The link between partial melting, granitization and granulite development in central Ribeira Fold Belt, SE Brazil: New evidence from elemental and Sr–Nd isotopic geochemistry

Author:

Bento dos Santos Telmo M.,Munhá José M.,Tassinari Colombo C.G.,Fonseca Paulo E.

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geology

Reference76 articles.

1. Nd-Sr isotopic relationship in granitoid rocks and continental crust development: a chemical approach to orogenesis;Allègre;Nature,1980

2. Titanohematite lattice preferred orientation and magnetic anisotropy in high-temperature mylonites;Bascou;Earth and Planetary Science Letters,2002

3. A Metodologia U–Pb na Universidade de São Paulo. Princípios metodológicos, aplicações e resultados obtidos;Basei;Anais da Academia Brasileira de Ciências,1995

4. Residence of REE, Y, Th and U in granites and crustal protoliths; implications for the chemistry of crustal melts;Bea;Journal of Petrology,1996

5. Nd–Sr isotopic composition of granulites and constrains on the evolution of the lower continental crust;Ben Othman;Nature,1984

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