Fossils from the Dunnage Mélange, north-central Newfoundland

Arenig conodonts and Tremadocian graptolites recovered from the Dunnage Mélange supplement previous fossil discoveries from the mélange and support the recent correlation of mélange lithologies with Exploits Group strata. The new fossil finds indicate that a block within the mélange is younger than...

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Published in:Canadian Journal of Earth Sciences
Main Authors: Hibbard, James P., Stouge, S., Skevington, D.
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1977
Subjects:
Online Access:http://dx.doi.org/10.1139/e77-107
http://www.nrcresearchpress.com/doi/pdf/10.1139/e77-107
id crcansciencepubl:10.1139/e77-107
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spelling crcansciencepubl:10.1139/e77-107 2024-10-13T14:09:07+00:00 Fossils from the Dunnage Mélange, north-central Newfoundland Hibbard, James P. Stouge, S. Skevington, D. 1977 http://dx.doi.org/10.1139/e77-107 http://www.nrcresearchpress.com/doi/pdf/10.1139/e77-107 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Earth Sciences volume 14, issue 5, page 1176-1178 ISSN 0008-4077 1480-3313 journal-article 1977 crcansciencepubl https://doi.org/10.1139/e77-107 2024-09-19T04:09:47Z Arenig conodonts and Tremadocian graptolites recovered from the Dunnage Mélange supplement previous fossil discoveries from the mélange and support the recent correlation of mélange lithologies with Exploits Group strata. The new fossil finds indicate that a block within the mélange is younger than portions of the matrix of this unit. This seemingly problematic relationship is resolvable in light of previous interpretations of a slump origin for the mélange as Tremadocian shales and Arenig carbonates were probably part of a pre-slump sedimentary–volcanic pile. The wide range in ages of fossils within the mélange is compatible with the interpretation that the mélange formed on a lower Paleozoic trench slope. Article in Journal/Newspaper Newfoundland Canadian Science Publishing Canadian Journal of Earth Sciences 14 5 1176 1178
institution Open Polar
collection Canadian Science Publishing
op_collection_id crcansciencepubl
language English
description Arenig conodonts and Tremadocian graptolites recovered from the Dunnage Mélange supplement previous fossil discoveries from the mélange and support the recent correlation of mélange lithologies with Exploits Group strata. The new fossil finds indicate that a block within the mélange is younger than portions of the matrix of this unit. This seemingly problematic relationship is resolvable in light of previous interpretations of a slump origin for the mélange as Tremadocian shales and Arenig carbonates were probably part of a pre-slump sedimentary–volcanic pile. The wide range in ages of fossils within the mélange is compatible with the interpretation that the mélange formed on a lower Paleozoic trench slope.
format Article in Journal/Newspaper
author Hibbard, James P.
Stouge, S.
Skevington, D.
spellingShingle Hibbard, James P.
Stouge, S.
Skevington, D.
Fossils from the Dunnage Mélange, north-central Newfoundland
author_facet Hibbard, James P.
Stouge, S.
Skevington, D.
author_sort Hibbard, James P.
title Fossils from the Dunnage Mélange, north-central Newfoundland
title_short Fossils from the Dunnage Mélange, north-central Newfoundland
title_full Fossils from the Dunnage Mélange, north-central Newfoundland
title_fullStr Fossils from the Dunnage Mélange, north-central Newfoundland
title_full_unstemmed Fossils from the Dunnage Mélange, north-central Newfoundland
title_sort fossils from the dunnage mélange, north-central newfoundland
publisher Canadian Science Publishing
publishDate 1977
url http://dx.doi.org/10.1139/e77-107
http://www.nrcresearchpress.com/doi/pdf/10.1139/e77-107
genre Newfoundland
genre_facet Newfoundland
op_source Canadian Journal of Earth Sciences
volume 14, issue 5, page 1176-1178
ISSN 0008-4077 1480-3313
op_rights http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining
op_doi https://doi.org/10.1139/e77-107
container_title Canadian Journal of Earth Sciences
container_volume 14
container_issue 5
container_start_page 1176
op_container_end_page 1178
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