South Atlantic divergent margin evolution: rift-border uplift and salt tectonics in the basins of SE Brazil

W. Mohriak; M. Nemčok; G. Enciso

doi:10.1144/sp294.19

journal article Jan 01, 2008

South Atlantic divergent margin evolution: rift-border uplift and salt tectonics in the basins of SE Brazil

W. Mohriak M. Nemčok G. Enciso

Geological Society, London, Special Publications Vol. 294 No. 1 pp. 365-398 · Geological Society of London

View at Publisher Save 10.1144/sp294.19

Abstract

Abstract
The South Atlantic Ocean evolved after rupture of the São Francisco–Congo–Rio de la Plata–Kalahari cratonic landmass and the Late Proterozoic fold belts. Break-up in the South Atlantic realm developed diachronously: rifting started in the south (Argentina) during the Jurassic and progressed towards the equatorial segment. The central portion was controlled by a rift-resistant cratonic nucleus (the São Francisco–Congo craton) and as a result underwent development of narrow basins; parts controlled by Neoproterozoic fold belts developed wide basins. The final break-up of western Gondwana and the onset of plate divergence were marked by thick wedges of seaward-dipping reflectors, located near the incipient ocean-ridge spreading centre that had already been formed by the time Aptian evaporites were deposited. Subsequently, a few episodes of intraplate tectonic and magmatic activity affected the Santos, Campos and Espírito Santo basins.
Post-break up development of the offshore basins was affected by gravity gliding over the Aptian evaporites. Continental uplift may be invoked as the main cause of salt mobilization, generating prograding clastic wedges that thickened basin-wards and produced a loading effect on the salt basin. Coupled with onshore erosional unloading and the effects of the gravity gliding, this probably resulted in further flexural uplift of the continental margin.

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Details

Published: Jan 01, 2008
Vol/Issue: 294(1)
Pages: 365-398
License: View

Authors

W

W. Mohriak

Petroleo Brasileiro S.A.–UN-EXP–GP-SSE, Avda. Chile, 65–s. 1302 20.035-900 Rio de Janeiro, RJ, Brazil (email: )

M

M. Nemčok

Energy & Geoscience Institute, 423 Wakara Way, Suite 300, Salt Lake City, UT 84108, USA

G

G. Enciso

Spinnaker Exploration, 1200 Smith Street, Suite 800, Houston, TX 77002, USA

Cite This Article

W. Mohriak, M. Nemčok, G. Enciso (2008). South Atlantic divergent margin evolution: rift-border uplift and salt tectonics in the basins of SE Brazil. Geological Society, London, Special Publications, 294(1), 365-398. https://doi.org/10.1144/sp294.19

South Atlantic divergent margin evolution: rift-border uplift and salt tectonics in the basins of SE Brazil

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