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Gomes, M. E. P. (2000) Stanniferous quartz veins and quartz veins with scheelite and cassiterite from the Rebordelo-Ervedosa-Agrochão Region, Northeastern Portugal: Mineralogical and geochemical characteristics. Cadernos Lab. Xeolóxico de Laxe Coruña. Vol. 25, pp. 243-244

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Year2000
Original EntryGomes, M. E. P. (2000) Stanniferous quartz veins and quartz veins with scheelite and cassiterite from the Rebordelo-Ervedosa-Agrochão Region, Northeastern Portugal: Mineralogical and geochemical characteristics. Cadernos Lab. Xeolóxico de Laxe Coruña. Vol. 25, pp. 243-244
Mindat Ref. ID15977737Long-form Identifiermindat:1:5:15977737:6
GUIDc959ac4f-358b-46c3-871f-fc583201cc51
Full ReferenceGomes, M. E. P. (2000) Stanniferous quartz veins and quartz veins with scheelite and cassiterite from the Rebordelo-Ervedosa-Agrochão Region, Northeastern Portugal: Mineralogical and geochemical characteristics. Cadernos Lab. Xeolóxico de Laxe Coruña. Vol. 25, pp. 243-244
Plain TextGomes, M. E. P. (2000) Stanniferous quartz veins and quartz veins with scheelite and cassiterite from the Rebordelo-Ervedosa-Agrochão Region, Northeastern Portugal: Mineralogical and geochemical characteristics. Cadernos Lab. Xeolóxico de Laxe Coruña. Vol. 25, pp. 243-244

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LocalityCitation Details
Ervedosa Mine (Tuela Mine), Ervedosa, Vinhais, Bragança, Portugal

Mineral Occurrences

LocalityMineral(s)
Ervedosa Mine (Tuela Mine), Ervedosa, Vinhais, Bragança, Portugalⓘ Apatite, ⓘ Arsenopyrite, ⓘ Biotite, ⓘ Bismuth, ⓘ Bismuthinite, ⓘ Cassiterite, ⓘ Chalcopyrite, ⓘ Fluorite, ⓘ Granite, ⓘ K Feldspar, ⓘ Matildite, ⓘ Muscovite, ⓘ Plagioclase, ⓘ Pyrite, ⓘ Pyrrhotite, ⓘ Quartz, ⓘ Rutile, ⓘ Sphalerite, ⓘ Stannite
Trigueiriça Mines, Rebordelo, Vinhais, Bragança, Portugalⓘ Apatite, ⓘ Arsenopyrite, ⓘ Biotite, ⓘ Bismuth, ⓘ Cassiterite, ⓘ Chalcopyrite, ⓘ Granite, ⓘ K Feldspar, ⓘ Muscovite, ⓘ Pyrite, ⓘ Pyrrhotite, ⓘ Quartz, ⓘ Rutile, ⓘ Scheelite, ⓘ Sphalerite, ⓘ Stannite, ⓘ Tourmaline
Bejanca Mine (Carvalhal do Estanho), Queirã, Vouzela, Viseu, Portugalⓘ Apatite, ⓘ Arsenopyrite, ⓘ Bismuth, ⓘ Cassiterite, ⓘ Chalcopyrite, ⓘ Covellite, ⓘ Granite, ⓘ Herzenbergite, ⓘ Muscovite, ⓘ Pyrite, ⓘ Pyrrhotite, ⓘ Quartz, ⓘ Rutile, ⓘ Scheelite, ⓘ Sphalerite, ⓘ Stannite, ⓘ Tourmaline

See Also

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GOMES, E. M. C. and FONSECA, P. E. - Metamorphic and metasomatic late-variscan events in Alvito region (Alentejo, southern Portugal) Cadernos Lab. Xeolóxico de Laxe, Coruña. 2006. Vol. 31, pp. 67 - 85.
Coruña. 2006. Vol. 31, pp. 67 - 85Cadernos Lab. Xeolóxico de Laxe
Cadernos Lab. Xeolóxico de Laxe
Cárdenes, V. (2013). The Valborraz tungsten mine: Description of a potential source of arsenic pollution. Cadernos Lab. Xeolóxico de Laxe Coruña. 2013. Vol. 37, pp. 147 - 162
Ferrer Modolell, A.E. (1991) Procesos hidrotermales asociados a la mineralización ferrífera de Celrá. Cuaderno Lab. Xeolóxico de Laxe, Coruña: 16: 75-83.
Neiva, A. M. R. (1994): Gold-​quartz veins at Gralheira, northern Portugal: mineralogical and geochemical characteristics. Transactions of the Institution of Mining and Metallurgy, Section B: Applied Earth Science 103, B188-B196.
Lee, C. (2020) Sequential Scheelite Mineralization of Quartz–Scheelite Veins at the Sangdong W-Deposit: Microtextural and Geochemical Approach. Minerals 10, 678.
Neiva, A.M.R. (2008) Geochemistry of cassiterite and wolframite from tin and tungsten quartz veins in Portugal. Ore Geology Reviews, 33 (3) 221-238 doi:10.1016/j.oregeorev.2006.05.013
Neiva, A. M. R.; Andráš, P.; Ramos, J. M. F. (2008): Antimony quartz and antimony-gold quartz veins from northern Portugal. Ore Geology Reviews 34, 533-546.
Costa, F., Canals, A. and Delgado, J. (2000). Las Areniscas de la Mina Eureka (Cu-U-V) (Pirineo Central). Texturas observadas versus reacciones planteadas. Cuadernos Lab. Xeológico de Laxe, Coruña. Vol. 25, pp. 309-311.
Gomes, C. A. L., & Neiva, A. M. (2022). Tourmalines in the Namacotche Li-Cs-Ta granitic pegmatite group, Mozambique: crystal chemistry and origin. Cadernos do Laboratorio Xeolóxico de Laxe. Revista de Xeoloxía Galega e do Hercínico Peninsular, 44, 132-153.
 
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