Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Patrícia Duffles"'
Publikováno v:
Anais do(a) Anais Simpósio de Gestão Ambiental e Biodiversidade.
Autor:
Rodrigo Vinagre Cintra Da Costa, Rudolph Allard Johannes Trouw, Andre Ribeiro, Julio Cezar Mendes, Felipe Tavares, Felipe Nepomuceno, Débora Barros Nascimento, Marcos Ferreira Fontainha, Patrícia Duffles, Camilo Correia Trouw
Publikováno v:
Journal of South American Earth Sciences. 124:104287
Publikováno v:
Precambrian Research. 278:69-86
The Embu Complex crops out in the southeastern part of Sao Paulo state in Brazil and consists mainly of Neoproterozoic metasedimentary rocks belonging to the interference zone between the Brasilia and Ribeira fold belts. We present U–Pb ages (LA-IP
Autor:
Rudolph A.J. Trouw, Gabriel Correa de Matos, Julio Cezar Mendes, Rodrigo Peternel, Rodrigo Vinagre, Patrícia Duffles
Publikováno v:
Journal of South American Earth Sciences. 54:120-139
This paper presents a detailed description of the Neoproterozoic Serra da Agua Limpa batholith (SALB) and the interpretation of its genesis. The batholith, located along the border of the states of Minas Gerais and Sao Paulo, was involved in the Soco
Publikováno v:
Brazilian Journal of Geology. 43:487-500
The Marins Granite forms an ellipsoidal body that crops out along the border between Sao Paulo and Minas Gerais states. It intrudes meta-sedimentary and meta-igneous rocks of Neoproterozoic age, belonging to the Socorro Nappe and Embu Complex, in the
Autor:
Julio Cezar Mendes, Patrícia Duffles Teixeira, Gabriel Corrêa de Matos, Isabel Pereira Ludka, Felipe Fonseca Fernandes de Medeiros, Ciro Alexandre Ávila
Publikováno v:
Revista Brasileira de Geociências. 37:101-113
Autor:
Rodrigo Vinagre, Rudolph Allard Johannes Trouw, Hugo Kussama, Rodrigo Peternel, Julio Cezar Mendes, Patrícia Duffles
Publikováno v:
Brazilian Journal of Geology, Vol 46, Iss 4, Pp 547-566
ABSTRACT: The study area is localized in the Socorro nappe, part of the southern Brasília belt, with a minor part in the Embu terrane, part of the central Ribeira belt. Three phases of deformation were detected, Dn-1, Dn and Dn+1. Sn-1 seems to be g
Externí odkaz:
https://doaj.org/article/ca5128d36e404bcab3c35157a2fd713c