Garnet-biotite diffusion mechanisms in complex high-grade orogenic belts: Understanding and constraining petrological cooling rates in granulites from Ribeira Fold Belt (SE Brazil)-Reference-Cited by-同舟云学术

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

Published:2014-12 Issue: Volume:56 Page:128-138
ISSN:0895-9811
Container-title:Journal of South American Earth Sciences
language:en
Short-container-title:Journal of South American Earth Sciences

Author:

Bento dos Santos Telmo M.^ORCID,Tassinari Colombo C.G.,Fonseca Paulo E.

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geology

Reference45 articles.

1. Titanohematite lattice preferred orientation and magnetic anisotropy in high-temperature mylonites;Bascou;Earth Planet. Sci. Lett.,2002

2. Petrologia e termocronologia de granulitos no sector central da Faixa Ribeira (Região de São Fidelis, Rio de Janeiro, Brasil);Bento dos Santos,2008

3. Thermochronological evidence for long-term elevated geothermal gradients in Ribeira Fold Belt, SE Brazil;Bento dos Santos;Geochim. Cosmochim. Acta,2007

4. Geodynamic evolution of the São Fidelis – Santo Antônio de Pádua sector, Ribeira Fold Belt, SE Brazil;Bento dos Santos;Comun. Geol.,2009

5. Assumptions and problems with Fe-Mg garnet – biotite diffusion based petrological cooling rates: a case study in granulites and migmatites from central Ribeira Fold Belt, SE Brazil;Bento dos Santos;Comun. Geol.,2009

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