Solubility of excess alumina in hydrous granitic melts in equilibrium with peraluminous minerals at 700–800 °C and 200 MPa, and applications of the aluminum saturation index
Author:
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics
Link
http://link.springer.com/content/pdf/10.1007/s00410-003-0486-6.pdf
Reference85 articles.
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2. Ayres M, Harris N, Vance D (1997) Possible constraints on anatectic melt residence times from accessory mineral dissolution rates: an example from Himalayan leucogranites. Min Mag 61:29–36
3. Barbero L, Villaseca C, Rogers G, Brown PE (1995) Geochemical and isotopic disequilibrium in crustal melting: an insight from the anatectic granitoids from Toledo, Spain. J Geophys Res 100:15745–15765
4. Barbey P, Macaudiere J, Nzenti JP (1990) High-pressure dehydration melting of metapelites: evidence from the Migmatites of Yaoundé (Cameroon). J Petrol 31:401–427
5. Bea F, Montero P (1999) Behaviour of accessory phases and redistribution of Zr, REE, Y, Th, and U during metamorphism and partial melting of metapelites in the lower crust: an example from the Kinzigite Formation of Ivrea-Verbano, NW Italy. Geochim Cosmochim Acta 63:1133–1153
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