Early Tertiary basalts from the Labrador Sea floor and Davis Strait region
Fine- to medium-grained, phyric and aphyric basalt samples from ODP Leg 105, site 647A, in the Labrador Sea show little evidence of alteration. Chemically, these rocks are low-potassium (0.01–0.09 wt.% K 2 O), olivine- to quartz-normative tholeiites that compare closely with the very depleted terres...
Published in: | Canadian Journal of Earth Sciences |
---|---|
Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Canadian Science Publishing
1989
|
Subjects: | |
Online Access: | http://dx.doi.org/10.1139/e89-077 http://www.nrcresearchpress.com/doi/pdf/10.1139/e89-077 |
id |
crcansciencepubl:10.1139/e89-077 |
---|---|
record_format |
openpolar |
spelling |
crcansciencepubl:10.1139/e89-077 2023-12-17T10:27:35+01:00 Early Tertiary basalts from the Labrador Sea floor and Davis Strait region Clarke, D. B. Cameron, B. I. Muecke, G. K. Bates, J. L. 1989 http://dx.doi.org/10.1139/e89-077 http://www.nrcresearchpress.com/doi/pdf/10.1139/e89-077 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Earth Sciences volume 26, issue 5, page 956-968 ISSN 0008-4077 1480-3313 General Earth and Planetary Sciences journal-article 1989 crcansciencepubl https://doi.org/10.1139/e89-077 2023-11-19T13:39:12Z Fine- to medium-grained, phyric and aphyric basalt samples from ODP Leg 105, site 647A, in the Labrador Sea show little evidence of alteration. Chemically, these rocks are low-potassium (0.01–0.09 wt.% K 2 O), olivine- to quartz-normative tholeiites that compare closely with the very depleted terrestrial Paleocene volcanic rocks in the Davis Strait region of Baffin Island and West Greenland. However, differences exist in the Sr–Nd isotope systematics of the two suites; the Labrador Sea samples have ε Nd values (+9.3) indicative of a more depleted source, and are higher in 87 Sr/ 86 Sr (0.7040), relative to the Davis Strait basalts (ε Nd +2.54 to +8.97; mean 87 Sr/ 86 Sr 0.7034). The higher 87 Sr/ 86 Sr in the Labrador Sea samples may reflect seawater exchange despite no petrographic evidence for significant alteration. The Labrador Sea and early Davis Strait basalts may have been derived from a similar depleted mantle source composition; however, the later Davis Strait magmas were generated from a different mantle. None of the Baffin Island, West Greenland, or Labrador Sea samples show unequivocal geochemical evidence for contamination with continental crust. Article in Journal/Newspaper Baffin Island Baffin Davis Strait Greenland Labrador Sea Canadian Science Publishing (via Crossref) Baffin Island Greenland Canadian Journal of Earth Sciences 26 5 956 968 |
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 Clarke, D. B. Cameron, B. I. Muecke, G. K. Bates, J. L. Early Tertiary basalts from the Labrador Sea floor and Davis Strait region |
topic_facet |
General Earth and Planetary Sciences |
description |
Fine- to medium-grained, phyric and aphyric basalt samples from ODP Leg 105, site 647A, in the Labrador Sea show little evidence of alteration. Chemically, these rocks are low-potassium (0.01–0.09 wt.% K 2 O), olivine- to quartz-normative tholeiites that compare closely with the very depleted terrestrial Paleocene volcanic rocks in the Davis Strait region of Baffin Island and West Greenland. However, differences exist in the Sr–Nd isotope systematics of the two suites; the Labrador Sea samples have ε Nd values (+9.3) indicative of a more depleted source, and are higher in 87 Sr/ 86 Sr (0.7040), relative to the Davis Strait basalts (ε Nd +2.54 to +8.97; mean 87 Sr/ 86 Sr 0.7034). The higher 87 Sr/ 86 Sr in the Labrador Sea samples may reflect seawater exchange despite no petrographic evidence for significant alteration. The Labrador Sea and early Davis Strait basalts may have been derived from a similar depleted mantle source composition; however, the later Davis Strait magmas were generated from a different mantle. None of the Baffin Island, West Greenland, or Labrador Sea samples show unequivocal geochemical evidence for contamination with continental crust. |
format |
Article in Journal/Newspaper |
author |
Clarke, D. B. Cameron, B. I. Muecke, G. K. Bates, J. L. |
author_facet |
Clarke, D. B. Cameron, B. I. Muecke, G. K. Bates, J. L. |
author_sort |
Clarke, D. B. |
title |
Early Tertiary basalts from the Labrador Sea floor and Davis Strait region |
title_short |
Early Tertiary basalts from the Labrador Sea floor and Davis Strait region |
title_full |
Early Tertiary basalts from the Labrador Sea floor and Davis Strait region |
title_fullStr |
Early Tertiary basalts from the Labrador Sea floor and Davis Strait region |
title_full_unstemmed |
Early Tertiary basalts from the Labrador Sea floor and Davis Strait region |
title_sort |
early tertiary basalts from the labrador sea floor and davis strait region |
publisher |
Canadian Science Publishing |
publishDate |
1989 |
url |
http://dx.doi.org/10.1139/e89-077 http://www.nrcresearchpress.com/doi/pdf/10.1139/e89-077 |
geographic |
Baffin Island Greenland |
geographic_facet |
Baffin Island Greenland |
genre |
Baffin Island Baffin Davis Strait Greenland Labrador Sea |
genre_facet |
Baffin Island Baffin Davis Strait Greenland Labrador Sea |
op_source |
Canadian Journal of Earth Sciences volume 26, issue 5, page 956-968 ISSN 0008-4077 1480-3313 |
op_rights |
http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining |
op_doi |
https://doi.org/10.1139/e89-077 |
container_title |
Canadian Journal of Earth Sciences |
container_volume |
26 |
container_issue |
5 |
container_start_page |
956 |
op_container_end_page |
968 |
_version_ |
1785579475671449600 |