Minerals of antimony: a newly found occurrence in the Karkonosze granitoid pluton and a review for Lower Silesia, Poland, with general background

Kozłowski, Andrzej; Marcinowska, Agnieszka

doi:10.24425/agp.2024.150011

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Tytuł artykułu

Minerals of antimony: a newly found occurrence in the Karkonosze granitoid pluton and a review for Lower Silesia, Poland, with general background

Autorzy

Kozłowski Andrzej , Marcinowska Agnieszka

Treść / Zawartość

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Identyfikatory

DOI

10.24425/agp.2024.150011

Warianty tytułu

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Abstrakty

The article describes assemblages of ore minerals of the size of tenths to a few millimetres, which occurred in small quartz veinlets and nests in 10 previously unknown sites. This mineralization was found in the north-eastern part of the Karkonosze granitoid pluton at the southern slope of the Wysoki Grzbiet (High Ridge) in Izera Mts. The studies concerned mainly 18 Sb minerals: antimony, Sb-bearing domeykite, getchellite, stibnite, willyamite, berthierite, boulangerite, bournonite, chalcostibite, falkmanite, famatinite, geocronite, robinsonite, semseyite, tetrahedrite-(Fe), cervantite, kermesite and schafarzikite; seven of them have been found in Poland for the first time. The parageneses, morphological features, XRD data and chemical composition of the Sb minerals are presented. Fluid inclusions in quartz adhering to the Sb minerals had generally homogenization temperature (Th) 108–341°C and total salinity ΣS 4.6–10.1 wt. %. The inclusion fluids were of the NaCO3-Ca(HCO3)2-NaCl-KCl type with minor F and S, and occasional CO2 presence. The parent granitoid contains Sb in trace amounts (0.18–0.36 ppm) and the rock was possibly a source of this (and other) element(s) for the ore minerals. Migration of meso-epithermal solutions with Sb etc. was probably stimulated by local reduction of pressure during the formation of fissures and cracks in granite, next filled by quartz with ore minerals. The features of the historical process of the recognition of Sb ores and previous studies of the minerals investigated in this research are included in the presentation and discussion. Special attention was paid to the listing of the occurreences of Sb minerals in Lower Silesia with appropriate references.

Słowa kluczowe

minerals Fluid inclusions Granitoid Karkonosze pluton Lower Silesia

minerały wtrącenia płynne inkluzja fluidalna granitoidy Karkonosze Województwo dolnośląskie

Wydawca

Faculty of Geology of the University of Warsaw
Komitet Nauk Geologicznych PAN

Czasopismo

Acta Geologica Polonica

Rocznik

2024

Tom

Vol. 74, no. 3

Strony

art. no. e17

Opis fizyczny

Bibliogr. 289 poz., rys., tab.

Twórcy

autor

Kozłowski Andrzej

a.j.kozlowski@uw.edu.pl

University of Warsaw, Faculty of Geology

autor

Marcinowska Agnieszka

amarcinowska@uw.edu.pl

University of Warsaw, Faculty of Geology
University of Gdańsk, Faculty of Oceanography and Geography

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Opracowanie rekordu ze środków MNiSW, umowa nr POPUL/SP/0154/2024/02 w ramach programu "Społeczna odpowiedzialność nauki II" - moduł: Popularyzacja nauki (2026).

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Bibliografia

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