Results 11 to 20 of about 62 (50)
Abstract 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) data. We analyzed the structural features of four sites along two major faults bordering the basin, the NE‐striking Portalegre Fault and the E‐W‐striking Malta Fault ...
M. A. Nicchio +7 more
wiley +1 more source
Abstract Pre‐existing crustal structures are known to influence rifting, but the factors controlling their influence remain poorly understood. We present results of digital image correlation that allows for the surface strain analysis of a series of analog rifting experiments designed to test the influence of the size, orientation, depth, and geometry ...
Edoseghe E. Osagiede +5 more
wiley +1 more source
In the Bom Jardim de Goiás region, the Transbrasiliano Lineament shows evidence of a fault reactivation along NE-SW structures (main direction) and secondary directions related to subsequent events.
Alexandre Messias Reis +2 more
doaj +1 more source
Abstract We present a new P‐wave seismic tomographic model for the region of the Paraná Basin and surroundings using a multiple‐frequency approach, providing better resolution than previous regional studies. We processed a total of 62,692 cross‐correlation delays for P, PKIKP, PcP, and PP phases distributed among 1,081 events using six different ...
G. M. P. C. Affonso +8 more
wiley +1 more source
ERRATA Revista: Geologia USP – Série Científica, V. 15 n. 2, p. 57 (referências) Curto, J. B., Vidotti, R. M., Fuck, R. A. R., Blakely, J., Alvarenga, C. J. S., Dantas, E. L. (2014).
Editor Editor
doaj +1 more source
The 2009 earthquake, magnitude mb 4.8, in the Pantanal Wetlands, west-central Brazil
The main goal of this paper is to characterize the Coxim earthquake occurred in June 15th, 2009 in the Pantanal Basin and to discuss the relationship between its faulting mechanism with the Transbrasiliano Lineament.
FÁBIO L. DIAS +6 more
doaj +1 more source
ABSTRACT. The Transbrasiliano Lineament (TBL) corresponds to a NE-trending mega shear zone of late Neoproterozoic age with an extensive segment underneath the Parnaíba Basin (northeastern Brazil); the Eopaleozoic to Mesozoic section of the basin evidence the lineament’s brittle reactivation events.
Thuany Patrícia Costa de Lima +4 more
openaire +2 more sources
This work analyses morphostructural aspects and their influence on the development of the karst relief of Serra da Capivara (State of Piauí, northeastern Brazil).
Mickaelle Braga da Silva +1 more
doaj +1 more source
Gamma-ray spectrometric responses of Archean rocks were studied in order to define a characteristic signature for these rocks. As the half-life of the most frequent Thorium isotope (232Th – half life of 14.05 Ga) is more than 3 times longer relative to ...
Marcus Flavio Nogueira Chiarini +9 more
doaj +1 more source
Ductile Extrusion Triggered by Continental Collision in NE Brazil
ABSTRACT The Borborema Province in northeastern Brazil hosts one of the world's largest strike‐slip shear zone networks, active during the late Neoproterozoic assembly of West Gondwana. Whether these shear zones initiated during active continental collision or as a post‐orogenic response to far‐field stresses remains debated.
L. R. Tesser +6 more
wiley +1 more source

