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Petroleum Exploration Opportunities in Jeanne d'Arc Basin , Call for ...

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4. Geology Summary of the <strong>Jeanne</strong><br />

d’Arc Bas<strong>in</strong><br />

• <strong>Jeanne</strong> d’Arc d<br />

Bas<strong>in</strong> and adjacent Central Ridge area host most of the<br />

significant oil discoveries <strong>in</strong> the Newfoundland and Labrador<br />

offshore area (there are also major gas discoveries off Labrador and<br />

an oil discovery <strong>in</strong> Flemish Pass Bas<strong>in</strong>), <strong>in</strong>clud<strong>in</strong>g the three currently<br />

rently<br />

produc<strong>in</strong>g fields; also Hebron and a series of satellites and field<br />

extensions which are now developed or planned <strong>for</strong> development<br />

• The bas<strong>in</strong> <strong>for</strong>ms an elongate, roughly NE trend<strong>in</strong>g, large half-graben,<br />

encompass<strong>in</strong>g an area of about 14,000 km 2 . It is bounded to the west<br />

by the Murre Fault, to the north by the Cumberland Belt Transfer<br />

Zone (CBTZ) l<strong>in</strong>eament, to the east by the Voyager Fault and to the t<br />

south by the Egret Fault. The bas<strong>in</strong> deepens to the north and shallows<br />

to the south, and conta<strong>in</strong>s over 20 km of Upper Triassic to Cenozoic<br />

oic<br />

sedimentary <strong>in</strong>fill <strong>in</strong> its depocentre, , situated to the north of the Trans-<br />

Bas<strong>in</strong> Fault Zone (TBFZ) and east of Hibernia<br />

• The sedimentary fill of this area was deposited, structured and<br />

fragmented dur<strong>in</strong>g repeated extensional episodes. Infill <strong>in</strong>cludes<br />

clastics, salt and carbonates. M<strong>in</strong>or trans-tensional tensional tectonic<br />

movements and several strong erosional <strong>in</strong>terludes have also reshaped<br />

the bas<strong>in</strong> and its associated ridges<br />

Enachescu, NL DNR 2009

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