Racklan Orogen

The term Racklan Orogen is applied to an extensive region of deformed rocks that underlies northwestern Canada. At least one period of deformation predated extrusion of the ca. 1267–1270 Ma basalt of the Coppermine River Group, and at least two periods of deformation postdated extrusion of the Coppe...

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Published in:Canadian Journal of Earth Sciences
Main Author: Cook, Frederick A.
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1992
Subjects:
Online Access:http://dx.doi.org/10.1139/e92-195
http://www.nrcresearchpress.com/doi/pdf/10.1139/e92-195
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spelling crcansciencepubl:10.1139/e92-195 2023-12-17T10:28:57+01:00 Racklan Orogen Cook, Frederick A. 1992 http://dx.doi.org/10.1139/e92-195 http://www.nrcresearchpress.com/doi/pdf/10.1139/e92-195 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Earth Sciences volume 29, issue 11, page 2490-2496 ISSN 0008-4077 1480-3313 General Earth and Planetary Sciences journal-article 1992 crcansciencepubl https://doi.org/10.1139/e92-195 2023-11-19T13:38:20Z The term Racklan Orogen is applied to an extensive region of deformed rocks that underlies northwestern Canada. At least one period of deformation predated extrusion of the ca. 1267–1270 Ma basalt of the Coppermine River Group, and at least two periods of deformation postdated extrusion of the Coppermine basalt. Limits on the age of deformation can be confidently placed between 1663 Ma (the age of the Narakay volcanic complex that postdates uppermost strata of the Hornby Bay Group) and 1100–800 Ma (the maximum age of the Mackenzie Mountains Supergroup). Article in Journal/Newspaper Coppermine River Mackenzie mountains Canadian Science Publishing (via Crossref) Canada Hornby Bay ENVELOPE(-118.087,-118.087,66.467,66.467) Canadian Journal of Earth Sciences 29 11 2490 2496
institution Open Polar
collection Canadian Science Publishing (via Crossref)
op_collection_id crcansciencepubl
language English
topic General Earth and Planetary Sciences
spellingShingle General Earth and Planetary Sciences
Cook, Frederick A.
Racklan Orogen
topic_facet General Earth and Planetary Sciences
description The term Racklan Orogen is applied to an extensive region of deformed rocks that underlies northwestern Canada. At least one period of deformation predated extrusion of the ca. 1267–1270 Ma basalt of the Coppermine River Group, and at least two periods of deformation postdated extrusion of the Coppermine basalt. Limits on the age of deformation can be confidently placed between 1663 Ma (the age of the Narakay volcanic complex that postdates uppermost strata of the Hornby Bay Group) and 1100–800 Ma (the maximum age of the Mackenzie Mountains Supergroup).
format Article in Journal/Newspaper
author Cook, Frederick A.
author_facet Cook, Frederick A.
author_sort Cook, Frederick A.
title Racklan Orogen
title_short Racklan Orogen
title_full Racklan Orogen
title_fullStr Racklan Orogen
title_full_unstemmed Racklan Orogen
title_sort racklan orogen
publisher Canadian Science Publishing
publishDate 1992
url http://dx.doi.org/10.1139/e92-195
http://www.nrcresearchpress.com/doi/pdf/10.1139/e92-195
long_lat ENVELOPE(-118.087,-118.087,66.467,66.467)
geographic Canada
Hornby Bay
geographic_facet Canada
Hornby Bay
genre Coppermine River
Mackenzie mountains
genre_facet Coppermine River
Mackenzie mountains
op_source Canadian Journal of Earth Sciences
volume 29, issue 11, page 2490-2496
ISSN 0008-4077 1480-3313
op_rights http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining
op_doi https://doi.org/10.1139/e92-195
container_title Canadian Journal of Earth Sciences
container_volume 29
container_issue 11
container_start_page 2490
op_container_end_page 2496
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