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001 | 9.836633 |
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003 | CaOODSP |
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005 | 20230221135047 |
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007 | cr ||||||||||| |
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008 | 170512s2017 oncab ob f000 0 eng d |
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040 | |aCaOODSP|beng |
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043 | |an-cn---|an-cn-nl |
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086 | 1 |aM183-2/8182E-PDF |
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100 | 1 |aWilliams, G. L. |
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245 | 10|aPalynological analyses of the two Labrador Shelf wells, Petro-Canada et al. Corte Real P-85 and Petro-Canada et al. Pothurst P-19, offshore Newfoundland and Labrador |h[electronic resource] / |cG.L. Williams. |
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260 | |a[Ottawa] : |bNatural Resources Canada, |c2017. |
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300 | |a50 p. : |bcol. ill., col. map + |e6 charts on 6 sheets |
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490 | 1 |aGeological Survey of Canada, open file ; |v8182 |
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500 | |aFig. 6 has been mis-labelled as fig. 2. |
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504 | |aIncludes bibliographical references (p. 27-32). |
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520 | |a"Both the Saglek and Hopedale sedimentary basins, located on the offshore Labrador margins, attracted hydrocarbon exploration in the 1970s and early 1980s. Two significant wells were Corte Real P-85 in the Hopedale Basin and Pothurst P-19 in the Saglek Basin. I undertook analyses of the organic-walled microfossils to determine the ages and paleoenvironments of the sediments in these wells. Both wells encountered only Tertiary sediments, with Corte Real P-85 being in the Ypresian at total depth and Pothurst P-19 being in the Lutetian at total depth. Reworking trends occur in both wells, with Carboniferous spores and Cretaceous spores and dinocysts common in Corte Real P-85, and reworked Cretaceous palynomorphs in Pothurst P-19, that presumably were transported from the west and northwest. Significant breaks in the section are the apparent absence of Bartonian and Middle Miocene and the attenuated Priabonian sediments in Pothurst P-19. Neither well discovered oil nor natural gas"--Summary provided by publisher. |
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692 | 07|2gccst|aNatural gas |
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692 | 07|2gccst|aPetroleum |
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692 | 07|2gccst|aPaleontology |
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692 | 07|2gccst|aStratigraphy |
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710 | 1 |aCanada. |bNatural Resources Canada. |
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710 | 2 |aGeological Survey of Canada. |
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830 | #0|aOpen file (Geological Survey of Canada)|v8182|w(CaOODSP)9.506878 |
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856 | 40|qPDF|s943 KB|uhttps://publications.gc.ca/collections/collection_2017/rncan-nrcan/M183-2/M183-2-8182-eng.pdf|zReport |
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856 | 40|qPDF|s2.17 MB|uhttps://publications.gc.ca/collections/collection_2017/rncan-nrcan/M183-2/M183-2-8182-1-eng.pdf|zFig. 2. Stratigraphy and paleoenvironments of Petro-Canada et al. Corte Real P-85 |
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856 | 40|qPDF|s397 KB|uhttps://publications.gc.ca/collections/collection_2017/rncan-nrcan/M183-2/M183-2-8182-2-eng.pdf|zFig. 3. Corte Real P-85 percentages |
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856 | 40|qPDF|s47 KB|uhttps://publications.gc.ca/collections/collection_2017/rncan-nrcan/M183-2/M183-2-8182-3-eng.pdf|zFig. 4. Plot showing stratigraphic ranges and abundances of dinocysts in Corte Real P-85 |
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856 | 40|qPDF|s106 KB|uhttps://publications.gc.ca/collections/collection_2017/rncan-nrcan/M183-2/M183-2-8182-4-eng.pdf|zFig. 5. Plot showing stratigraphic ranges and relative abundances of miospores, acritarchs and other palynomorphs in Corte Real P-85 |
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856 | 40|qPDF|s768 KB|uhttps://publications.gc.ca/collections/collection_2017/rncan-nrcan/M183-2/M183-2-8182-5-eng.pdf|zFig. [6]. Stratigraphy and paleoenvironments of Petro-Canada et al. Pothurst P-19 |
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856 | 40|qPDF|s33 KB|uhttps://publications.gc.ca/collections/collection_2017/rncan-nrcan/M183-2/M183-2-8182-6-eng.pdf|zFig. 7. Plot showing stratigraphic ranges of dinocysts in Pothurst P-19 |
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