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| 02130cam 2200349za 4500 |
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| 001 | 9.837138 |
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| 003 | CaOODSP |
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| 005 | 20221107151051 |
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| 007 | cr ||||||||||| |
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| 008 | 170523s1990 oncdba |o f|0| 0 eng d |
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| 020 | |z0-660-13725-9 |
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| 040 | |aCaOODSP|beng |
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| 041 | |aeng|bfre |
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| 043 | |an-cn--- |
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| 086 | 1 |aM44-89/17E-PDF|zM44-89/17E |
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| 100 | 1 |aMcAlpine, K. D. |
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| 245 | 10|aMesozoic stratigraphy, sedimentary evolution, and petroleum potential of the Jeanne D'Arc Basin, Grand Banks of Newfoundland |h[electronic resource] / |cK.D. McAlpine. |
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| 260 | |aOttawa : |bGeological Survey of Canada, |cc1990. |
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| 300 | |a50 p. : |bcharts, maps, ill. |
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| 490 | 1 |aGeological Survey of Canada. Paper ;|v89-17 |
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| 500 | |aDigitized edition from print 2013 [produced by Natural Resources Canada]. |
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| 504 | |aIncludes bibliographical references. |
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| 520 | |a"The Jeanne d'Arc Basin, located at the northeastern part of the Grand Banks of Newfoundland, is a Mesozoic failed-rift basin containing in excess of 22 km of sedimentary fill. Despite a period of vigorous exploration activity initiated by the discovery of the giant-class Hibernia oil field in 1979, the lithostratigraphic nomenclature is not yet standard. This has led to a plethora of lithostratigraphies used by various industry groups, government agencies, and academia, a situation that has caused communication problems. A new lithostratigraphic nomenclature is proposed for the Mesozoic rocks older than the Late Cretaceous Dawson Canyon Formation. The tzomenclature consists of 17 formations (14 new), 3 members (new), and 2 markers (new)"--Abstract, p. 1. |
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| 546 | |aAbstract and summary in English and French. |
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| 692 | 07|2gccst|aStratigraphy |
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| 692 | 07|2gccst|aSediments |
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| 692 | 07|2gccst|aPetroleum |
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| 692 | 07|2gccst|aGeology |
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| 710 | 1 |aCanada. |bEnergy, Mines and Resources Canada. |
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| 710 | 2 |aGeological Survey of Canada. |
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| 830 | #0|aGeological Survey of Canada. Paper ;|v89-17|w(CaOODSP)9.815431 |
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| 856 | 40|qPDF|s7.11 MB|uhttps://publications.gc.ca/collections/collection_2017/rncan-nrcan/M44-89-17-eng.pdf |
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