Origin and Emplacement of Acadian Granitic Rocks, Northern Cape Breton Island
Acadian granitic rocks in northern Cape Breton Island consist entirely of even-grained leucocratic granodiorite and adamellite. The compositional range is small, and the average composition corresponds well with melts that could be generated in the crust. Abundant pegmatites in the contact zone sugg...
Published in: | Canadian Journal of Earth Sciences |
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Language: | English |
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Canadian Science Publishing
1975
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Online Access: | http://dx.doi.org/10.1139/e75-022 http://www.nrcresearchpress.com/doi/pdf/10.1139/e75-022 |
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crcansciencepubl:10.1139/e75-022 2023-12-17T10:28:22+01:00 Origin and Emplacement of Acadian Granitic Rocks, Northern Cape Breton Island Wiebe, Robert A. 1975 http://dx.doi.org/10.1139/e75-022 http://www.nrcresearchpress.com/doi/pdf/10.1139/e75-022 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Earth Sciences volume 12, issue 2, page 252-262 ISSN 0008-4077 1480-3313 General Earth and Planetary Sciences journal-article 1975 crcansciencepubl https://doi.org/10.1139/e75-022 2023-11-19T13:38:28Z Acadian granitic rocks in northern Cape Breton Island consist entirely of even-grained leucocratic granodiorite and adamellite. The compositional range is small, and the average composition corresponds well with melts that could be generated in the crust. Abundant pegmatites in the contact zone suggest high water content.Within the major plutons these granitic rocks show: (1) high scatter on a Rb–Sr isochron (Cormier 1972), (2) apparently random areal variation in K and Ca, but a systematic areal variation in K/Rb and Ca/Sr, and (3) high scatter of Na 2 O and K 2 O on plots against differentiation index. The minor compositional heterogeneity indicated by these relations could have originated within the source region of melting or by assimilation during emplacement.The granitic plutons are elongate north–south and occur in an en echelon pattern within a NNE-trending migmatite zone. The spatial arrangement of pre-emplacement structures in the country rock and the distribution of xenoliths in the intrusions suggest that emplacement was accommodated by east–west expansion, upbowing of the surrounding country rock, faulting, and minor stoping. Article in Journal/Newspaper Breton Island Canadian Science Publishing (via Crossref) Breton Island ENVELOPE(141.383,141.383,-66.800,-66.800) Canadian Journal of Earth Sciences 12 2 252 262 |
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 Wiebe, Robert A. Origin and Emplacement of Acadian Granitic Rocks, Northern Cape Breton Island |
topic_facet |
General Earth and Planetary Sciences |
description |
Acadian granitic rocks in northern Cape Breton Island consist entirely of even-grained leucocratic granodiorite and adamellite. The compositional range is small, and the average composition corresponds well with melts that could be generated in the crust. Abundant pegmatites in the contact zone suggest high water content.Within the major plutons these granitic rocks show: (1) high scatter on a Rb–Sr isochron (Cormier 1972), (2) apparently random areal variation in K and Ca, but a systematic areal variation in K/Rb and Ca/Sr, and (3) high scatter of Na 2 O and K 2 O on plots against differentiation index. The minor compositional heterogeneity indicated by these relations could have originated within the source region of melting or by assimilation during emplacement.The granitic plutons are elongate north–south and occur in an en echelon pattern within a NNE-trending migmatite zone. The spatial arrangement of pre-emplacement structures in the country rock and the distribution of xenoliths in the intrusions suggest that emplacement was accommodated by east–west expansion, upbowing of the surrounding country rock, faulting, and minor stoping. |
format |
Article in Journal/Newspaper |
author |
Wiebe, Robert A. |
author_facet |
Wiebe, Robert A. |
author_sort |
Wiebe, Robert A. |
title |
Origin and Emplacement of Acadian Granitic Rocks, Northern Cape Breton Island |
title_short |
Origin and Emplacement of Acadian Granitic Rocks, Northern Cape Breton Island |
title_full |
Origin and Emplacement of Acadian Granitic Rocks, Northern Cape Breton Island |
title_fullStr |
Origin and Emplacement of Acadian Granitic Rocks, Northern Cape Breton Island |
title_full_unstemmed |
Origin and Emplacement of Acadian Granitic Rocks, Northern Cape Breton Island |
title_sort |
origin and emplacement of acadian granitic rocks, northern cape breton island |
publisher |
Canadian Science Publishing |
publishDate |
1975 |
url |
http://dx.doi.org/10.1139/e75-022 http://www.nrcresearchpress.com/doi/pdf/10.1139/e75-022 |
long_lat |
ENVELOPE(141.383,141.383,-66.800,-66.800) |
geographic |
Breton Island |
geographic_facet |
Breton Island |
genre |
Breton Island |
genre_facet |
Breton Island |
op_source |
Canadian Journal of Earth Sciences volume 12, issue 2, page 252-262 ISSN 0008-4077 1480-3313 |
op_rights |
http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining |
op_doi |
https://doi.org/10.1139/e75-022 |
container_title |
Canadian Journal of Earth Sciences |
container_volume |
12 |
container_issue |
2 |
container_start_page |
252 |
op_container_end_page |
262 |
_version_ |
1785580460683821056 |