Ordovician rocks in the Eastcan et al. Freydis B-87 and other wells in offshore Atlantic Canada

Acritarchs and Chitinozoa from the lower 1300 ft (400 m) of the Eastcan et al. Freydis B-87 well, Labrador Shelf, indicate that these strata accumulated in a marine setting during Late Ordovician time. Five or more other exploratory wells on the Labrador Shelf and the Grand Banks of Newfoundland als...

Full description

Bibliographic Details
Published in:Canadian Journal of Earth Sciences
Main Author: Jenkins, W. A. M.
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1984
Subjects:
Online Access:http://dx.doi.org/10.1139/e84-092
http://www.nrcresearchpress.com/doi/pdf/10.1139/e84-092
id crcansciencepubl:10.1139/e84-092
record_format openpolar
spelling crcansciencepubl:10.1139/e84-092 2024-09-15T18:19:55+00:00 Ordovician rocks in the Eastcan et al. Freydis B-87 and other wells in offshore Atlantic Canada Jenkins, W. A. M. 1984 http://dx.doi.org/10.1139/e84-092 http://www.nrcresearchpress.com/doi/pdf/10.1139/e84-092 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Earth Sciences volume 21, issue 7, page 864-868 ISSN 0008-4077 1480-3313 journal-article 1984 crcansciencepubl https://doi.org/10.1139/e84-092 2024-07-25T04:10:05Z Acritarchs and Chitinozoa from the lower 1300 ft (400 m) of the Eastcan et al. Freydis B-87 well, Labrador Shelf, indicate that these strata accumulated in a marine setting during Late Ordovician time. Five or more other exploratory wells on the Labrador Shelf and the Grand Banks of Newfoundland also have encountered Ordovician rocks. Article in Journal/Newspaper Newfoundland Canadian Science Publishing Canadian Journal of Earth Sciences 21 7 864 868
institution Open Polar
collection Canadian Science Publishing
op_collection_id crcansciencepubl
language English
description Acritarchs and Chitinozoa from the lower 1300 ft (400 m) of the Eastcan et al. Freydis B-87 well, Labrador Shelf, indicate that these strata accumulated in a marine setting during Late Ordovician time. Five or more other exploratory wells on the Labrador Shelf and the Grand Banks of Newfoundland also have encountered Ordovician rocks.
format Article in Journal/Newspaper
author Jenkins, W. A. M.
spellingShingle Jenkins, W. A. M.
Ordovician rocks in the Eastcan et al. Freydis B-87 and other wells in offshore Atlantic Canada
author_facet Jenkins, W. A. M.
author_sort Jenkins, W. A. M.
title Ordovician rocks in the Eastcan et al. Freydis B-87 and other wells in offshore Atlantic Canada
title_short Ordovician rocks in the Eastcan et al. Freydis B-87 and other wells in offshore Atlantic Canada
title_full Ordovician rocks in the Eastcan et al. Freydis B-87 and other wells in offshore Atlantic Canada
title_fullStr Ordovician rocks in the Eastcan et al. Freydis B-87 and other wells in offshore Atlantic Canada
title_full_unstemmed Ordovician rocks in the Eastcan et al. Freydis B-87 and other wells in offshore Atlantic Canada
title_sort ordovician rocks in the eastcan et al. freydis b-87 and other wells in offshore atlantic canada
publisher Canadian Science Publishing
publishDate 1984
url http://dx.doi.org/10.1139/e84-092
http://www.nrcresearchpress.com/doi/pdf/10.1139/e84-092
genre Newfoundland
genre_facet Newfoundland
op_source Canadian Journal of Earth Sciences
volume 21, issue 7, page 864-868
ISSN 0008-4077 1480-3313
op_rights http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining
op_doi https://doi.org/10.1139/e84-092
container_title Canadian Journal of Earth Sciences
container_volume 21
container_issue 7
container_start_page 864
op_container_end_page 868
_version_ 1810458274234892288