Locality type: | Prospect |
Classification |
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Species: | Quartz |
Formula: | SiO2 |
Confirmation |
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Validity: | Believed Valid |
Data |
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Mineral Data: | Click here to view Quartz data |
Locality Data: | Click here to view Şoimuş Ilii vein, Highiş Massif, Arad County, Romania |
Data Identifiers |
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Mindat Occurrence Record ID: | 1234802 |
Long-form Identifier: | 1:3:1234802:8 |
GUID (UUID V4): | c2d36e80-c8e2-412e-a5e4-886b1aff84aa |
Nearest other occurrences of Quartz |
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2.3km (1.4 miles) | ⓘCovăsinţ, Highiş Massif, Arad County, Romania |
70.8km (44.0 miles) | ⓘBăiţa mining district, Nucet, Bihor County, Romania |
77.5km (48.2 miles) | ⓘTincova Cu deposit, Valisor–Tincova, Constantin Daicoviciu, Caraş-Severin County, Romania |
79.5km (49.4 miles) | ⓘAleului Valley, Pietroasa, Bihor County, Romania |
79.7km (49.5 miles) | ⓘMusariu Cu-Au deposit, Mustari, Brad, Hunedoara County, Romania |
84.0km (52.2 miles) | ⓘValea Rea skarn, Pietroasa, Bihor County, Romania |
86.3km (53.6 miles) | ⓘPestera din Valea Rea, Pietroasa, Bihor County, Romania |
87.0km (54.0 miles) | ⓘRusca Montană mining area, Rusca Montană, Caraş-Severin County, Romania |
91.8km (57.1 miles) | ⓘTrestia Mine, Trestia, Băița, Hunedoara County, Romania |
93.1km (57.8 miles) | ⓘMăgura veins, Certeju de Sus, Hunedoara County, Romania |
References |
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Ciobanu, C. L., Cook, N. J., Damian, F., & Damian, G. (2006). Gold scavenged by bismuth melts: An example from Alpine shear-remobilizates in the Highiş Massif, Romania. Mineralogy and Petrology, 87(3-4), 351-384. |
Reference Search (possible matching items) |
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| Bristol, Samantha K., Spry, Paul G., Voudouris, Panagiotis Ch., Melfos, Vasilios, Mathur, Ryan D., Fornadel, Andrew P., Sakellaris, Gregory Aarne (2015) Geochemical and geochronological constraints on the formation of shear-zone hosted Cu–Au–Bi–Te mineralization in the Stanos area, Chalkidiki, northern Greece. Ore Geology Reviews, 66. 266-282 doi:10.1016/j.oregeorev.2014.11.001 | Journal (article/letter/editorial) | the Proterozoic- to Silurian-aged Serbomacedonian Massif, which tectonically borders the Mesozoic CircumRhodope...to the west and crystalline rocks of the Rhodope Massif to the east. This area contains the Paliomylos...muscovite–biotite– chlorite–actinolite–feldspar–quartz schists of the Silurian Vertiskos Unit. Metallic...aggregates along foliation planes and in boudinaged quartz veins. Iron-bearing sulfides (pyrite, arsenopyrite...primary aqueous liquid–vapor inclusions in stage I quartz veins range from 170.1 °C to 349.6 °C (peak at |
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