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The AAPG/Datapages Combined Publications Database

AAPG Special Volumes


Pub. Id: A156 (1989)

First Page: 295

Last Page: 303

Book Title: M 46: Extensional Tectonics and Stratigraphy of the North Atlantic Margins

Article/Chapter: Environment of Petroleum Source Rock Deposition in the Jeanne d'Arc Basin Off Newfoundland: Chapter 19: North American Margins

Subject Group: Structure, Tectonics, Paleostructure

Spec. Pub. Type: Memoir

Pub. Year: 1989

Author(s): H. von der Dick


Geochemical analyses on cuttings and cores of more than 30 wells in the Jeanne d'Arc basin of the Grand Banks identify three formations as petroleum source rocks of significance for regional hydrocarbon generation.

The principal source rock is the Kimmeridgian Egret Formation, a thick sequence of calcareous organic-rich shales deposited under euxinic conditions that were established with the initial breakup of an epeiric basin. Initial rifting formed the semi-silled basin geometry essential for the formation of anoxia. The Previous HitkerogenNext Hit is mainly amorphous-bituminous, and dinoflagellates and bacteria are the primary source materials.

Euxinic conditions and rich source rock formation were terminated with the climax of rifting in the Kimmeridgian, which flooded the basin with coarse clastics and mud. Conditions of source rock formation were extended stratigraphically at the eastern margin of the basin, but the amount of terrigenous material also increased. These conditions resulted in a considerably thicker, but diluted source sequence in the east.

In the late Kimmeridgian the rich source facies was terminated across the basin. Subsequent depositions incorporated a mainly terrestrial Previous HitkerogenNext Hit, which has contributed to hydrocarbon generation in the Kimmeridgian Jeanne d'Arc Shale above the Egret Formation and the Jeanne d'Arc reservoir sands.

The formation of potential petroleum source rocks was reintroduced in the early Tertiary in a now-open marine system. This was the result of high bioproductivity in surface waters and the associated oxygen depletion of midwater zones. However, the oxygen-minimum zone was apparently not effective enough to permanently preserve the oil-prone Previous HitkerogenNext Hit. Although lower Tertiary sediments are high in organic carbon of predominantly marine origin, most of the labile Previous HitkerogenTop is severely degraded by oxidation. However, prolific Tertiary oil source rock may have been preserved in isolated pockets which, upon maturation, generated the Adolphus oil in the center of the basin.

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