Timing of crust formation, deposition of supracrustal sequences, and Transamazonian and Brasiliano metamorphism in the East Pernambuco belt (Borborema Province, NE Brazil): Implications for western Gondwana assembly

2006 ◽  
Vol 149 (3-4) ◽  
pp. 197-216 ◽  
Author(s):  
Sérgio P. Neves ◽  
Olivier Bruguier ◽  
Alain Vauchez ◽  
Delphine Bosch ◽  
José Maurício Rangel da Silva ◽  
...  
2015 ◽  
Vol 28 (3) ◽  
pp. 1183-1196 ◽  
Author(s):  
Ticiano José Saraiva dos Santos ◽  
Wagner da Silva Amaral ◽  
Matheus Fernando Ancelmi ◽  
Michele Zorzetti Pitarello ◽  
Reinhardt Adolfo Fuck ◽  
...  

2020 ◽  
Author(s):  
Fabrício Andrade Caxito ◽  
Camila Franco Basto ◽  
Lauro Cézar Montefalco de Lira Santos ◽  
Elton Luiz Dantas ◽  
Vladimir Cruz de Medeiros ◽  
...  

2021 ◽  
pp. 104283
Author(s):  
Felipe Holanda dos Santos ◽  
Wagner da Silva Amaral ◽  
Kurt Konhauser ◽  
Douglas Teixeira Martins ◽  
Marco Paulo de Castro ◽  
...  

2021 ◽  
Vol 58 (3) ◽  
pp. 568-573
Author(s):  
Juan F. Micheloud ◽  
Lluís Luján ◽  
Luis A. Colque-Caro ◽  
Susana C. Núñez-Montoya ◽  
Claudio G. Barbeito ◽  
...  

Five adult Saanen goats received a single oral dose of Heterophyllaea pustulata containing 42.25 μg/kg rubiadin (anthraquinone) and 3 adult goats were untreated controls. All goats were exposed to sunlight and sequential ear skin biopsies were collected before treatment and at 32 hours, 3 days, 8 days, and 15 days after treatment. Changes at 32 hours after dosing included epidermal spongiosis, single cell death and acantholysis, an increased BAX/BCL-2 protein ratio, and dermal edema. Lesions at day 3 included epidermal and adnexal necrosis, crust formation, and acanthosis. Acanthosis, hyperkeratosis, and dermal fibrosis and neovascularization were present at day 15. The pro-apoptotic (BAX)/anti-apoptotic (BCL-2) protein ratio increased at 32 hours, whereas epidermal and dermal PCNA immunolabeling increased between days 8 and 15 after treatment. The cutaneous lesions were consistent with sunlight-induced damage, and the occurrence in treated but not control goats indicates photosensitization.


2021 ◽  
Vol 11 (1) ◽  
Author(s):  
Carlos E. Ganade ◽  
Roberto F. Weinberg ◽  
Fabricio A. Caxito ◽  
Leonardo B. L. Lopes ◽  
Lucas R. Tesser ◽  
...  

AbstractDispersion and deformation of cratonic fragments within orogens require weakening of the craton margins in a process of decratonization. The orogenic Borborema Province, in NE Brazil, is one of several Brasiliano/Pan-African late Neoproterozoic orogens that led to the amalgamation of Gondwana. A common feature of these orogens is that a period of extension and opening of narrow oceans preceded inversion and collision. For the case of the Borborema Province, the São Francisco Craton was pulled away from its other half, the Benino-Nigerian Shield, during an intermittent extension event between 1.0–0.92 and 0.9–0.82 Ga. This was followed by inversion of an embryonic and confined oceanic basin at ca. 0.60 Ga and transpressional orogeny from ca. 0.59 Ga onwards. Here we investigate the boundary region between the north São Francisco Craton and the Borborema Province and demonstrate how cratonic blocks became physically involved in the orogeny. We combine these results with a wide compilation of U–Pb and Nd-isotopic model ages to show that the Borborema Province consists of up to 65% of strongly sheared ancient rocks affiliated with the São Francisco/Benino-Nigerian Craton, separated by major transcurrent shear zones, with only ≈ 15% addition of juvenile material during the Neoproterozoic orogeny. This evolution is repeated across a number of Brasiliano/Pan-African orogens, with significant local variations, and indicate that extension weakened cratonic regions in a process of decratonization that prepared them for involvement in the orogenies, that led to the amalgamation of Gondwana.


2017 ◽  
Vol 297 ◽  
pp. 56-76 ◽  
Author(s):  
Nicholas J. Gardiner ◽  
Arthur H. Hickman ◽  
Christopher L. Kirkland ◽  
Yongjun Lu ◽  
Tim Johnson ◽  
...  

1998 ◽  
Vol 75 (5) ◽  
pp. 581-584 ◽  
Author(s):  
D'Anne Hayman ◽  
R. C. Hoseney ◽  
J. M. Faubion

Sign in / Sign up

Export Citation Format

Share Document