Lithospheric structuration onshore-offshore of the Sergipe-Alagoas passive margin, NE Brazil, based on wide-angle seismic data - Université de Bretagne Occidentale Access content directly
Journal Articles Journal of South American Earth Sciences Year : 2018

Lithospheric structuration onshore-offshore of the Sergipe-Alagoas passive margin, NE Brazil, based on wide-angle seismic data

M. Evain
F. Klingelhoefer
A. Loureiro
  • Function : Author
R. Fuck
  • Function : Author
J. Soares
  • Function : Author
Marina Rabineau
M. Benabdellouahed
  • Function : Author
  • PersonId : 965199
I. Rio
  • Function : Author
D. Alves
  • Function : Author
Y. Biari
  • Function : Author
  • PersonId : 969030
C. Corela
  • Function : Author
J. Duarte
  • Function : Author
Z. Mokeddem
  • Function : Author
  • PersonId : 845965
W. Roest

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 an anomalous velocity zone underneath the area.
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Dates and versions

hal-01958592 , version 1 (12-04-2021)

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J.M. Pinheiro, P. Schnürle, M. Evain, A. Afilhado, F. Gallais, et al.. Lithospheric structuration onshore-offshore of the Sergipe-Alagoas passive margin, NE Brazil, based on wide-angle seismic data. Journal of South American Earth Sciences, 2018, 88, pp.649-672. ⟨10.1016/j.jsames.2018.09.015⟩. ⟨hal-01958592⟩
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