Detrital zircon sedimentary provenance ages for the Eoarchaean Isua supracrustal belt southern West Greenland: Juxtaposition of an imbricated ca. 3700Ma juvenile arc against an older complex with 3920-3760 Ma components
The amphibolite facies Eoarchaean Isua supracrustal belt (northern part of the Nuuk region, southern West Greenland) is dominated by strongly deformed metabasalts, with chert, banded iron formation, felsic volcanic and volcano-sedimentary rocks and minor
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Online Access: | http://hdl.handle.net/1885/49847 |
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ftanucanberra:oai:digitalcollections.anu.edu.au:1885/49847 2023-05-15T16:25:00+02:00 Detrital zircon sedimentary provenance ages for the Eoarchaean Isua supracrustal belt southern West Greenland: Juxtaposition of an imbricated ca. 3700Ma juvenile arc against an older complex with 3920-3760 Ma components Nutman, Allen Friend, Clark R.L. Paxton, Shane 2015-12-10T22:13:39Z http://hdl.handle.net/1885/49847 unknown Elsevier 0301-9268 http://hdl.handle.net/1885/49847 Precambrian Research Journal article 2015 ftanucanberra 2015-12-28T23:26:50Z The amphibolite facies Eoarchaean Isua supracrustal belt (northern part of the Nuuk region, southern West Greenland) is dominated by strongly deformed metabasalts, with chert, banded iron formation, felsic volcanic and volcano-sedimentary rocks and minor Article in Journal/Newspaper Greenland Nuuk Australian National University: ANU Digital Collections Greenland Nuuk ENVELOPE(-52.150,-52.150,68.717,68.717) |
institution |
Open Polar |
collection |
Australian National University: ANU Digital Collections |
op_collection_id |
ftanucanberra |
language |
unknown |
description |
The amphibolite facies Eoarchaean Isua supracrustal belt (northern part of the Nuuk region, southern West Greenland) is dominated by strongly deformed metabasalts, with chert, banded iron formation, felsic volcanic and volcano-sedimentary rocks and minor |
format |
Article in Journal/Newspaper |
author |
Nutman, Allen Friend, Clark R.L. Paxton, Shane |
spellingShingle |
Nutman, Allen Friend, Clark R.L. Paxton, Shane Detrital zircon sedimentary provenance ages for the Eoarchaean Isua supracrustal belt southern West Greenland: Juxtaposition of an imbricated ca. 3700Ma juvenile arc against an older complex with 3920-3760 Ma components |
author_facet |
Nutman, Allen Friend, Clark R.L. Paxton, Shane |
author_sort |
Nutman, Allen |
title |
Detrital zircon sedimentary provenance ages for the Eoarchaean Isua supracrustal belt southern West Greenland: Juxtaposition of an imbricated ca. 3700Ma juvenile arc against an older complex with 3920-3760 Ma components |
title_short |
Detrital zircon sedimentary provenance ages for the Eoarchaean Isua supracrustal belt southern West Greenland: Juxtaposition of an imbricated ca. 3700Ma juvenile arc against an older complex with 3920-3760 Ma components |
title_full |
Detrital zircon sedimentary provenance ages for the Eoarchaean Isua supracrustal belt southern West Greenland: Juxtaposition of an imbricated ca. 3700Ma juvenile arc against an older complex with 3920-3760 Ma components |
title_fullStr |
Detrital zircon sedimentary provenance ages for the Eoarchaean Isua supracrustal belt southern West Greenland: Juxtaposition of an imbricated ca. 3700Ma juvenile arc against an older complex with 3920-3760 Ma components |
title_full_unstemmed |
Detrital zircon sedimentary provenance ages for the Eoarchaean Isua supracrustal belt southern West Greenland: Juxtaposition of an imbricated ca. 3700Ma juvenile arc against an older complex with 3920-3760 Ma components |
title_sort |
detrital zircon sedimentary provenance ages for the eoarchaean isua supracrustal belt southern west greenland: juxtaposition of an imbricated ca. 3700ma juvenile arc against an older complex with 3920-3760 ma components |
publisher |
Elsevier |
publishDate |
2015 |
url |
http://hdl.handle.net/1885/49847 |
long_lat |
ENVELOPE(-52.150,-52.150,68.717,68.717) |
geographic |
Greenland Nuuk |
geographic_facet |
Greenland Nuuk |
genre |
Greenland Nuuk |
genre_facet |
Greenland Nuuk |
op_source |
Precambrian Research |
op_relation |
0301-9268 http://hdl.handle.net/1885/49847 |
_version_ |
1766013642100178944 |