Bibliografías temáticas / Abrolhos magmatism

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Literatura académica sobre el tema "Abrolhos magmatism"

Autor: Grafiati
Publicado: 4 de junio de 2021
Última modificación: 7 de febrero de 2022

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Artículos de revistas sobre el tema "Abrolhos magmatism"

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Oliveira, Leonardo Costa de, Renata Marins Alvim Gama de Oliveira, and Egberto Pereira. "Seismic characteristics of the onshore Abrolhos magmatism, East-Brazilian continental margin." Marine and Petroleum Geology 89 (January 2018): 488–99. http://dx.doi.org/10.1016/j.marpetgeo.2017.10.016.

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Ferreira, Talles Souza, Mario Neto Cavalcanti de Araújo, and Fernando César Alves da Silva. "Cenozoic folding in the Cumuruxatiba basin, Brazil: An approach to the deformation trigger by the Abrolhos magmatism." Marine and Petroleum Geology 54 (June 2014): 47–64. http://dx.doi.org/10.1016/j.marpetgeo.2014.02.012.

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FODAR, R. V., S. B. MUKASA, C. B. GOMES, and U. G. CORDANI. "Ti-rich Eocene Basaltic Rocks, Abrolhos Platform, Offshore Brazil, 18 S: Petrology with Respect to South Atlantic Magmatism." Journal of Petrology 30, no. 3 (1989): 763–86. http://dx.doi.org/10.1093/petrology/30.3.763.

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Stanton, Natasha, Andres Gordon, Cassia Cardozo, and Nick Kusznir. "Morphostructure, emplacement and duration of the Abrolhos Magmatic Province: A geophysical analysis of the largest post-breakup magmatism of the South-Eastern Brazilian margin." Marine and Petroleum Geology 133 (November 2021): 105230. http://dx.doi.org/10.1016/j.marpetgeo.2021.105230.

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Adriano, Leandro B., Paulo T. L. Menezes, Manuela S. Adriano, et al. "Jequitinhonha Basin: Structural aspects, relationship with igneous activity, and hydrocarbon exudations." Interpretation 6, no. 1 (2018): T51—T60. http://dx.doi.org/10.1190/int-2017-0120.1.

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The Jequitinhonha Basin (JB) is one of the sedimentary basins in the Brazilian Eastern Margin. Although several regional studies have been conducted to define its tectonic framework and petroleum system, neither one is very well-understood. For instance, the extent and influence of the volcanic rocks in the petroleum system of the JB are still matters of debate among geoscientists. We found a new integrated interpretation for the structural framework of JB in which we discover the major faults, the mapped volcanics, and a new basement map. Finally, we evaluate the correlation of known exudatio
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Lockwood, A. M., and C. D’Ercole. "THE EVOLUTION OF THE BERNIER RIDGE, SOUTHERN CARNARVON BASIN, WESTERN AUSTRALIA:IMPLICATIONS FOR PETROLEUM PROSPECTIVITY." APPEA Journal 44, no. 1 (2004): 241. http://dx.doi.org/10.1071/aj03009.

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The basement topography of the Gascoyne Platform and adjoining areas in the Southern Carnarvon Basin was investigated using satellite gravity and seismic data, assisted by a depth to crystalline basement map derived from modelling the isostatic residual gravity anomaly. The resulting enhanced view of the basement topography reveals that the Gascoyne Platform extends further westward than previously indicated, and is bounded by a northerly trending ridge of shallow basement, named the Bernier Ridge.The Bernier Ridge is a product of rift-flank uplift prior to the Valanginian breakup of Gondwana,
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Tesis sobre el tema "Abrolhos magmatism"

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Arena, Michele Correia. "Petrologia da sucessão magmática do Arquipélago de Abrolhos." Universidade do Estado do Rio de Janeiro, 2008. http://www.bdtd.uerj.br/tde_busca/arquivo.php?codArquivo=722.

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A Sucessão Magmática do Arquipélago de Abrolhos é composta por quatro unidades, quais sejam: Olivina-Plagioclásio Basalto (b1), Piroxênio-Plagioclásio-Olivina Basalto (b2), Piroxênio-Plagioclásio Basalto (b3) e Cumulado (b4). As unidades não são correlacionáveis litoestratigraficamente e estão empilhadas da base para o topo em unidade b1, b2, b3 e b4. As unidades da sucessão magmática são diferentes quanto à textura, estrutura e mineralogia. A análise litogeoquímica de vinte e três amostras de rochas basálticas das unidades da sucessão magmática discriminou uma série transicional de afinidade
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Ferreira, Talles Souza. "An?lise estrutural da deforma??o cenoz?ica na Bacia de Cumuruxatiba (BA)." Universidade Federal do Rio Grande do Norte, 2010. http://repositorio.ufrn.br:8080/jspui/handle/123456789/18810.

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Made available in DSpace on 2015-03-13T17:08:29Z (GMT). No. of bitstreams: 1 TallesSF_DISSERT_1-74.pdf: 3503129 bytes, checksum: 43d4d5f0a963aecc3dec332abad3bc2d (MD5) Previous issue date: 2010-09-03<br>The Cumuruxatiba basin is located at the southern coast State of Bahia in northeastern of Brazil. This basin was formed in distensional context, with rifting and subsequent thermal phase during Neocomian to late Cretaceous. At Cenozoic ages, the Abrolhos magmatism occurs in the basin with peaks during the Paleocene and Eocene. In this period, there was a kinematic inversion in the basi
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