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Poland | |
- Lower Silesian Voivodeship
| Wojtulek, Piotr Marian, Puziewicz, Jacek, Ntaflos, Theodoros, Bukała, Michał (2016) Podiform chromitites from the Variscan ophiolite serpentinites of Lower Silesia (SW Poland): petrologic and tectonic setting implications. Geological Quarterly, 60. |
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| Gil, G., Borowski, M. P., Barnes, J. D., Jokubauskas, P., Bagiński, B., Gunia, P., & Ilnicki, S. (2022). Formation of serpentinite-hosted talc in a continental crust setting: Petrographic, mineralogical, geochemical, and O, H and Cl isotope study of the Gilów deposit, Góry Sowie Massif (SW Poland). Ore Geology Reviews, 146, 104926.
Dera, P., Rapp, R., Chornkrathok, S., Zhang, D., Prakapenka, V.B., Woźniak, K. (2023). New high-pressure phase of CaSiO3 wollastonite with penta-coordinated silicon. 9th Meeting of the Mineralogical Society of Poland / 28th Meeting of the Petrology group of the Mineralogical Society of Poland, "Oceanic lithosphere: rocks, minerals, and critical resources", October 19-22, Bielawa, Poland. Mineralogia - Special Papers, 51, 51. |
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| Dathe, E. (1902) - Geologische Karte von Preußen und benachbarten deutschen Ländern 1:25000. Blatt [Neue Nr. 5365]
Langenbielau [Bielawa]
Lieferung 115
Preußische Geologische Landesanstalt Berlin. |
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| Lis, Józef, Sylwestrzak, Hubert (1986) Minerały Dolnego Śląska [Minerals of the Lower Silesia]. Wydawnictwa Geologiczne, Warszawa. p.1-791. |
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| Gil, Grzegorz, Gunia, Piotr, Barnes, Jaime D., Szymański, Michał, Jokubauskas, Petras, Kalbarczyk-Gil, Anna, Bagiński, Bogusław (2019) Origin of Talc and Fe-Ti-V Mineralization in the Kletno Deposit (the Śnieżnik Massif, SW Poland) Minerals, 10 (1) 13 doi:10.3390/min10010013 |
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| Harańczyk C., Wala A. (1970) Mineralizacja endogeniczna w masywach skał ultrazasadowych północnego przedpola Sudetów Środkowych. Przegląd Geologiczny nr 6. (In Polish) |
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| Finckh L. (1919) Geologische Karte von Preußen und benachbarten deutschen Ländern. Blatt 5165 Weizenrodau. Geologisch bearbeitet 1912. Preuss. Geologische Landesanstalt Berlin. |
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| Lis, Józef, Sylwestrzak, Hubert (1986) Minerały Dolnego Śląska [Minerals of the Lower Silesia]. Wydawnictwa Geologiczne, Warszawa. p.1-791. |
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| Lis, Józef, Sylwestrzak, Hubert (1986) Minerały Dolnego Śląska [Minerals of the Lower Silesia]. Wydawnictwa Geologiczne, Warszawa. p.1-791. |
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| Wiewiora, Andrzej, Rausell-colom, Jose A., Garcia-gonzalez, Teresa (1991) The crystal structure of amesite from Mount Sobotka: A nonstandard polytype. American Mineralogist, 76 (3-4) 647-652 |
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| Wojtulek, Piotr Marian, Puziewicz, Jacek, Ntaflos, Theodoros, Bukała, Michał (2016) Podiform chromitites from the Variscan ophiolite serpentinites of Lower Silesia (SW Poland): petrologic and tectonic setting implications. Geological Quarterly, 60. |
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| Pieczka, A., Biagioni, C., Gołębiowska, B., Jeleń, P., Pasero, M., & Sitarz, M. (2018). Parafiniukite, Ca2Mn3 (PO4) 3Cl, a New Member of the Apatite Supergroup from the Szklary Pegmatite, Lower Silesia, Poland: Description and Crystal Structure. Minerals, 8(11), 485.
Szuszkiewicz, Adam, Adam Pieczka, Bożena Gołębiowska, Magdalena Dumańska-Słowik, Mariola Marszałek, and Eligiusz Szełęg. (2018) "Chemical Composition of Mn- and Cl-Rich Apatites from the Szklary Pegmatite, Central Sudetes, SW Poland: Taxonomic and Genetic Implications" Minerals 8, no. 8: 350. https://doi.org/10.3390/min8080350
Pieczka, A., Evans, R. J., Grew, E. S., Groat, L. A., Ma, C., & Rossman, G. R. (2013). The dumortierite supergroup. II. Three new minerals from the Szklary pegmatite, SW Poland: Nioboholtite,(Nb0. 6⃞0. 4) Al6BSi3O18, titanoholtite,(Ti0. 75⃞0. 25) Al6BSi3O18, and szklaryite, ⃞Al6BAs33+ O15. Mineralogical Magazine, 77(6), 2841-2856. |
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| Kaczan, W., Kudełko, J., Wirth, H. (2021) Szklary nickel deposit — a review and introduction to attempts in hydrometallurgical processing. Mineral Economics, 34, 315-322.
Pieczka, A., & Gołębiowska, B. (2001). Altered pyrochlore from the Szklary rare-element pegmatite, Lower Silesia, Poland. In Mineral Deposits at the Beginning of the 21 st Century. Proceedings of the Joint sixth Biennial SGA-SEG Meeting (pp. 469-472). |
