Locality type: | Deposit |
Classification |
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Species: | Muscovite var: Sericite |
Formula: | KAl2(AlSi3O10)(OH)2 |
Confirmation |
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Validity: | Believed Valid |
Data |
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Mineral Data: | Click here to view Sericite data |
Locality Data: | Click here to view Aktepe Deposit, Namangan Region, Uzbekistan |
Data Identifiers |
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Mindat Occurrence Record ID: | 1255009 |
Long-form Identifier: | 1:3:1255009:4 |
GUID (UUID V4): | 4780befd-3c9f-4c56-af66-f6c0618a9989 |
Nearest other occurrences of Sericite |
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23.1km (14.3 miles) | ⓘChadak mine, Namangan Region, Uzbekistan |
39.1km (24.3 miles) | ⓘKockbulak mine (Kochbulak Au-Ag-Te deposit), Ohangaron District, Tashkent Region, Uzbekistan |
65.8km (40.9 miles) | ⓘAdrasman Mine, Adrasmon (Adrasman), Ghafurov District, Sughd, Tajikistan |
72.6km (45.1 miles) | ⓘSary Cheku Mine, Ohangaron District, Tashkent Region, Uzbekistan |
77.1km (47.9 miles) | ⓘKyzata Mine, Piskent District, Tashkent, Uzbekistan |
81.1km (50.4 miles) | ⓘKalmakyr Mine (Almalyk Mine), Piskent District, Tashkent, Uzbekistan |
81.2km (50.5 miles) | ⓘKal'makyr ore body, Kalmakyr Mine (Almalyk Mine), Piskent District, Tashkent, Uzbekistan |
88.4km (54.9 miles) | ⓘSardob deposit, Altyn-Topkan ore field (Zarnisor ore field), Mastchoh District, Sughd, Tajikistan |
91.9km (57.1 miles) | ⓘBiryuzakan deposit, Ghafurov District, Sughd, Tajikistan |
92.9km (57.7 miles) | ⓘAltyn-Topkan deposit (Altyntopkan deposit; Altyn-Topkan Mine; Zarnisor deposit; Zarnisori Shimoli deposit; Northern Zarnisor deposit), Altyn-Topkan ore field (Zarnisor ore field), Mastchoh District, Sughd, Tajikistan |
References |
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Kovalenker, V. A., Rusinov, V. L., Kabo, A. E., & Jambor, J. L. (1995). The Aktepe silver-arsenide deposits, Uzbekistan. Exploration and Mining Geology, 2(4), 111-119. |
Reference Search (possible matching items) |
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| Volkov, V. N., Lebedev, V. А., Goltsman, Yu. V., Arakelyants, М. М., Golubev, V. N., Bairova, Е. D. (1999) Magmatic Associations and Ore Mineralization of the Aktepe Ore Field (Kuraminsk Ridge, Uzbekistan): Formation Sequence and Isotope Age. Geology of Ore Deposits, 41 (3) 238-251 | Journal (article/letter/editorial) | and Ore Mineralization of the Aktepe Ore Field (Kuraminsk Ridge, Uzbekistan): Formation Sequence and Isotope...Received OctoЬer 26, 1998 оп the territory of the Aktepe ore field were found to Ье formed as а result of...process related to the origin of the Aktepe silver-arsenide deposit. According to the data, the ore deposition...articles devoted to the description of the Aktepe silver-arsenide deposit this proЫem has not been considered...have studied the deposit, it was widely believed that the ore bodies of this deposit were derived from | | | Journal (article/letter/editorial) | and I. V. Chernyshev Institute of Geology of Ore Deposit[A1]s, Petrography, Mineralogy, and Geochemistry...central, and southern Asia (Sukhoi Log, Dukat, Aktepe, and Kolar); and North America (Kidd Creek). The...the mineral deposits discussed here Sample no. Deposit A2 Kremnica (Slovakia) A3 Banska Hodrusa...higher than 2–3 wt %. Silver from the Kongsberg deposit appeared to be poorest in the above impurity elements...phases were detected in a grain from the Karabash deposit (Fig. 1a): gold with high Ag content (18.8 wt %) | | Lebedev, V. I., Borovikov, A. A., Gushchina, L. V., Shabalin, S. I. (2019) Physicochemical Modeling of Hydrothermal Mineralization Processes at Ni–Co–As (±U–Ag), Co–S–As (±Au–W), and Cu–Co–As (±Sb–Ag) Deposits. Geology of Ore Deposits, 61 (3) 225-255 doi:10.1134/s107570151903005x | Journal (article/letter/editorial) | of Co-bearing ore clusters in the Central Asia region, western Mongolia, and northwestern Africa (Morocco)...(Central Tuva region), calcareous skarns with Co sulfoarsenides, 368–383 Ma (Ar–Ar sericite method) (Fig...Kharadzhul’ and Butrakhty (Khakassia), 409 Ma (Ar–Ar sericite method (Fig. 4); Cu– Co–W ores in hornfels, Kara-Kul’..., 1960), magnesian skarns of the Vladimirovka deposit are genetically related to gabbro–diorite of the...(D3–C1), while the absolute age of Co ores from this deposit, determined by the Re–Os method at the Analytical |
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