Lithospheric structuration onshore-offshore of the Sergipe-Alagoas passive margin, NE Brazil, based on wide-angle seismic data. (December 2018)
- Record Type:
- Journal Article
- Title:
- Lithospheric structuration onshore-offshore of the Sergipe-Alagoas passive margin, NE Brazil, based on wide-angle seismic data. (December 2018)
- Main Title:
- Lithospheric structuration onshore-offshore of the Sergipe-Alagoas passive margin, NE Brazil, based on wide-angle seismic data
- Authors:
- Morvan, L.
Mazé, J.P.
Pierre, D.
Roudaut-Pitel, M.
Rio, I.
Alves, D.
Barros Junior, P.
Biari, Y.
Corela, C.
Crozon, J.
Duarte, J.L.
Ducatel, C.
Falcão, C.
Fernagu, P.
Le Piver, D.
Mokeddem, Z.
Pelleau, P.
Rigoti, C.
Roest, W.
Roudaut, M.
Pinheiro, J.M.
Schnurle, P.
Evain, M.
Afilhado, A.
Gallais, F.
Klingelhoefer, F.
Loureiro, A.
Fuck, R.
Soares, J.
Cupertino, J.A.
Viana, A.
Rabineau, M.
Baltzer, A.
Benabdellouahed, M.
Dias, N.
Moulin, M.
Aslanian, D.
… (more) - Abstract:
- Abstract: The structure and nature of the crust underlying the Camamu-Almada-Jequitinhonha-Sergipe-Alagoas basins System, in the NE Brazilian margin, were investigated based on the interpretation of 12 wide-angle seismic profiles acquired during the SALSA (Sergipe ALagoas Seismic Acquisition) experiment in 2014. In this work, we present two 220-km-long NW-SE combined wide-angle and reflection seismic profiles, SL 01 and SL 02, that have been acquired using 15 ocean-bottom-seismometers along each profile, offshore the southern part of the Sergipe Alagoas Basin (SAB), north of the Vaza-Barris Transfer zone. The SL 02 has a 150-km long inland continuation with 20 land-seismic-stations until the Sergipano Fold Belt (SFB). Wide-angle seismic forward modeling allows us to precisely divide the crust in three domains: beneath the continental shelf, a ∼100 km wide necking zone is imaged where the continental crust thins from ∼35 km on the Unthinned Continental Domain, which displays a three-layered crust structure, to less than 8 km on the Oceanic Crust Domain. In the necking zone, the upper and the middle layers thin dramatically and almost disappear, while the Moho discontinuity shows clear PmPs. The Continental-Oceanic Crust Boundary (COB) is located at ∼80 km from the coastline and is marked by intracrustal seismic reflectors and changes in the seismic velocity, showing a sharp transition. On profile SL02, the oceanic crust is perturbed by a volcanic edifice together with anAbstract: The structure and nature of the crust underlying the Camamu-Almada-Jequitinhonha-Sergipe-Alagoas basins System, in the NE Brazilian margin, were investigated based on the interpretation of 12 wide-angle seismic profiles acquired during the SALSA (Sergipe ALagoas Seismic Acquisition) experiment in 2014. In this work, we present two 220-km-long NW-SE combined wide-angle and reflection seismic profiles, SL 01 and SL 02, that have been acquired using 15 ocean-bottom-seismometers along each profile, offshore the southern part of the Sergipe Alagoas Basin (SAB), north of the Vaza-Barris Transfer zone. The SL 02 has a 150-km long inland continuation with 20 land-seismic-stations until the Sergipano Fold Belt (SFB). Wide-angle seismic forward modeling allows us to precisely divide the crust in three domains: beneath the continental shelf, a ∼100 km wide necking zone is imaged where the continental crust thins from ∼35 km on the Unthinned Continental Domain, which displays a three-layered crust structure, to less than 8 km on the Oceanic Crust Domain. In the necking zone, the upper and the middle layers thin dramatically and almost disappear, while the Moho discontinuity shows clear PmPs. The Continental-Oceanic Crust Boundary (COB) is located at ∼80 km from the coastline and is marked by intracrustal seismic reflectors and changes in the seismic velocity, showing a sharp transition. On profile SL02, the oceanic crust is perturbed by a volcanic edifice together with an anomalous velocity zone underneath the area. Highlights: Sergipe Alagoas Basin passive margin modeling. Wide-angle refraction seismic integrated with Multi-Channel reflection seismic data. Location of the Continental- Oceanic crust boundary. Lithospheric structuration and segmentation of Brazil's margin in Central Atlantic. … (more)
- Is Part Of:
- Journal of South American earth sciences. Volume 88(2018)
- Journal:
- Journal of South American earth sciences
- Issue:
- Volume 88(2018)
- Issue Display:
- Volume 88, Issue 2018 (2018)
- Year:
- 2018
- Volume:
- 88
- Issue:
- 2018
- Issue Sort Value:
- 2018-0088-2018-0000
- Page Start:
- 649
- Page End:
- 672
- Publication Date:
- 2018-12
- Subjects:
- South Atlantic ocean -- NE Brazil -- Sergipe-Alagoas basin -- Passive margins -- Wide-angle refraction seismics -- Crustal structure -- Tectonic inheritance
Geology -- Latin America -- Periodicals
Earth sciences -- Latin America -- Periodicals
Geology -- Antarctica -- Periodicals
Earth sciences -- Antarctica -- Periodicals
Geology -- Caribbean Area -- Periodicals
Earth sciences -- Caribbean Area -- Periodicals
Géologie -- Amérique latine -- Périodiques
Sciences de la terre -- Amérique latine -- Périodiques
Géologie -- Antarctique -- Périodiques
Sciences de la terre -- Antarctique -- Périodiques
Géologie -- Caraïbes (Région) -- Périodiques
Sciences de la terre -- Caraïbes (Région) -- Périodiques
Earth sciences
Geology
Antarctica
Caribbean Area
Latin America
Periodicals
550.5 - Journal URLs:
- http://www.sciencedirect.com/science/journal/08959811 ↗
http://www.elsevier.com/journals ↗ - DOI:
- 10.1016/j.jsames.2018.09.015 ↗
- Languages:
- English
- ISSNs:
- 0895-9811
- Deposit Type:
- Legaldeposit
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