Occurrence and Origin of Andalusite in Peraluminous Felsic Igneous Rocks

Autor: JM Ugidos, Ben J. Williamson, CL Gomes, Donna L. Whitney, Pavel Uher, HH Woodard, B. Gottesmann, Ajsc Pereira, Bernardo Cesare, Alcides N. Sial, Simon Richards, Axel D. Renno, Hans-Jürgen Förster, Friedrich Koller, Ljpf Neves, Michel Pichavant, Martha Leticia Gaeta, M. El Baghdadi, Saskia Erdmann, Carlos Villaseca, Alejandro J. Toselli, Daniel S. Barker, Drm Pattison, Dario Visonà, Carlos W. Rapela, Geoffrey L. Clarke, B. Barbarin, Michael J. Dorais, J. Saavedra, A. Rottura, George B. Morgan, Daniel J. Kontak, D. B. Clarke, Malcolm P. Roberts, David London, Rebecca Anne Jamieson

Publikováno v: Journal of Petrology
Journal of Petrology, Oxford University Press (OUP), 2005, 46, pp.3, 441-472. ⟨10.1093/petrology/egh083⟩
E-Prints Complutense: Archivo Institucional de la UCM
Universidad Complutense de Madrid
Journal of Petrology, 2005, 46, pp.3, 441-472. ⟨10.1093/petrology/egh083⟩
SEDICI (UNLP)
Universidad Nacional de La Plata
instacron:UNLP
E-Prints Complutense. Archivo Institucional de la UCM
instname

Andalusite occurs as an accessory mineral in many types of peraluminous felsic igneous rocks, including rhyolites, aplites, granites, pegmatites, and anatectic migmatites. Some published stability curves for And = Sil and the water-saturated granite

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a21a60fa5be603d9d4b4aaec5eecbd98
http://eprints.ucm.es/12348/