Late magmatic controls on the origin of schorlitic and foititic tourmalines from late-Variscan peraluminous granites of the Arbus pluton (SW Sardinia, Italy): Crystal-chemical study and petrological constraints

Author:

Bosi Ferdinando,Naitza Stefano,Skogby Henrik,Secchi Francesco,Conte Aida M.,Cuccuru Stefano,Hålenius Ulf,De La Rosa Nathaly,Kristiansson Per,Charlotta Nilsson E.J.,Ros Linus,Andreozzi Giovanni B.

Funder

Sapienza University of Rome

FdS-RAS

Swedish Research Council

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference96 articles.

1. Thermodynamic modeling of biotite stability in assemblage with feldspar, quartz, fayalite, pyrrhotite, and ilmenite in a COHSF fluid at 427–1027 °C and 2 kbar;Abramov;Geochem. Int.,2000

2. Linking Mössbauer and structural parameters in elbaite-schorl-dravite tourmalines;Andreozzi;Am. Mineral.,2008

3. Phase relations of tourmaline leucogranites and the significance of tourmaline in silicic magmas;Benard;J. Geol.,1985

4. Stereochemical constraints in tourmaline: from a short-range to a long-range structure;Bosi;Can. Mineral.,2011

5. Bond-valence constraints around the O1 site of tourmaline;Bosi;Mineral. Mag.,2013

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