Zobrazeno 1 - 10
of 100
pro vyhledávání: '"Dom Feliciano Belt in Uruguay"'
Publikováno v:
In Journal of South American Earth Sciences June 2021 108
Publikováno v:
In Precambrian Research March 2011 185(3-4):149-163
Autor:
Masquelin, Henri1 emasquelin@fcien.edu.uy, Lara, Hernán Silva2 hsilva@fcien.edu.uy, Bettucci, Leda Sánchez1, Demarco, Pablo Núñez1, Pascual, Sofía3, Muzio, Rossana1, Peel, Elena1, Scaglia, Fernando3 scagliageo@gmail.com
Publikováno v:
Brazilian Journal of Geology. 2017, Vol. 47 Issue 1, p21-42. 22p.
Autor:
Lenz, C.1 crislenz@yahoo.com.br, Porcher, C.2 carla.porcher@ufrgs.br, Fernandes, L.2 ladfernandes@gmail.com, Masquelin, H.3 hmasquel@fcien.edu.uy, Koester, E.2 edineikoester@yahoo.com.br, Conceição, R.2 rommulo.conceicao@ufrgs.br
Publikováno v:
Mineralogy & Petrology. Oct2013, Vol. 107 Issue 5, p785-806. 22p.
Autor:
Miguel Angelo Stipp Basei, Sebastián Oriolo, Pedro Oyhantçabal, D. Frei, Klaus Wemmer, Siegfried Siegesmund
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
New isotopic and geochemical data for the Paleo- Meso- and Neoproterozoic metasedimentary cover of the southern Dom Feliciano Belt (Brasiliano/Pan-African) are presented and evaluated combined with published information. Whole-rock major and trace el
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4740bb2b148fbd316232c23190b2c502
Publikováno v:
Precambrian Research. 185(3-4):149-163
Neoproterozoic ages of magmatic and metamorphic events were obtained from in situ SHRIMP analysis of zircons from the Cerro Bori Orthogneisses, eastern domain of the Dom Feliciano Belt in Uruguay. Detailed textural analysis of zircons and their ages
Akademický článek
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Autor:
Elena Peel, Sofía Pascual, Leda Sánchez Bettucci, Fernando Scaglia, Hernán Silva Lara, Henri Masquelin, Pablo Núñez Demarco, Rossana Muzio
Publikováno v:
Brazilian Journal of Geology, Volume: 47, Issue: 1, Pages: 21-42, Published: JAN 2017
COLIBRI
Universidad de la República
instacron:Universidad de la República
CONICET Digital (CONICET)
Consejo Nacional de Investigaciones Científicas y Técnicas
instacron:CONICET
Brazilian Journal of Geology, Vol 47, Iss 1, Pp 21-42
Brazilian Journal of Geology v.47 n.1 2017
Brazilian Journal of Geology
Sociedade Brasileira de Geologia (SBGEO)
instacron:SBGEO
COLIBRI
Universidad de la República
instacron:Universidad de la República
CONICET Digital (CONICET)
Consejo Nacional de Investigaciones Científicas y Técnicas
instacron:CONICET
Brazilian Journal of Geology, Vol 47, Iss 1, Pp 21-42
Brazilian Journal of Geology v.47 n.1 2017
Brazilian Journal of Geology
Sociedade Brasileira de Geologia (SBGEO)
instacron:SBGEO
This work is the result of a multiyear effort to use field geology to describe lithologies, to establish contact relationships and to create a sketch of the tectonic evolution of the Meso- to Neoproterozoic metasedimentary successions within the Schi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::03fa578c5b0105b35c30148eb2f671b3
http://www.scielo.br/scielo.php?script=sci_arttext&pid=S2317-48892017000100021&lng=en&tlng=en
http://www.scielo.br/scielo.php?script=sci_arttext&pid=S2317-48892017000100021&lng=en&tlng=en
Autor:
Henri Masquelin, Cristine Lenz, Edinei Koester, L.A.D. Fernandes, Rommulo Vieira Conceição, Carla Cristine Porcher
Publikováno v:
Mineralogy and Petrology. 107:785-806
The Cerro Bori orthogneisses, crystallized between ca. 800 and 767 Ma, are composed of a sequence of mafic gneisses, with dioritic-gabbroic and dioritic composition tectonically interleaved with a sequence of tonalitic and granodioritic gneisses. The
Autor:
Henri Masquelin, Hernán Silva Lara, Leda Sánchez Bettucci, Pablo Núñez Demarco, Sofía Pascual, Rossana Muzio, Elena Peel, Fernando Scaglia
Publikováno v:
Brazilian Journal of Geology, Vol 47, Iss 1, Pp 21-42
ABSTRACT: This work is the result of a multiyear effort to use field geology to describe lithologies, to establish contact relationships and to create a sketch of the tectonic evolution of the Meso- to Neoproterozoic metasedimentary successions withi
Externí odkaz:
https://doaj.org/article/52c32bb62cb941888b32adf135f7f320