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

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<strong>Petroleum</strong> Geology<br />

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

Bas<strong>in</strong> is a hydrocarbon prolific bas<strong>in</strong> that conta<strong>in</strong>s<br />

almost exclusively all the oil volumes discovered offshore<br />

Newfoundland<br />

• The bas<strong>in</strong>’s s <strong>in</strong>fill conta<strong>in</strong>s structured synrift rock successions<br />

(<strong>in</strong>cludes evaporites, carbonates and coarse and f<strong>in</strong>e clastics)<br />

rang<strong>in</strong>g <strong>in</strong> age from Late Triassic to late Early - Cretaceous<br />

(Extensional Stage sedimentary sequence)<br />

• Oil prone source rocks are present <strong>in</strong> Late Jurassic (<strong>Call</strong>ovian(<br />

<strong>Call</strong>ovian,<br />

Ox<strong>for</strong>dian and especially Kimmeridgian); the potential <strong>for</strong> other<br />

source rocks is recognized with<strong>in</strong> the Early and Late Cretaceous<br />

and Early Tertiary<br />

• The early sedimentary fill conta<strong>in</strong>s the Argo Salt that later<br />

became mobile and created salt <strong>in</strong>duced structures <strong>in</strong> the<br />

overly<strong>in</strong>g sediments (e.g. White Rose Diapir, , Amethyst Ridge)<br />

(Enachescu et al., 2000)<br />

• Post rift sedimentary sequence is represented by parallel, slightly<br />

de<strong>for</strong>med sedimentary layers (ma<strong>in</strong>ly f<strong>in</strong>e clastics and th<strong>in</strong> chalk<br />

and carbonates)<br />

Enachescu&Foote/NLDNR 2009

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