| Locality type: | Village |
| Classification |
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| Species: | 'Chlorite Group' (not an IMA approved species) |
| Confirmation |
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| Validity: | Believed Valid |
| Data |
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| Mineral Data: | Click here to view Chlorite Group data |
| Locality Data: | Click here to view Dobromirtsi, Kirkovo Municipality, Kardzhali Province, Bulgaria |
| Data Identifiers |
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| Mindat Occurrence Record ID: | 1321263 |
| Long-form Identifier: | 1:3:1321263:2 |
| GUID (UUID V4): | a8634855-059f-4509-9ce6-5104a5b025a1 |
| Nearest other occurrences of Chlorite Group |
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| 22.2km (13.8 miles) | ⓘBorieva Mine, Madan Municipality, Smolyan Province, Bulgaria |
| 23.9km (14.8 miles) | ⓘPcheloyad mine, Pcheloyad, Krumovgrad Municipality, Kardzhali Province, Bulgaria |
| 35.3km (21.9 miles) | ⓘGorgona, Myki, Xanthi, Eastern Macedonia and Thrace, Greece |
| 38.0km (23.6 miles) | ⓘAda Tepe Au deposit, Krumovgrad Municipality, Kardzhali Province, Bulgaria |
| 41.8km (26.0 miles) | ⓘStremtsi, Kardzhali Municipality, Kardzhali Province, Bulgaria |
| 60.4km (37.6 miles) | ⓘLaki tailings dam, Laki, Laki Municipality, Plovdiv Province, Bulgaria |
| 61.2km (38.1 miles) | ⓘKassiteres-Sapes area, Maroneia-Sapes, Rhodope, Eastern Macedonia and Thrace, Greece |
| 61.4km (38.2 miles) | ⓘMadzharovo deposit, Madzharovo, Madzharovo Municipality, Haskovo Province, Bulgaria |
| 65.1km (40.5 miles) | ⓘMaroneia, Maroneia-Sapes, Rhodope, Eastern Macedonia and Thrace, Greece |
| 65.3km (40.6 miles) | ⓘRuby occurrence, Paranesti, Drama, Eastern Macedonia and Thrace, Greece |
| References |
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Jiménez, J. M. G., Kerestedjian, T., Fernández, J. A. P., & Linares, F. G. (2009). Metamorphism on chromite ores from the Dobromirtsi ultramafic massif, Rhodope mountains (SE Bulgaria). Geologica Acta, 7(4), 413-429. |
| Reference Search (possible matching items) |
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 | Borojević Šoštarić, S., Palinkaš, A.L., Neubauer, F., Cvetković, V., Bernroider, M., Genser, J. (2014) The origin and age of the metamorphic sole from the Rogozna Mts., Western Vardar Belt: New evidence for the one-ocean model for the Balkan ophiolites. Lithos, 192. 39-55 doi:10.1016/j.lithos.2014.01.011 | Journal (article/letter/editorial) | | serpentinite nappe and consists of amphibolites and talc-chlorite schists. The Rogozna amphibolites are medium-...containing actinolite, epidote, clinoclore, sericite, chlorite, and magnetite. The amphibolites formed due to...Ma, slightly postdate the sole formation. Talc-chlorite schists are related to retrograde greenschist-facies...metamorphism. They consist of Fe-rich talc and Cr-rich chlorite (peninite-diabantite) pseudomorphs after amphibole...related to earlier, amphibolite facies metamorphism. Chlorite pseudomorphs after amphibole were formed at 300–410 |  | | Book | | Innovative and Applied Research on Platinum-Group and Rare Earth Elements Dedicated to the Work and Memory...Platinum-Group and Rare Earth Elements Innovative and Applied Research on Platinum-Group and Rare...Issue “Innovative and Applied Research on Platinum-Group and Rare Earth Elements” Reprinted from: Minerals...Nikolay V. Bryansky and Nikolay V. Smagunov Platinum Group Elements in Arsenopyrites and Pyrites of the Natalkinskoe...Universities of Europe was mainly focused on the platinum-group elements in mafic-ultramafic rocks and associated |  | | Report (volume) | | Gonzalez-Jimenez (2016) provide an overview of platinum-group minerals (PGM), pointing out that, where present...(1985) The origin of the fractionation of platinum-group elements in terrestrial magmas. Chem Geol 53:302–323...González-Jiménez J (2016) Petrogenesis of the platinum-group minerals. Rev Mineral Geochem 81:489–578 Parrington...(2008) Environmental relevance of the platinum-group elements. Elements 4, 259–263 Rosenberg B, VanCamp...Origin of the base metal sulfides and platinum group minerals ................................315 HIGHLY |
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