 | Bačík, Peter, Dikej, Jakub, Fridrichová, Jana, Miglierini, Marcel, Števko, Martin (2017) Chemical composition and evolution of tourmaline-supergroup minerals from the Sb hydrothermal veins in Rožňava area, Western Carpathians, Slovakia. Mineralogy and Petrology, 111 (4) 609-624 doi:10.1007/s00710-017-0507-1 | Journal (article/letter/editorial) | | the Sb hydrothermal veins in Rožňava area, Western Carpathians, Slovakia Peter Bačík 1 & Jakub Dikej...veins on Betliar – Straková, Čučma – Gabriela and Rožňava – Peter-Pavol vein deposits in the Rožňava area...area, Slovakia. Tourmaline-supergroup minerals form relatively large prismatic to radial aggregates of parallel...Tourmaline-supergroup minerals from Betliar – Straková and Rožňava – Peter-Pavol are almost homogeneous...Fe)Na−1Al−1 and X□AlNa −1(Mg,Fe)−1. Betliar – Straková and Rožňava – Peter-Pavol tourmaline-supergroup |  | | Book | | Ľubietová-Podlipa, DO strana 5: Tetraedrit, xx 10mm, Rožňava, DP strana 6: Bari!- wolnýn, xx 20mm, Rožiiava...Okruhlicovi (Banská Bystrica) a Jozefovi Molnárovi (Košice), Bohuslavovi Burešovi (Praha), Lubomírovi Mlčochovi...zbierok kfotodokumentácii: Dušanovi Petercovi (Košice), Albertovi Russovi, Martinovi Števkovi, Petrovi...Kotuľakovi, Jozefovi Salanarovi a Jozefovi Molnárovi (Košice), Norbertovi Hesounovi (Banská Štiavnica) a Michalovi...akciová spoločnost'. Jelšava; MONTANA Košice, spol. s r.o., Košice; Ludovika Energy, s.1:0., Spišská Nová |  | Jerzykowska, Irena, Majzlan, Juraj, Michalik, Marek, Göttlicher, Jörg, Steininger, Ralph, Błachowski, Artur, Ruebenbauer, Krzysztof (2014) Mineralogy and speciation of Zn and As in Fe-oxide-clay aggregates in the mining waste at the MVT Zn–Pb deposits near Olkusz, Poland. Geochemistry, 74 (3) 393-406 doi:10.1016/j.chemer.2014.03.003 | Journal (article/letter/editorial) | | deposit Sulfide MVT deposits in the Cracow–Silesia region are hosted by the Triassic carbonate rocks of the...al., 2009) occur rarely. Mining activity in the region Olkusz was carried out with brief interruptions...eV in the region from −150 to −50 eV relative to the absorption edge, of 2 eV in the region from −50 eV...(Cabala and Teper, 2007; Cabała et al., 2009) and quartz grains. The results of bulk chemical analyses are...LOI = loss on ignition. 14aI pH (H2O) dolomite quartz smithsonite hemimorphite clays goethite Mn oxides |  | | Journal (article/letter/editorial) | | within the Neoproterozoic rocks. Five generations of quartz veins, referred to as Q0 through Q4 were distinguished:...veins its culmination and Q3 veins its fading. Late quartz gangue (Q 4) is associated with uneconomic Ag–Pb–Zn...vein-type ores hosted by calcite–barite–(quartz) veins. Quartz vein thickness (~0.3 to ~300 mm), spacing...3–25%) evolve systematically across the studied ore district, reflecting both the major host rock and other...analogous to the J1 joints prior to the formation of quartz veins. The formation of the Q1–2 veins at the Mokrsko-East |  | | Book | | casts (FIG. 1.38) of the hollow pith or medullary region in calamites and preserve an impression of the...different mechanisms were involved, depending on the region and the location of the coal balls within the coal...(Chapter 3). In another study on fluid inclusions in quartz from the 3.5 Ga Dresser Formation (North Pole)...hyphae that are distinctly septate, with the central region of the septum slightly thickened (Kidston and Lang...becomes intracellular only within a well-defined region of the cortex where it forms arbuscules. The fungus |
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