| Locality type: | Prospect |
| Classification |
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| Species: | Muscovite |
| Formula: | KAl2(AlSi3O10)(OH)2 |
| Confirmation |
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|
| Validity: | Believed Valid |
| Data |
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| Mineral Data: | Click here to view Muscovite 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: | 1234824 |
| Long-form Identifier: | 1:3:1234824:0 |
| GUID (UUID V4): | 76702627-6bda-47de-80f2-190dad09d849 |
| Nearest other occurrences of Muscovite |
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|
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| 2.3km (1.4 miles) | ⓘCovăsinţ, Highiş Massif, Arad County, Romania |
| 30.9km (19.2 miles) | ⓘTalagiu Cu-Au deposit, Chisindia, Arad County, Romania |
| 79.7km (49.5 miles) | ⓘMusariu Cu-Au deposit, Mustari, Brad, Hunedoara County, Romania |
| 83.5km (51.9 miles) | ⓘValea Morii prospect (Valei Morii prospect), Crișcior, Hunedoara County, Romania |
| 83.7km (52.0 miles) | ⓘCofu Cu deposit, Oțelu Roșu, Caraş-Severin County, Romania |
| 86.3km (53.6 miles) | ⓘPestera din Valea Rea, Pietroasa, Bihor County, Romania |
| 93.0km (57.8 miles) | ⓘDeva Mine, Deva, Hunedoara County, Romania |
| 93.2km (57.9 miles) | ⓘDelineşti deposit, Brebu, Caraş-Severin County, Romania |
| 93.5km (58.1 miles) | ⓘVoia Cu deposit, Băița, Hunedoara County, Romania |
| 99.3km (61.7 miles) | ⓘMarga Hill, Marga, Caraş-Severin 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) |
|---|
 | 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... amphibolite gneiss, metagabbro, and various muscovite–biotite– chlorite–actinolite–feldspar–quartz schists...Pagoni Rachi, Maronia, Stypsi, Perama Hill), sheeted vein (e.g., Xanthi), carbonate replacement (e.g., Madem...Shear-zone hosted deposits in the Serbomacedonian Massif part of the province occur in four general areas |
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