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Comment on 'Geochronology (Ar-Ar, K-Ar and He-exposure ages) of Cenozoic magmatic rocks from northern Chile (18-22°S): implications for magmatism and tectonic evolution of the central Andes' of Wörner et al. (2000)
(Servicio Nacional de Geología y Minería (SERNAGEOMIN), 2001)
Late cretaceous-early tertiary ultrabasic magmatism in the western part of the state of Rio de Janeiro, BrazilLate cretaceous-early tertiary ultrabasic magmatism in the western part of the state of Rio de Janeiro, Brazil
(Universidade de São Paulo, Instituto de Geociências, 1991)
Chilled and frozen margins: evidence of thermal contrast in mafic dykes and their significance for magmatic consolidationChilled and frozen margins: evidence of thermal contrast in mafic dykes and their significance for magmatic consolidation
(Universidade de São Paulo, Instituto de Geociências, 1991)
Magmatic and post-magmatic signatures of chromian spinels in podiform chromitites from the Cheshmeh- Bid chromitite deposit, Khajeh-Jamali Ophiolitic Massifs, Iran
(2015)
Podiform bodies of high-Cr chromitite in the Cheshmeh-Bid chromitite deposit are located at the mantle-lower crust transition zone (MTZ) of the Late Cretaceous Khajeh-Jamali ophiolitic massifs, Iran. The unaltered core of ...
Large scale magmatic banding in mesozoic basic sill of the Paraná basin, Campinas, São Paulo State, BrazilLarge scale magmatic banding in mesozoic basic sill of the Paraná basin, Campinas, São Paulo State, Brazil
(Universidade de São Paulo, Instituto de Geociências, 1998)
Time constraints on magmatism along the Major Gercino Shear Zone, southern Brazil: Implications for West Gondwana reconstruction
(ELSEVIER SCIENCE BVAMSTERDAM, 2012)
The Dom Feliciano Belt, situated in southernmost Brazil and Uruguay, contains a large mass of granite-gneissic rocks (also known as Florianopolis/Pelotas Batholith) formed during the pre-, syn- and post-orogenic phases of ...
The alkaline silica-saturated ultrapotassic magmatism of the Riacho do Pontal Fold Belt, NE Brazil: an example of syenite–granite Neoproterozoic association
(Journal of South American Earth Sciences, 2000)
The Neoproterozoic of northeastern Brazil was marked by the development of collisional fold belts, mainly surrounding the Sa˜o Francisco
Craton, and an associated widespread granitic magmatism. The Casa Nova 555 ^ 10 Ma; ...
The late precambrian K-alkaline magmatism in the Ribeira Fold Belt: a case study of the Piracaia Pluton, State of São Paulo, SE Brazil, and its potential mineralization (Cu, Zn, Gd)
(Elsevier B.V., 2001-04-01)
The Pluriserial Ribeira Magmatic System-590 of the Late Precambrian Ribeira Fold Belt comprises seven groups of high-K rocks of crustal or mantle origin with ages ranging between 620 and 570 Ma. One of these groups is ...