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

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Hydrocarbon Traps<br />

Structural traps <strong>in</strong> the <strong>Jeanne</strong> d’Arc d<br />

Bas<strong>in</strong> are associated with<br />

rift<strong>in</strong>g of the Newfoundland Marg<strong>in</strong>, subsidence and <strong>for</strong>mation<br />

of the deep extensional bas<strong>in</strong> and movement of the Argo salt<br />

•The ma<strong>in</strong> structural traps are extensional anticl<strong>in</strong>es, roll-overs, overs, faulted<br />

anticl<strong>in</strong>es, faulted and tilted blocks and elongated horsts<br />

• Numerous salt <strong>in</strong>duced structures such as pillows, domes, diapirs,<br />

ridges, allochthonous teardrops and turtle anticl<strong>in</strong>es are common<br />

•The great majority of faults are listric normal faults, but some transfer<br />

faults, accommodation zones and local <strong>in</strong>versions due to transtension<br />

sion<br />

and halok<strong>in</strong>esis are also <strong>for</strong>m<strong>in</strong>g traps<br />

•Most of the discovered fields have a stratigraphic trapp<strong>in</strong>g component<br />

onent<br />

• Stratigraphic traps are widespread. Paleo-valleys, bas<strong>in</strong> marg<strong>in</strong> and<br />

bas<strong>in</strong> floor fans are abundant <strong>in</strong> the bas<strong>in</strong> and conta<strong>in</strong> some discovered<br />

resources<br />

Enachescu, NL DNR 2009

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