Zobrazeno 1 - 10
of 18
pro vyhledávání: '"Carlos Alejandro Salazar"'
Autor:
Sérgio Wilians de Oliveira Rodrigues, Fabrizio Prior Caltabeloti, Vidya Viera de Almeida, Mariane Brumati, Carlos José Archanjo, Maria Helena B.M. Hollanda, Carlos Alejandro Salazar, Dunyi Liu
Publikováno v:
Geologia USP. Série Científica, Vol 11, Iss 3, Pp 3-21 (2011)
The Patrimônio Santo Antônio and São Domingos Granites are located in the northwest portion of the Itaiacoca Belt,which is part of the Apiaí Terrane (or tectonic domain), a segment of the southern Ribeira Belt, the major tectonic unit of theManti
Externí odkaz:
https://doaj.org/article/8cea439aa2924b4c929716d392eb2248
Autor:
Sérgio Wilians de Oliveira Rodrigues, Fabrizio Prior Caltabeloti, Vidya Viera de Almeida, Mariane Brumati, Carlos José Archanjo, Maria Helena B.M Hollanda, Carlos Alejandro Salazar, Dunyi Liu
Publikováno v:
Geologia USP. Série Científica, Vol 11, Iss 3 (2011)
Os Granitos Patrimônio Santo Antônio e São Domingos localizam-se na porção noroeste da Faixa Itaiacoca constituinte do Terreno (ou domínio tectônico) Apiaí segmento do Cinturão Ribeira Meridional da Província Mantiqueira localizada no sudoe
Externí odkaz:
https://doaj.org/article/51202a177bab426ba0317fed04fb6666
Autor:
Carlos Alejandro Salazar
Publikováno v:
Biblioteca Digital de Teses e Dissertações da USPUniversidade de São PauloUSP.
A trama de magmas graníticos alojados na crosta intermediária e superior pode-se originar pela ação de forças de corpo (ascensionais, convectivas) e/ou tectônicas. Diferentes mecanismos podem concorrer para a formação de tramas, embora a inte
Autor:
Carlos Alejandro Salazar
Publikováno v:
Biblioteca Digital de Teses e Dissertações da USPUniversidade de São PauloUSP.
O batólito Itaóca é uma suíte granítica Neoproterozóica cristalizada na crosta rasa cuja fácies dominantes, é constituída por um monzogranito porfirítico. O batólito intrude rochas metamorfisadas em fácies xisto verde do Bloco Lajeado, é
Publikováno v:
Geociências, Sociedade e Sustentabilidade
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3c592d10094256a908cb30cce7f3f4e5
https://doi.org/10.37423/200300543
https://doi.org/10.37423/200300543
Autor:
Fabrizio P. Caltabellota, Carlos Alejandro Salazar, Carlos José Archanjo, Sérgio Wilians de Oliveira Rodrigues
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
Strike-slip shear zones formed during continental collisions accommodate the convergence and indentation of rigid cratonic blocks. In high-temperature settings of deeply eroded orogens, such as the Neoproterozoic Ribeira belt in southeastern Brazil,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a9ce97c251c2920b3cdac9e0809cf45f
https://doi.org/10.1016/j.precamres.2021.106417
https://doi.org/10.1016/j.precamres.2021.106417
Autor:
Marcelo Esteves Almeida, Marcia Caroline R. Carneiro, Carlos Alejandro Salazar, Rielva Solimairy Campelo do Nascimento, Marcel Silva Passos, Vanisse de Oliveira Rodrigues, Ivaldo Rodrigues da Trindade
Publikováno v:
Journal of South American Earth Sciences. 77:310-326
A lithostratigraphic review of the Cauaburi Complex was carried out by means of field, tectono-metamorphic and geochemical data, which were the basis for the sub-division of the Cauaburi Complex orthogneisses into the Santa Izabel do Rio Negro, Cumat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::50b195d047ccfe89d312b310f95f592c
https://doi.org/10.1016/j.jsames.2017.06.001
https://doi.org/10.1016/j.jsames.2017.06.001
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
The Madeira granite is one of the Paleoproterozoic (1.82 Ga) A-type granite intrusions in the Amazonian Craton. It is elongated in the NE–SW direction and is composed of four facies. Classical structural techniques and the anisotropy of magnetic su
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6e7989de12ca76a71b2939a10be9161b
https://doi.org/10.1016/j.lithos.2016.10.021
https://doi.org/10.1016/j.lithos.2016.10.021
Publikováno v:
Anais do(a) Anais do XVI Simposio de Geologia da Amazônia.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::84765b9584f06cc2a3d0299c72f71167
https://doi.org/10.29327/15025.1-1
https://doi.org/10.29327/15025.1-1
Autor:
Márcio Yee, Sonia Hatsue Tatumi, Marcel Silva Passos, Emílio Alberto Amaral Soares, J.C.R. Mittani, Ericson Hideki Hayakawa, Carlos Alejandro Salazar
Publikováno v:
Journal of South American Earth Sciences. 98:102455
Three levels of Pleistocene-Holocene fluvial terraces, informally referred to as Upper (UT), Intermediate (IT) and Lower (LT) Terraces, are described in the stretch between the Purus and Manacapuru tributaries (Western Amazonia) of the Solimoes-Amazo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3848d38801065c20700e8d2435014c9f
https://doi.org/10.1016/j.jsames.2019.102455
https://doi.org/10.1016/j.jsames.2019.102455