22008/fk2/oepn9z/jvpg1t https://dx.doi.org/10.22008/fk2/oepn9z/zmhpbr https://dx.doi.org/10.22008/fk2/oepn9z/ifvtrr https://dx.doi.org/10.22008/fk2/oepn9z/qqdx94 https://dx.doi.org/10.22008/fk2/oepn9z/v3jrvt https://dx.doi.org/10.22008/fk2/oepn9z/yg7ygd https://dx.doi.org/10.22008/fk2/oepn9z/iquvyi https://dx.doi.org/10.22008/fk2/oepn9z/bwbezi dataset Dataset 2021 ftdatacite https://doi.org/10.22008/fk2/oepn9z https://doi.org/10.22008/fk2/oepn9z/bkb71l https://doi.org/10.22008/fk2/oepn9z/xxrdul https://doi.org/10.22008/fk2/oepn9z/jvpg1t https://doi.org/10.22008/fk2/oepn9z/zmhpbr https://doi.org/10.22008/fk2/oepn9z/i 2021-11-05T12:55:41Z The Aeromag 1997 project was conducted over the Disko-Nuussuaq region of central West Greenland (size: 46 390 km²). The survey area was located both onshore and offshore. The data were collected and processed by Sanders Geophysics Ltd. and financed by the Greenlandic government. The regular line direction was north-south with tie-lines east-west. The easternmost part of the survey area was flown with a line spacing of 500 metres, while the westernmost part of the survey area was flown with a line spacing of 1000 metres. Control lines were flown with a spacing of 5000 metres. The easternmost part of the survey area is dominated by Precambrian basement terrain, while the westernmost part,which includes offshore areas, is dominated by Tertiary basaltsin a mainly Cretaceous sedimentary basin.The northermost part of the survey reaches into the Karrat region of Umanak Fjord. The Precambrian terrain consistsof orthogneisses, intercalated with units of strongly deformed Archaean supracrustal rocks which compriseboth metavolcanic and metasedimentary rocks where local gold occurrences have been found. Most of the region was overprinted by early Proterozoic deformation and metamorphism. A detailed investigation of a 400 square km area off-shore the eastern coast of Disko Ø was flown in 1998, in order to map a circular shaped anomaly. Dataset Disko Bay Greenland greenlandic Nuussuaq DataCite Metadata Store (German National Library of Science and Technology) Greenland Nuussuaq ENVELOPE(-51.918,-51.918,66.626,66.626) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
unknown |
description |
The Aeromag 1997 project was conducted over the Disko-Nuussuaq region of central West Greenland (size: 46 390 km²). The survey area was located both onshore and offshore. The data were collected and processed by Sanders Geophysics Ltd. and financed by the Greenlandic government. The regular line direction was north-south with tie-lines east-west. The easternmost part of the survey area was flown with a line spacing of 500 metres, while the westernmost part of the survey area was flown with a line spacing of 1000 metres. Control lines were flown with a spacing of 5000 metres. The easternmost part of the survey area is dominated by Precambrian basement terrain, while the westernmost part,which includes offshore areas, is dominated by Tertiary basaltsin a mainly Cretaceous sedimentary basin.The northermost part of the survey reaches into the Karrat region of Umanak Fjord. The Precambrian terrain consistsof orthogneisses, intercalated with units of strongly deformed Archaean supracrustal rocks which compriseboth metavolcanic and metasedimentary rocks where local gold occurrences have been found. Most of the region was overprinted by early Proterozoic deformation and metamorphism. A detailed investigation of a 400 square km area off-shore the eastern coast of Disko Ø was flown in 1998, in order to map a circular shaped anomaly. |
format |
Dataset |
author |
Feargal, Murphy Maurice, Coyle |
spellingShingle |
Feargal, Murphy Maurice, Coyle AEROMAG 1997 - Aeromagnetic survey - Disko Bay, Greenland |
author_facet |
Feargal, Murphy Maurice, Coyle |
author_sort |
Feargal, Murphy |
title |
AEROMAG 1997 - Aeromagnetic survey - Disko Bay, Greenland |
title_short |
AEROMAG 1997 - Aeromagnetic survey - Disko Bay, Greenland |
title_full |
AEROMAG 1997 - Aeromagnetic survey - Disko Bay, Greenland |
title_fullStr |
AEROMAG 1997 - Aeromagnetic survey - Disko Bay, Greenland |
title_full_unstemmed |
AEROMAG 1997 - Aeromagnetic survey - Disko Bay, Greenland |
title_sort |
aeromag 1997 - aeromagnetic survey - disko bay, greenland |
publisher |
GEUS Dataverse |
publishDate |
2021 |
url |
https://dx.doi.org/10.22008/fk2/oepn9z https://dataverse01.geus.dk/citation?persistentId=doi:10.22008/FK2/OEPN9Z |
long_lat |
ENVELOPE(-51.918,-51.918,66.626,66.626) |
geographic |
Greenland Nuussuaq |
geographic_facet |
Greenland Nuussuaq |
genre |
Disko Bay Greenland greenlandic Nuussuaq |
genre_facet |
Disko Bay Greenland greenlandic Nuussuaq |
op_relation |
https://dx.doi.org/10.22008/fk2/oepn9z/bkb71l https://dx.doi.org/10.22008/fk2/oepn9z/xxrdul https://dx.doi.org/10.22008/fk2/oepn9z/jvpg1t https://dx.doi.org/10.22008/fk2/oepn9z/zmhpbr https://dx.doi.org/10.22008/fk2/oepn9z/ifvtrr https://dx.doi.org/10.22008/fk2/oepn9z/qqdx94 https://dx.doi.org/10.22008/fk2/oepn9z/v3jrvt https://dx.doi.org/10.22008/fk2/oepn9z/yg7ygd https://dx.doi.org/10.22008/fk2/oepn9z/iquvyi https://dx.doi.org/10.22008/fk2/oepn9z/bwbezi |
op_doi |
https://doi.org/10.22008/fk2/oepn9z https://doi.org/10.22008/fk2/oepn9z/bkb71l https://doi.org/10.22008/fk2/oepn9z/xxrdul https://doi.org/10.22008/fk2/oepn9z/jvpg1t https://doi.org/10.22008/fk2/oepn9z/zmhpbr https://doi.org/10.22008/fk2/oepn9z/i |
_version_ |
1766397063266828288 |