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| 02177nam 2200373za 4500 |
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001 | 9.821658 |
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003 | CaOODSP |
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005 | 20230131161137 |
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007 | cr ||||||||||| |
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008 | 160726s2011 nsc|||||o f|0| 0 eng d |
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040 | |aCaOODSP|beng |
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043 | |an-cn--- |
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086 | 1 |aM183-2/6838E-PDF |
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100 | 1 |aGould, K.M. |
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245 | 10|aLateral correlation of sediment facies in the Panuke and Venture fields, Scotian Basin |h[electronic resource] : |bimplications for reservoir connectivity / |cK.M. Gould, D.J.W. Piper, and G. Pe-Piper. |
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260 | |aDartmouth, N.S. : |bNatural Resources Canada, Geological Survey of Canada, |c2011. |
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300 | |a87 p. : |bphotos, tables, figures, graphs. |
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490 | 1 |aOpen file (Geological Survey of Canada)|v6838 |
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504 | |aIncludes bibliographical references. |
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520 | |aGamma logs and conventional core have been correlated in Upper Jurassic–Lower Cretaceous deltaic successions from closely spaced wells in two areas of the Scotian Basin: around the Panuke and Cohasset fields, and the West Venture-Venture fields. In the Panuke-Cohasset area, the Como P-21, Panuke B-90, Cohasset A-52, Balmoral M-32, and Lawrence D-14 wells, located 3–8 km apart, have been correlated in the upper part of the Missisauga Formation and the Cree Member of the Logan Canyon Formation. In the West Venture-Venture area, the West Olympia O-51, West Venture N-91, West Venture C-62, Venture B-52, and Venture H-22 wells, located 2.5 to 11.5 km apart, have been correlated in the Lower Member of the Missisauga Formation. ... |
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692 | 07|2gccst|aPetrology |
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692 | 07|2gccst|aSedimentology |
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693 | 4|aPetrography |
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693 | 4|aLithofacies |
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693 | 4|aSandstones |
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693 | 4|aWells |
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700 | 1 |aPiper, D. J. W. |
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700 | 1 |aPe-Piper, Georgia. |
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710 | 1 |aCanada. |bNatural Resources Canada. |
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710 | 2 |aGeological Survey of Canada (Atlantic) |
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710 | 2 |aBedford Institute of Oceanography. |
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710 | 2 |aGeological Survey of Canada. |
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830 | #0|aOpen file (Geological Survey of Canada)|v6838|w(CaOODSP)9.506878 |
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856 | 40|qPDF|s7.64 MB|uhttps://publications.gc.ca/collections/collection_2016/rncan-nrcan/M183-2-6838-eng.pdf |
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