Contrasting metamorphic terranes near Chéticamp, Cape Breton Highlands, Nova Scotia
Two contrasting metamorphic terranes can be recognized in northwestern Cape Breton Island. One terrane (Pleasant Bay complex) consists of biotite gneiss and quartzite with minor calc-silicate lenses that were metamorphosed in Late Precambrian time (about 550 Ma) and were subsequently intruded by Sil...
Published in: | Canadian Journal of Earth Sciences |
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Canadian Science Publishing
1987
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Online Access: | http://dx.doi.org/10.1139/e87-228 http://www.nrcresearchpress.com/doi/pdf/10.1139/e87-228 |
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crcansciencepubl:10.1139/e87-228 2023-12-17T10:28:22+01:00 Contrasting metamorphic terranes near Chéticamp, Cape Breton Highlands, Nova Scotia Currie, K. L. 1987 http://dx.doi.org/10.1139/e87-228 http://www.nrcresearchpress.com/doi/pdf/10.1139/e87-228 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Earth Sciences volume 24, issue 12, page 2422-2435 ISSN 0008-4077 1480-3313 General Earth and Planetary Sciences journal-article 1987 crcansciencepubl https://doi.org/10.1139/e87-228 2023-11-19T13:38:59Z Two contrasting metamorphic terranes can be recognized in northwestern Cape Breton Island. One terrane (Pleasant Bay complex) consists of biotite gneiss and quartzite with minor calc-silicate lenses that were metamorphosed in Late Precambrian time (about 550 Ma) and were subsequently intruded by Silurian salic and mafic plutons that were, in turn, deformed and intruded by granite in Devonian time. The other terrane (Jumping Brook complex) consists of volcanogenic and sedimentary schists of probable Silurian age that were metamorphosed in Devonian time. P–T estimates indicate that the older parts of the Pleasant Bay complex were metamorphosed at about 790 °C and 7 kbar (1 kbar = 100 MPa) at low to moderate water fugacities during a major intrusive episode. The Jumping Brook complex exhibits a single progressive metamorphic sequence now disrupted by faulting. P–T conditions during this Devonian (370–390 Ma) metamorphism varied from greenschist (300 °C at <3 kbar) to amphibolite (650 °C at 4 kbar) facies. Metamorphism probably occurred in a thermal dome. The data suggest a moderately deformed basement–cover relation between the Pleasant Bay and Jumping Brook complexes. Article in Journal/Newspaper Breton Island Canadian Science Publishing (via Crossref) Breton Island ENVELOPE(141.383,141.383,-66.800,-66.800) Dome The ENVELOPE(166.000,166.000,-85.367,-85.367) Canadian Journal of Earth Sciences 24 12 2422 2435 |
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Canadian Science Publishing (via Crossref) |
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crcansciencepubl |
language |
English |
topic |
General Earth and Planetary Sciences |
spellingShingle |
General Earth and Planetary Sciences Currie, K. L. Contrasting metamorphic terranes near Chéticamp, Cape Breton Highlands, Nova Scotia |
topic_facet |
General Earth and Planetary Sciences |
description |
Two contrasting metamorphic terranes can be recognized in northwestern Cape Breton Island. One terrane (Pleasant Bay complex) consists of biotite gneiss and quartzite with minor calc-silicate lenses that were metamorphosed in Late Precambrian time (about 550 Ma) and were subsequently intruded by Silurian salic and mafic plutons that were, in turn, deformed and intruded by granite in Devonian time. The other terrane (Jumping Brook complex) consists of volcanogenic and sedimentary schists of probable Silurian age that were metamorphosed in Devonian time. P–T estimates indicate that the older parts of the Pleasant Bay complex were metamorphosed at about 790 °C and 7 kbar (1 kbar = 100 MPa) at low to moderate water fugacities during a major intrusive episode. The Jumping Brook complex exhibits a single progressive metamorphic sequence now disrupted by faulting. P–T conditions during this Devonian (370–390 Ma) metamorphism varied from greenschist (300 °C at <3 kbar) to amphibolite (650 °C at 4 kbar) facies. Metamorphism probably occurred in a thermal dome. The data suggest a moderately deformed basement–cover relation between the Pleasant Bay and Jumping Brook complexes. |
format |
Article in Journal/Newspaper |
author |
Currie, K. L. |
author_facet |
Currie, K. L. |
author_sort |
Currie, K. L. |
title |
Contrasting metamorphic terranes near Chéticamp, Cape Breton Highlands, Nova Scotia |
title_short |
Contrasting metamorphic terranes near Chéticamp, Cape Breton Highlands, Nova Scotia |
title_full |
Contrasting metamorphic terranes near Chéticamp, Cape Breton Highlands, Nova Scotia |
title_fullStr |
Contrasting metamorphic terranes near Chéticamp, Cape Breton Highlands, Nova Scotia |
title_full_unstemmed |
Contrasting metamorphic terranes near Chéticamp, Cape Breton Highlands, Nova Scotia |
title_sort |
contrasting metamorphic terranes near chéticamp, cape breton highlands, nova scotia |
publisher |
Canadian Science Publishing |
publishDate |
1987 |
url |
http://dx.doi.org/10.1139/e87-228 http://www.nrcresearchpress.com/doi/pdf/10.1139/e87-228 |
long_lat |
ENVELOPE(141.383,141.383,-66.800,-66.800) ENVELOPE(166.000,166.000,-85.367,-85.367) |
geographic |
Breton Island Dome The |
geographic_facet |
Breton Island Dome The |
genre |
Breton Island |
genre_facet |
Breton Island |
op_source |
Canadian Journal of Earth Sciences volume 24, issue 12, page 2422-2435 ISSN 0008-4077 1480-3313 |
op_rights |
http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining |
op_doi |
https://doi.org/10.1139/e87-228 |
container_title |
Canadian Journal of Earth Sciences |
container_volume |
24 |
container_issue |
12 |
container_start_page |
2422 |
op_container_end_page |
2435 |
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1785580476450209792 |