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A tectono-stratigraphic review of continental breakup on intraplate continental margins and its impact on resultant hydrocarbon systems
Abstract Intraplate Continental Margins comprise fully rifted areas of continents and cratons
recording the tectonic events associated with plate breakup and subsequent continental …
recording the tectonic events associated with plate breakup and subsequent continental …
Where does a continent prefer to break up? Some lessons from the South Atlantic margins
The localization of Gondwana rifting, break-up and subsequent opening of the South Atlantic
basin appears to have been primarily controlled by inherited zones of lithospheric …
basin appears to have been primarily controlled by inherited zones of lithospheric …
The chronology and tectonic style of landscape evolution along the elevated Atlantic continental margin of South Africa resolved by joint apatite fission track and (U‐Th …
Atlantic‐type continental margins have long been considered “passive” tectonic settings
throughout the entire postrift phase. Recent studies question the long‐term stability of these …
throughout the entire postrift phase. Recent studies question the long‐term stability of these …
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 …
[HTML][HTML] Post break-up tectonic inversion across the southwestern cape of South Africa: New insights from apatite and zircon fission track thermochronometry
The south-west African margin is regarded as an example of a passive continental margin
formed by continental rifting following a phase of lithospheric extension and thinning. Recent …
formed by continental rifting following a phase of lithospheric extension and thinning. Recent …
Architectural rift geometry of the Rio do Peixe Basin (Brazil): implications for its tectonic evolution and Precambrian heritage
Preexisting shear zones in the basement may influence the formation of normal faults in rift
environments. However, the specific role and interaction between these preexisting shear …
environments. However, the specific role and interaction between these preexisting shear …
Differential Phanerozoic evolution of cratonic and non-cratonic lithosphere from a thermochronological perspective: São Francisco Craton and marginal orogens …
ACL Fonseca, TA Novo, S Nachtergaele… - Gondwana …, 2021 - Elsevier
The São Francisco Craton (SFC) and its marginal Araçuaí and Brasília orogens exhibit a
significant diversity in their lithospheric architecture. These orogens were shaped during the …
significant diversity in their lithospheric architecture. These orogens were shaped during the …
[HTML][HTML] New insights from low-temperature thermochronology into the tectonic and geomorphologic evolution of the south-eastern Brazilian highlands and passive …
G Van Ranst, AC Pedrosa-Soares, T Novo… - Geoscience …, 2020 - Elsevier
Abstract The South Atlantic passive margin along the south-eastern Brazilian highlands
exhibits a complex landscape, including a northern inselberg area and a southern elevated …
exhibits a complex landscape, including a northern inselberg area and a southern elevated …
Depicting past stress history at passive margins: A combination of calcite twinning and stylolite roughness paleopiezometry in supra-salt Sendji deep carbonates …
The paleostress history and associated deformation mechanisms affecting passive margins
are seldom studied, as access to offshore parts is rather limited. We analyze an offshore …
are seldom studied, as access to offshore parts is rather limited. We analyze an offshore …
Correlation between tectonic stress regimes and methane seepage on the western Svalbard margin
A Plaza-Faverola, M Keiding - Solid earth, 2019 - se.copernicus.org
Methane seepage occurs across the western Svalbard margin at water depths ranging
from< 300 m, landward from the shelf break, to> 1000 m in regions just a few kilometres from …
from< 300 m, landward from the shelf break, to> 1000 m in regions just a few kilometres from …