Vote for your favorite mineral in #MinCup26! - Quartz vs. Asagiite
It's a classic vs a newbie as the most common named mineral in the crust Quartz is up against an exceedingly-rare sea foam-green mineral discovered just a few years ago Asagiite.
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Sericite from
Neves-Corvo Mine, Santa Bárbara de Padrões, Castro Verde, Beja, Portugal


Locality type:Mine
Classification
Species:Muscovite var: Sericite
Formula:KAl2(AlSi3O10)(OH)2
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Sericite data
Locality Data:Click here to view Neves-Corvo Mine, Santa Bárbara de Padrões, Castro Verde, Beja, Portugal
Data Identifiers
Mindat Occurrence Record ID:430254
Long-form Identifier:1:3:430254:4
GUID (UUID V4):0
Nearest other occurrences of Sericite
7.7km (4.8 miles) ⓘBarrigão Mine, Santa Cruz, Almodôvar, Beja, Portugal
36.9km (23.0 miles) ⓘAlgares deposit, Aljustrel Mine, Aljustrel e Rio de Moinhos, Aljustrel, Beja, Portugal
37.1km (23.0 miles) ⓘFeitais deposit, Aljustrel Mine, Aljustrel e Rio de Moinhos, Aljustrel, Beja, Portugal
63.8km (39.7 miles) ⓘSalgadinho Mine, Cercal do Alentejo, Santiago do Cacém, Setúbal, Portugal
64.9km (40.3 miles) ⓘLousal Mine, Azinheira dos Barros, Grândola, Setúbal, Portugal
76.0km (47.2 miles) ⓘFilón Norte open pit (Filón Norte Mine), Tharsis Mines, Tharsis, Alosno, Huelva, Andalusia, Spain
85.4km (53.1 miles) ⓘLagoa Salgada deposit, Grândola e Santa Margarida da Serra, Grândola, Setúbal, Portugal
96.8km (60.1 miles) ⓘMasa Valverde Mine (Valverde Mine), Beas, Huelva, Andalusia, Spain
References
Serranti, S.; Ferrini, V.; Masi, U.; Cabri, L. J. (2002) Trace-element distribution in cassiterite and sulfides from rubané and massive ores of the Corvo deposit, Portugal. The Canadian Mineralogist, 40 (3). 815-835 doi:10.2113/gscanmin.40.3.815
Relvas, J. M.R.S., Barriga, F. J.A.S., Ferreira, A., Noiva, P. C., Pacheco, N., Barriga, G. (2006) Hydrothermal Alteration and Mineralization in the Neves-Corvo Volcanic-Hosted Massive Sulfide Deposit, Portugal. I. Geology, Mineralogy, and Geochemistry. Economic Geology, 101 (4) 753-790 doi:10.2113/gsecongeo.101.4.753
 
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