The Mg/(Fe + Mg) ratio and the Ti and A site contents of tourmaline as promising indicators of granitic magma evolution

Author:

da Costa Isabel Ribeiro,Antunes Isabel Margarida Horta Ribeiro,Récio Clemente

Publisher

Springer Science and Business Media LLC

Subject

Stratigraphy,Geology

Reference37 articles.

1. Antunes, I. M. H. R. (2006). Mineralogia, petrologia e geoquímica de rochas granitóides da área de Castelo Branco—Idanha-a-Nova. Unpubl. PhD Thesis, Universidade de Coimbra, 453 pp.

2. Borthwick, J., & Harmon, R. S. (1982). A note regarding ClF3 as an alternative to Br F5 for oxygen isotope analysis. Geochimica et Cosmochimica Acta, 46, 1665–1668.

3. Broska, I., & Uher, P. (2001). Whole-rock chemistry and genetic typology of the west Carpathian Variscan granites. Geol. Carpathica, 52, 78–90.

4. Chappell, B. W., & Hine, R. (2006). The Cornubian Batholith: an example of magmatic fractionation on a crustal scale. Resource Geology, 56, 203–244.

5. Chappell, B. W., & White, A. J. R. (2001). Two contrasting granite types: 25 years later. Australian Journal of Earth Sciences, 48, 489–499.

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