| Reference Type | Journal (article/letter/editorial) |
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| Title | Mineralogická charakteristika granátického skarnu z lokality Trohanka pri Prakovciach (gemerikum, Slovenská republika)
[Mineralogical characteristics of a garnet skarn from the Trohanka locality near Prakovce (Gemeric Unit, Slovak Republic)] |
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| Journal | Bulletin Mineralogie Petrologie |
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| Authors | Myšľan, Pavol | Author |
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| Ružička, Peter | Author |
| Števko, Martin | Author |
| Mikuš, Tomáš | Author |
| Year | 2021 | Volume | 29 |
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| Issue | 2 |
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| Publisher | Bulletin Mineralogie Petrologie |
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| URL | |
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| Download URL | http://www.bullmineral.cz/paper/download/289/fulltext |
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| DOI | doi:10.46861/bmp.29.230Search in ResearchGate |
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| Generate Citation Formats |
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| Original Entry | |
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| Languages | Slovak |
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| Classification | Not set | LoC | Not set |
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| Mindat Ref. ID | 16094053 | Long-form Identifier | mindat:1:5:16094053:0 |
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| GUID | 0 |
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| Full Reference | Myšľan, Pavol, Ružička, Peter, Števko, Martin, Mikuš, Tomáš (2021) Mineralogická charakteristika granátického skarnu z lokality Trohanka pri Prakovciach (gemerikum, Slovenská republika) [Mineralogical characteristics of a garnet skarn from the Trohanka locality near Prakovce (Gemeric Unit, Slovak Republic)]. Bulletin Mineralogie Petrologie, 29 (2) 230-240 doi:10.46861/bmp.29.230 |
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| Plain Text | Myšľan, Pavol, Ružička, Peter, Števko, Martin, Mikuš, Tomáš (2021) Mineralogická charakteristika granátického skarnu z lokality Trohanka pri Prakovciach (gemerikum, Slovenská republika) [Mineralogical characteristics of a garnet skarn from the Trohanka locality near Prakovce (Gemeric Unit, Slovak Republic)]. Bulletin Mineralogie Petrologie, 29 (2) 230-240 doi:10.46861/bmp.29.230 |
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| In | (2021) Bulletin Mineralogie Petrologie Vol. 29 (2) Mgr. Jiří Sejkora |
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| Abstract/Notes | Garnet skarn mineralization was recently studied at the Trohanka locality near Prakovce (Gemeric Unit, Eastern Slovakia). Ca-skarn forms lenticular bodies in green schist environment. It mainly consists of zonal garnets, pyroxenes, amphiboles and magnetite accumulations. Studied garnets are rich in andradite component (up to 89.95 mol. %) with minor grossular component (6.83 - 39.67 mol. %). Strong oscillatory zoning in andradite is caused by substitution of Fe3+ and Al3+. Most pyroxenes are rich in the hedenbergite component. In some cases, euhedral diopside crystals with marginal transition zones (composed of diopside with lower content of Mg2+ and higher content of Fe2+) were found in hedenbergite matrix. Amphiboles are dominantly represented by ferro-actinolite and ferro-hornblende in association with isolated euhedral crystals of ferro-tschermakite and ferro-pargasite. Indistinct chemical zonality of amphibole euhedral crystals is caused by presence of ferro-pargasite in the central parts and ferro-tschermakite in the peripheral parts of crystals. |
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