Zobrazeno 1 - 10
of 29
pro vyhledávání: '"Carlos Eduardo Ganade"'
Autor:
Fabrício de Andrade Caxito, Lauro Cézar Montefalco de Lira Santos, Carlos Eduardo Ganade, Abderrahmane Bendaoud, El-Hocine Fettous, Merlain Houketchang Bouyo
Publikováno v:
Brazilian Journal of Geology, Vol 50, Iss 2 (2020)
Abstract Both the Borborema Province of NE Brazil and the geological provinces of NW Africa (the Trans-Saharan Orogen consisted of the Tuareg and Benino-Nigerian shields and the Central African Orogen of Cameroon, Chad, and Central African Republic)
Externí odkaz:
https://doaj.org/article/7d2517599d454cc19c7eba41595b6efd
Autor:
Felipe Grandjean da Costa, Carlos Eduardo Ganade de Araújo, Wagner da Silva Amaral, Antonio Maurilio Vasconcelos, Joseneusa Brilhante Rodrigues
Publikováno v:
Geologia USP. Série Científica, Vol 13, Iss 2, Pp 159-174 (2013)
The Tamboril-Santa Quitéria Complex (TSQC) is one of the largest Neoproterozoic plutonic manifestations in the northBorborema Province (NE Brazil). It represents an anatectic/igneous association characterized by a number of magmaticpulses that occur
Externí odkaz:
https://doaj.org/article/58a55af99bd74ee09e76e714c219e0cb
Autor:
Felipe Grandjean da Costa, Carlos Eduardo Ganade de Araújo, Wagner da Silva Amaral, Antonio Maurilio Vasconcelos, Joseneusa Brilhante Rodrigues
Publikováno v:
Geologia USP. Série Científica, Vol 13, Iss 2 (2013)
O Complexo Tamboril Santa-Quitéria (CTSQ) é uma das maiores manifestações plutônicas do Neoproterozoico na porção norte da Província Borborema (NE Brasil). Corresponde a uma associação granito-migmatítica envolvendo granitoides diversos no
Externí odkaz:
https://doaj.org/article/5036ce85509a4865b642374ae32d13fe
Publikováno v:
Biblioteca Digital de Teses e Dissertações da USPUniversidade de São PauloUSP.
O Orógeno Gondwana Oeste (OGO), sugerido nesta Tese, é uma faixa linear que se estende por mais de 5000 km do atual noroeste da África ao Brasil Central. Perspectivas modernas e tradicionais sugerem que este Orógeno resultou do consumo e fechamen
Autor:
Juliana Fernandes Bonifacio, Carlos Eduardo Ganade, Anderson Costa dos Santos, Ricardo Ivan Ferreira da Trindade
Publikováno v:
Earth-Science Reviews. 238:104333
Autor:
Lynthener B. Takenaka, William Griffin, Suzanne Yvette O'Reilly, Miguel Basei, Carlos Eduardo Ganade, Dorrit E. Jacob
Publikováno v:
Goldschmidt Abstracts.
Autor:
Érico Natal Pedro Zacchi, José Affonso Brod, Carlos Eduardo Ganade de Araujo, Ítalo Lopes de Oliveira, Cimara Francisca Monteiro, Elton Luiz Dantas, Reinhardt A. Fuck
Publikováno v:
Precambrian Research. 351:105963
The first occurrence of Mesoproterozoic carbonatite in the Rio de la Plata Craton – RDPC indicates extensional event prior to the opening of the Charrua Ocean. Nd-Sr-Hf Isotopic and U-Pb on zircon geochronological data are presented for the Tres Es
Autor:
Hartwig E. Frimmel, Miguel Angelo Stipp Basei, Mario da Costa Campos Neto, Neivaldo Araújo de Castro, Claudia Regina Passarelli, Carlos Eduardo Ganade de Araujo
Publikováno v:
Regional Geology Reviews ISBN: 9783319689197
Closure of the southern Adamastor Ocean led to the development of the Neoproterozoic-Early Cambrian orogens on both margins of the present South Atlantic Ocean, which preserve a rich record of West Gondwana assembly and large-scale crustal evolution.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::dfd428ee2a76d92be5b80002f78eef55
https://doi.org/10.1007/978-3-319-68920-3_3
https://doi.org/10.1007/978-3-319-68920-3_3
Publikováno v:
Terra Nova. 26:157-168
We propose that the development of the Borborema Province from 620 to 570 Ma resulted from two discrete collisional events. Collision I, along the West Gondwana Orogen on the west side of the Province, took place at c. 620–610 Ma as the result of c
Autor:
Joseneusa Brilhante Rodrigues, Wagner da Silva Amaral, Carlos Eduardo Ganade de Araujo, Felipe Grandjean da Costa, Antônio Maurílio Vasconcelos
Publikováno v:
Geologia USP. Série Científica, Vol 13, Iss 2, Pp 159-174 (2013)
The Tamboril-Santa Quiteria Complex (TSQC) is one of the largest Neoproterozoic plutonic manifestations in the north Borborema Province (NE Brazil). It represents an anatectic/igneous association characterized by a number of magmatic pulses that occu