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Geologia dos Granitoides Sanga Rasa, terreno Taquarembó, Bagé, RS [PDF]

, 2013
O Terreno Taquarembó está localizado na porção SW do Escudo Sul-rio-grandense e é interpretado como um fragmento do Cráton Rio de La Plata. Este Terreno é composto por gnaisses paleoproterozóicos do Complexo Granulítico Santa Maria Chico (CGSMC ...
Tambara, Guilherme Baldissera
core  

Origin of granitoid rocks [PDF]

Nature, 1983
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Geoquímica e geocronologia U-Pb, Sm-Nd e Rb-Sr dos granitoides orosirianos do domínio Erepecuru-Trombetas, Província Amazônia Central, Noroeste do Pará

, 2015
The granitic rocks of the northwestern Pará State are part of two large volcano- plutonic associations that marked the central region of the Amazonian Craton during Orosirian.
LEAL, Rafael Estumano
core  

Granitoid-series evaluation of the Archaean Johannesburg Dome granitoids, South Africa.

BULLETIN OF THE GEOLOGICAL SURVEY OF JAPAN, 2002
Shunso ISHIHARA, ANHAEUSSER Carl R., ROBB Laurence J.   +2 more
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Composición química de granitos batolíticos de las sierras pampeanas

Revista del Museo de La Plata
Se describe en esta contribución la metodología químico-analítica y los resultados obtenidos mediante la misma a los efectos de la determinación de elementos mayoritarios y trazas en cuerpos graníticos mayores de las Sierras Pampeanas.
Carlos W. Rapela, Larry Heaman
doaj  

Granitoid-associated veins

, 1995
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Pseudomorphic lines of autochthonous granitoids

, 2006
Для автохтонних ультраметаморфічних гранітоїдів показано існування в природі шести псевдоморфних рядів: лейкогранітоїдного, аляскітоїдного, кінцигітоїдного, плагіогранітоїдного, діоритоїдного й ендербітоїдного та розглянуті їх петрохімічні особливості.
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On the origin of magnetite-series granitoids in the terrane of ilmenite-series granitoids, with special reference to some granitoids in the San'yo belt, southwest Japan

, 1992
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Granitoides of the State of Bahia, Brazil

, 1987
Conceicao, H., Davison, I., Fujimori, S., McReath, I., /Sabaté, Pierre   +4 more
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Metamorphism of Granitoids

1994
Granitoid rocks comprise granites, alkali-feldspar granites, granodiorites and tonalites, and constitute a large portion of the continental crust. Because the main constituents — alkali-feldspar, plagioclase, quartz, biotite, muscovite, hornblende — are found over a wide range of P-T conditions, this rock group is not a very useful indicator of ...
Kurt Bucher, Martin Frey
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