Zobrazeno 1 - 10
of 17
pro vyhledávání: '"Carlos Eduardo Ganade de Araujo"'
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:
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
Autor:
Reinhardt A. Fuck, Vicente Antonio Vitorio Girardi, Miguel Angelo Stipp Basei, Carlos Eduardo Ganade de Araujo, Umberto G. Cordani, Márcio Martins Pimentel
Publikováno v:
Repositório Institucional da USP (Biblioteca Digital da Produção Intelectual)
Universidade de São Paulo (USP)
instacron:USP
Universidade de São Paulo (USP)
instacron:USP
Previous studies have proposed that a major suture resulted from the collision between the Amazonian and Sao Francisco-Congo cratons during the Cambrian, following the closure of a supposed Clymene Ocean. The proposal tentatively located this ocean a
Autor:
Miguel Angelo Stipp Basei, Umberto G. Cordani, Walter Maurício Sproesser, N. A. Castro, Kei Sato, Carlos Eduardo Ganade de Araujo
Publikováno v:
Repositório Institucional da USP (Biblioteca Digital da Produção Intelectual)
Universidade de São Paulo (USP)
instacron:USP
Universidade de São Paulo (USP)
instacron:USP
U–Pb geochronological analyses have been acquired on detrital zircon grains collected from 14 samples in the Ceara Central (CCD) and Medio Coreau (MCD) tectonic domains, separated by the Transbrasiliano-Kandi Lineament (TKL) on the Borborema Provin
Autor:
Candido Augusto Veloso Moura, Felipe Grandjean da Costa, Tercyo Rinaldo Gonçalves Pinéo, Carlos Eduardo Ganade de Araujo, José C. Cavalcante
Publikováno v:
Journal of South American Earth Sciences. 33:21-33
The Tamboril–Santa Quiteria Complex is an important Neoproterozoic granitic–migmatitic unit from the Ceara Central Domain that developed from ca. 650 to 610 Ma. In general the granitoids range in composition from diorite to granite with predomina
Publikováno v:
Repositório Institucional de Geociências-RIGEO
Companhia de Pesquisa de Recursos Minerais (CPRM)
instacron:CPRM
Biblioteca Digital de Teses e Dissertações da USP
Universidade de São Paulo (USP)
instacron:USP
Companhia de Pesquisa de Recursos Minerais (CPRM)
instacron:CPRM
Biblioteca Digital de Teses e Dissertações da USP
Universidade de São Paulo (USP)
instacron:USP
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
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9024e8f3c466042c2ccbc36370485666
https://doi.org/10.11606/t.44.2014.tde-25092014-144415
https://doi.org/10.11606/t.44.2014.tde-25092014-144415
Autor:
Miguel Angelo Stipp Basei, Renaud Caby, Joerg Hermann, Carlos Eduardo Ganade de Araujo, Daniela Rubatto, Umberto G. Cordani
Publikováno v:
Nature Communications
Nature Communications, Nature Publishing Group, 2014, 5, pp.5198. ⟨10.1038/ncomms6198⟩
Repositório Institucional da USP (Biblioteca Digital da Produção Intelectual)
Universidade de São Paulo (USP)
instacron:USP
Nature Communications, Nature Publishing Group, 2014, 5, pp.5198. ⟨10.1038/ncomms6198⟩
Repositório Institucional da USP (Biblioteca Digital da Produção Intelectual)
Universidade de São Paulo (USP)
instacron:USP
International audience; The deeply eroded West Gondwana Orogen is a major continental collision zone that exposes numerous occurrences of deeply subducted rocks, such as eclogites. The position of these eclogites marks the suture zone between collidi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5928bdd60e6c0311b2200732c6c1d264
https://hal.archives-ouvertes.fr/hal-01122789/file/ncomms6198.pdf
https://hal.archives-ouvertes.fr/hal-01122789/file/ncomms6198.pdf