000 02177nam  2200373za 4500
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008160726s2011    nsc|||||o    f|0| 0 eng d
040 |aCaOODSP|beng
043 |an-cn---
0861 |aM183-2/6838E-PDF
1001 |aGould, K.M.
24510|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.
260 |aDartmouth, N.S. : |bNatural Resources Canada, Geological Survey of Canada, |c2011.
300 |a87 p. : |bphotos, tables, figures, graphs.
4901 |aOpen file (Geological Survey of Canada)|v6838
504 |aIncludes bibliographical references.
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. ...
69207|2gccst|aPetrology
69207|2gccst|aSedimentology
693 4|aPetrography
693 4|aLithofacies
693 4|aSandstones
693 4|aWells
7001 |aPiper, D. J. W.
7001 |aPe-Piper, Georgia.
7101 |aCanada. |bNatural Resources Canada.
7102 |aGeological Survey of Canada (Atlantic)
7102 |aBedford Institute of Oceanography.
7102 |aGeological Survey of Canada.
830#0|aOpen file (Geological Survey of Canada)|v6838|w(CaOODSP)9.506878
85640|qPDF|s7.64 MB|uhttps://publications.gc.ca/collections/collection_2016/rncan-nrcan/M183-2-6838-eng.pdf