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The Late Cretaceous tectonic evolution of the South China Sea area: An overview, and new perspectives from 3D seismic reflection data
Abstract The Late Cretaceous is a significant geologic period in the South China Sea area,
as it marks the tectonic transition from the early Paleo-Pacific Plate subduction to the …
as it marks the tectonic transition from the early Paleo-Pacific Plate subduction to the …
Post-rift faulting controlled by different geodynamics in the Pearl River Mouth Basin, northern South China Sea margin
Abstract The South China Sea (SCS), located at the junction of the Eurasian Plate, the
Philippine Sea Plate and the Indo-Australian Plate, developed as the result of intra …
Philippine Sea Plate and the Indo-Australian Plate, developed as the result of intra …
Postrift stress field inversion in the Potiguar Basin, Brazil–Implications for petroleum systems and evolution of the equatorial margin of South America
Rifting and related normal stress regime in the equatorial continental margin of Brazil
ceased during the Late Cretaceous, when the stress regimes in eastern South America and …
ceased during the Late Cretaceous, when the stress regimes in eastern South America and …
Fault damage zones width: Implications for the tectonic evolution of the northern border of the Araripe Basin, Brazil, NE Brazil
Fault zones commonly have spatially variable fault rocks and brittle structures. Differing fault-
rock attributes may retard or increase cross-and along-fault permeability. Our work analyzed …
rock attributes may retard or increase cross-and along-fault permeability. Our work analyzed …
Transtensional tectonics during the Gondwana breakup in northeastern Brazil: Early Cretaceous paleostress inversion in the Araripe Basin
Intraplate deformation during the Mesozoic breakup of West Gondwana predominantly
occurred along major ancient lithospheric discontinuities. The Precambrian Patos Shear …
occurred along major ancient lithospheric discontinuities. The Precambrian Patos Shear …
Tectonic inversion assessed by integration of geological and geophysical data: The intracontinental Rio do Peixe Basin, NE Brazil
Common basin models assume that the post‐rift tectonic evolution of most basins is usually
associated with tectonic quiescence. However, tectonic inversion during the post‐rift phase …
associated with tectonic quiescence. However, tectonic inversion during the post‐rift phase …
Review of tectonic inversion of sedimentary basins in NE and N Brazil: analysis of mechanisms, timing and effects on structures and relief
Most intraplate areas worldwide are under compression characterized by thrust and strike-
slip deformations. The sources of the stresses in these regions are a combination of far-field …
slip deformations. The sources of the stresses in these regions are a combination of far-field …
Relations between inherited basement fabric and fault nucleation in a continental setting: The Rio do Peixe Basin, NE Brazil
The control of normal fault growth by preexisting basement structures is still a worldwide
matter of debate. The objectives of the present study are (i) to investigate where rift faults …
matter of debate. The objectives of the present study are (i) to investigate where rift faults …
An integrated structural and magnetic fabric study to constrain the progressive extensional tectonics of the Rio do Peixe Basin, Brazil
We constrained the tectonic evolution of the intracratonic Cretaceous Rio do Peixe Basin
(RPB) in NE Brazil, combining structural and Anisotropy of Magnetic Susceptibility (AMS) …
(RPB) in NE Brazil, combining structural and Anisotropy of Magnetic Susceptibility (AMS) …
[HTML][HTML] Variation of thickness, internal structure and petrophysical properties in a deformation band fault zone in siliciclastic rocks
We studied the geometry and petrophysical properties of fault core and damage zones of a
deformation band fault zone in the arkosic sandstones of the Cretaceous Antenor Navarro …
deformation band fault zone in the arkosic sandstones of the Cretaceous Antenor Navarro …