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Detalhes Referência

Tipo
Artigos em Revista

Tipo de Documento
Artigo Completo

Título
Garnet-biotite diffusion mechanisms in complex high-grade orogenic belts: Understanding and constraining petrological cooling rates in granulites from Ribeira Fold Belt (SE Brazil)

Participantes na publicação
Telmo M. Bento dos Santos (Author)
Dep. Geologia
IDL
Colombo C.G. Tassinari (Author)
Paulo E. Fonseca (Author)
Dep. Geologia
CEGUL

Data de Publicação
2014-12

Suporte
Journal of South American Earth Sciences

Identificadores da Publicação
ISSN - 0895-9811

Editora
Elsevier BV

Volume
56

Número de Páginas
10
Página Inicial
128
Página Final
138

Identificadores do Documento
DOI - https://doi.org/10.1016/j.jsames.2014.09.003
URL - http://dx.doi.org/10.1016/j.jsames.2014.09.003

Identificadores de Qualidade
SCOPUS Q2 (2014) - 0.873 - Earth-Surface Processes
SCOPUS Q2 (2014) - 0.873 - Geology


Exportar referência

APA
Telmo M. Bento dos Santos, Colombo C.G. Tassinari, Paulo E. Fonseca, (2014). Garnet-biotite diffusion mechanisms in complex high-grade orogenic belts: Understanding and constraining petrological cooling rates in granulites from Ribeira Fold Belt (SE Brazil). Journal of South American Earth Sciences, 56, 128-138. ISSN 0895-9811. eISSN . http://dx.doi.org/10.1016/j.jsames.2014.09.003

IEEE
Telmo M. Bento dos Santos, Colombo C.G. Tassinari, Paulo E. Fonseca, "Garnet-biotite diffusion mechanisms in complex high-grade orogenic belts: Understanding and constraining petrological cooling rates in granulites from Ribeira Fold Belt (SE Brazil)" in Journal of South American Earth Sciences, vol. 56, pp. 128-138, 2014. 10.1016/j.jsames.2014.09.003

BIBTEX
@article{39880, author = {Telmo M. Bento dos Santos and Colombo C.G. Tassinari and Paulo E. Fonseca}, title = {Garnet-biotite diffusion mechanisms in complex high-grade orogenic belts: Understanding and constraining petrological cooling rates in granulites from Ribeira Fold Belt (SE Brazil)}, journal = {Journal of South American Earth Sciences}, year = 2014, pages = {128-138}, volume = 56 }