Petrology of ODP Leg 210 and Leg 173, and DSDP Leg 47 sites ...
Sand detrital modes of Albian-Eocene clastic gravity-flow deposits cored and recovered at Ocean Drilling Program Site 1276 reflect the postrift geologic evolution of the Newfoundland passive continental margin. Cretaceous sandstone compositions (average: Q57F23L20; Ls%Lsc = 35; total%bioclasts = 3)...
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ftdatacite:10.1594/pangaea.776571 2024-09-30T14:38:55+00:00 Petrology of ODP Leg 210 and Leg 173, and DSDP Leg 47 sites ... Marsaglia, Kathleen M Pavia, Jennifer A Maloney, Sara J 2007 application/zip https://dx.doi.org/10.1594/pangaea.776571 https://doi.pangaea.de/10.1594/PANGAEA.776571 en eng PANGAEA https://dx.doi.org/10.2973/odp.proc.sr.210.107.2007 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig Leg47 Leg173 Leg210 Glomar Challenger Joides Resolution Deep Sea Drilling Project DSDP Ocean Drilling Program ODP Collection Supplementary Publication Series of Datasets article 2007 ftdatacite https://doi.org/10.1594/pangaea.77657110.2973/odp.proc.sr.210.107.2007 2024-09-02T08:37:33Z Sand detrital modes of Albian-Eocene clastic gravity-flow deposits cored and recovered at Ocean Drilling Program Site 1276 reflect the postrift geologic evolution of the Newfoundland passive continental margin. Cretaceous sandstone compositions (average: Q57F23L20; Ls%Lsc = 35; total%bioclasts = 3) are consistent with a source on Grand Banks such as Avalon Uplift. Their relatively low potassium feldspar (Qm71K8P21) contents distinguish them from Iberian sandstones and appear to preclude an easterly source during the early history of the ocean basin. Isolated volcaniclastic input near the Paleocene/Eocene boundary (~60 Ma) at Site 1276 is also present in Iberian samples of this age, suggesting that magmatism was widespread across the North Atlantic during this time frame; the source(s) of this volcanic debris remains equivocal. In the Eocene, the development of carbonate bank facies on the shelf marks a profound compositional change to calcareous grainstones (average: Q27F11L62; Ls%Lsc = 82; total%bioclasts = ... : Supplement to: Marsaglia, Kathleen M; Pavia, Jennifer A; Maloney, Sara J (2007): Petrology and provenance of Eocene-Albian sandstones and grainstones recovered during ODP Leg 210: Implications for passive margin (rift-to-drift) sandstone provenance models. In: Tucholke, BE; Sibuet, J-C; Klaus, A (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 210, 1-47 ... Article in Journal/Newspaper Newfoundland North Atlantic DataCite Klaus ENVELOPE(24.117,24.117,65.717,65.717) Maloney ENVELOPE(-163.583,-163.583,-85.683,-85.683) |
institution |
Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Drilling/drill rig Leg47 Leg173 Leg210 Glomar Challenger Joides Resolution Deep Sea Drilling Project DSDP Ocean Drilling Program ODP |
spellingShingle |
Drilling/drill rig Leg47 Leg173 Leg210 Glomar Challenger Joides Resolution Deep Sea Drilling Project DSDP Ocean Drilling Program ODP Marsaglia, Kathleen M Pavia, Jennifer A Maloney, Sara J Petrology of ODP Leg 210 and Leg 173, and DSDP Leg 47 sites ... |
topic_facet |
Drilling/drill rig Leg47 Leg173 Leg210 Glomar Challenger Joides Resolution Deep Sea Drilling Project DSDP Ocean Drilling Program ODP |
description |
Sand detrital modes of Albian-Eocene clastic gravity-flow deposits cored and recovered at Ocean Drilling Program Site 1276 reflect the postrift geologic evolution of the Newfoundland passive continental margin. Cretaceous sandstone compositions (average: Q57F23L20; Ls%Lsc = 35; total%bioclasts = 3) are consistent with a source on Grand Banks such as Avalon Uplift. Their relatively low potassium feldspar (Qm71K8P21) contents distinguish them from Iberian sandstones and appear to preclude an easterly source during the early history of the ocean basin. Isolated volcaniclastic input near the Paleocene/Eocene boundary (~60 Ma) at Site 1276 is also present in Iberian samples of this age, suggesting that magmatism was widespread across the North Atlantic during this time frame; the source(s) of this volcanic debris remains equivocal. In the Eocene, the development of carbonate bank facies on the shelf marks a profound compositional change to calcareous grainstones (average: Q27F11L62; Ls%Lsc = 82; total%bioclasts = ... : Supplement to: Marsaglia, Kathleen M; Pavia, Jennifer A; Maloney, Sara J (2007): Petrology and provenance of Eocene-Albian sandstones and grainstones recovered during ODP Leg 210: Implications for passive margin (rift-to-drift) sandstone provenance models. In: Tucholke, BE; Sibuet, J-C; Klaus, A (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 210, 1-47 ... |
format |
Article in Journal/Newspaper |
author |
Marsaglia, Kathleen M Pavia, Jennifer A Maloney, Sara J |
author_facet |
Marsaglia, Kathleen M Pavia, Jennifer A Maloney, Sara J |
author_sort |
Marsaglia, Kathleen M |
title |
Petrology of ODP Leg 210 and Leg 173, and DSDP Leg 47 sites ... |
title_short |
Petrology of ODP Leg 210 and Leg 173, and DSDP Leg 47 sites ... |
title_full |
Petrology of ODP Leg 210 and Leg 173, and DSDP Leg 47 sites ... |
title_fullStr |
Petrology of ODP Leg 210 and Leg 173, and DSDP Leg 47 sites ... |
title_full_unstemmed |
Petrology of ODP Leg 210 and Leg 173, and DSDP Leg 47 sites ... |
title_sort |
petrology of odp leg 210 and leg 173, and dsdp leg 47 sites ... |
publisher |
PANGAEA |
publishDate |
2007 |
url |
https://dx.doi.org/10.1594/pangaea.776571 https://doi.pangaea.de/10.1594/PANGAEA.776571 |
long_lat |
ENVELOPE(24.117,24.117,65.717,65.717) ENVELOPE(-163.583,-163.583,-85.683,-85.683) |
geographic |
Klaus Maloney |
geographic_facet |
Klaus Maloney |
genre |
Newfoundland North Atlantic |
genre_facet |
Newfoundland North Atlantic |
op_relation |
https://dx.doi.org/10.2973/odp.proc.sr.210.107.2007 |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.77657110.2973/odp.proc.sr.210.107.2007 |
_version_ |
1811641505851375616 |