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Fuertes-Fuente, M., Martin-Izard, A., Boiron, M. C., Vinuela, J. M. (2000) P T PATH AND FLUID EVOLUTION IN THE FRANQUEIRA GRANITIC PEGMATITE, CENTRAL GALICIA, NORTHWESTERN SPAIN. The Canadian Mineralogist, 38 (5) 1163-1175 doi:10.2113/gscanmin.38.5.1163

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Reference TypeJournal (article/letter/editorial)
TitleP T PATH AND FLUID EVOLUTION IN THE FRANQUEIRA GRANITIC PEGMATITE, CENTRAL GALICIA, NORTHWESTERN SPAIN
JournalThe Canadian Mineralogist
AuthorsFuertes-Fuente, M.Author
Martin-Izard, A.Author
Boiron, M. C.Author
Vinuela, J. M.Author
Year2000 (October 1)Volume38
Issue5
PublisherMineralogical Association of Canada
Download URLhttps://rruff.info/doclib/cm/vol38/CM38_1163.pdf+
DOIdoi:10.2113/gscanmin.38.5.1163Search in ResearchGate
Generate Citation Formats
Mindat Ref. ID63398Long-form Identifiermindat:1:5:63398:1
GUID0
Full ReferenceFuertes-Fuente, M., Martin-Izard, A., Boiron, M. C., Vinuela, J. M. (2000) P T PATH AND FLUID EVOLUTION IN THE FRANQUEIRA GRANITIC PEGMATITE, CENTRAL GALICIA, NORTHWESTERN SPAIN. The Canadian Mineralogist, 38 (5) 1163-1175 doi:10.2113/gscanmin.38.5.1163
Plain TextFuertes-Fuente, M., Martin-Izard, A., Boiron, M. C., Vinuela, J. M. (2000) P T PATH AND FLUID EVOLUTION IN THE FRANQUEIRA GRANITIC PEGMATITE, CENTRAL GALICIA, NORTHWESTERN SPAIN. The Canadian Mineralogist, 38 (5) 1163-1175 doi:10.2113/gscanmin.38.5.1163
In(2000, October) The Canadian Mineralogist Vol. 38 (5) Mineralogical Association of Canada

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Fuertes-Fuente, M., Martin-Izard, A., Boiron, M. C., Mangas, J. (2000) Fluid evolution of rare-element and muscovite granitic pegmatites from central Galicia, NW Spain. Mineralium Deposita, 35 (4) 332-345 doi:10.1007/s001260050245
Fuertes-Fuente, M., & Martin-Izard, A. (2001). The Forcarei Norte and Lalín pegmatite fields, Galicia, Northwest of Spain. Mineral Deposits at the Beginning of the 21st Century, 413.
Martin-Izard, A., Paniagua, A., Moreiras, D. (1995) Metasomatism at a granitic pegmatite-dunite contact in Galicia: the Franqueira occurrence of chrysoberyl (alexandrite), emerald, and phenakite. Canadian Mineralogist, 33, 775-792.
Martin-Izard, A., Paniagua, A., Moreiras, D., Acevedo, R.D., and Marcos-Pascual, C. (1995) Metasomatism at a granitic pegmatite - dunite contact in Galicia: the Franqueira occurrence of chrysoberyl (alexandrite), emerald, and phenakite. The Canadian Mineralogist: 33: 775-792.
Fuertes-Fuente, Mercedes, Cepedal, Antonia, Martin-Izard, Agustín (2019) Mineralogical study of the wallrock metasomatism in barren and Li-Sn-Ta mineralized pegmatites from NW Spain (Central Galicia) The Canadian Mineralogist, 57 (5) 741-743 doi:10.3749/canmin.ab00010
Cepedal, A., Fuertes-Fuente, M., Martin-Izard, A., Gonzalez-Nistal, S., Barrero, M. (2008) old-bearing As-rich pyrite and arsenopyrite from the El Valle gold deposit, Asturias, northwestern Spain. The Canadian Mineralogist, 46 (1). 233-247 doi:10.3749/canmin.46.1.233
Franz, G., Gilg, H. A., Grundmann, G., Morteani, G., Martin-Izard, A., Paniagua, A., ... & Marcos-Pascual, C. (1996). Metasomatism at a granitic pegmatite-dunite contact in Galicia; the Franqueira occurrence of chrysoberyl (alexandrite), emerald, and phenakite; discussion and reply. The Canadian Mineralogist, 34(6), 1329-1336.
Brown, C. D., Wise, M. A. (2001) INTERNAL ZONATION AND CHEMICAL EVOLUTION OF THE BLACK MOUNTAIN GRANITIC PEGMATITE, MAINE. The Canadian Mineralogist, 39 (1) 45-55 doi:10.2113/gscanmin.39.1.45
Puga, E., Nieto, J. M., De Federico, A. D. (2000) CONTRASTING P T PATHS IN ECLOGITES OF THE BETIC OPHIOLITIC ASSOCIATION, MULHACEN COMPLEX, SOUTHEASTERN SPAIN. The Canadian Mineralogist, 38 (5) 1137-1161 doi:10.2113/gscanmin.38.5.1137
Canosa, Francisco, Martin-Izard, Agustín, Fuertes-Fuente, Mercedes (2012) Evolved granitic systems as a source of rare-element deposits: The Ponte Segade case (Galicia, NW Spain) Lithos, 153. 165-176 doi:10.1016/j.lithos.2012.06.029
Masau, M., Černý, P., Chapman, R. (2000) Dysprosian xenotime-(Y) from the Annie Claim #3 granitic pegmatite, southeastern Manitoba, Canada; evidence of the tetrad effect? The Canadian Mineralogist, 38 (4). 899-905 doi:10.2113/gscanmin.38.4.899
 
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