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Adriano Viana

Petrobras

Av Chile, 65, room 401

Rio de Janeiro, 20031-912

Brazil

SCHOLARLY PAPERS

3

DOWNLOADS

266

TOTAL CITATIONS

0

Scholarly Papers (3)

1.

Neogene Isolated Carbonate Platform of the Rio Grande Rise (Southwest Atlantic Ocean)

Number of pages: 67 Posted: 21 May 2024
affiliation not provided to SSRN, affiliation not provided to SSRN, Universidade do Vale do Rio dos Sinos, affiliation not provided to SSRN, affiliation not provided to SSRN, affiliation not provided to SSRN, affiliation not provided to SSRN, Geological Survey of Brazil, Geological Survey of Brazil, affiliation not provided to SSRN, affiliation not provided to SSRN and Petrobras
Downloads 119 (600,462)

Abstract:

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Southwest-Atlantic, Rio-Grande-Rise, Isolated-carbonate-platform, Microfacies

2.

Imaging Exhumed Continental and Proto-Oceanic Crusts in the Camamu Triple Junction, Brazil

Number of pages: 29 Posted: 15 Feb 2023
affiliation not provided to SSRN, affiliation not provided to SSRN, IFREMER, IFREMER, affiliation not provided to SSRN, IFREMER, IFREMER, Federal University of Santa Catarina (UFSC), Universidade de Brasília (UnB), Universidade de Brasília (UnB), Petrobras, Petrobras, affiliation not provided to SSRN, IFREMER, IFREMER and affiliation not provided to SSRN
Downloads 86 (765,566)

Abstract:

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NE Brazil, South Atlantic Ocean, Passive margins, Camamu triple point, Wide-angle refraction seismic, PSDM, Crustal structure, Cretaceous breakup, exhumed lower continental crust, SALSA

3.

From São Francisco Craton to Jacuipe Basin, Passing Trough the South Tucano and Recôncavo Grabens: New Insights from Wide-Angle-Mcs Data

Number of pages: 34 Posted: 03 Apr 2023
IFREMER, affiliation not provided to SSRN, affiliation not provided to SSRN, IFREMER, Federal University of Santa Catarina (UFSC), affiliation not provided to SSRN, affiliation not provided to SSRN, affiliation not provided to SSRN, Petrobras, Petrobras and IFREMER
Downloads 61 (951,658)

Abstract:

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Wide-angle-MCS data, Brazilian Margins, Tucano graben, lower continental crust, Passive margin evolution