Mineralogy and geochemistry of Cu-Sn-Bi ores from the Miedzianka-Ciechanowice deposit, Sudety Mts., Poland

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00023272%3A_____%2F25%3A10136955" target="_blank" >RIV/00023272:_____/25:10136955 - isvavai.cz</a>

Výsledek na webu

<a href="https://gq.pgi.gov.pl/article/view/34281" target="_blank" >https://gq.pgi.gov.pl/article/view/34281</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.7306/gq.1782" target="_blank" >10.7306/gq.1782</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Mineralogy and geochemistry of Cu-Sn-Bi ores from the Miedzianka-Ciechanowice deposit, Sudety Mts., Poland

Popis výsledku v původním jazyce

Miedzianka-Ciechanowice is a hydrothermal vein-type quartz and quartz-carbonate-sulphide deposit in the eastern metamorphic cover of the Karkonosze Granite in the Sudeten Mts. Within this diverse deposit, polymetallic Cu-Sn-Bi mineralization was identified. Two ore mineral stages of precipitation were recognised: I - a high-temperaure mineralization stage in skarn; and II - a medium and low-temperature stage of vein mineralization. Stage I, associated with skarns, is represented by rutile, magnetite I and II, cassiterite and minor amounts of sulphides (sphalerite, pyrite, chalcopyrite and galena). Stage II, associated with quartz or quartz-carbonate veins, is represented by pyrrhotite, pyrite, arsenopyrite, cobaltite, gersdorffite, sphalerite, chalcopyrite, minerals of the tetrahedrite-group, roquesite, bornite and galena. In addition a wide range of tin sulphides: stannoidite, mawsonite, ferrokesterite and bismuth sulphosalts (bismuthinite, aikinite, ikunolite, gustavite, lillianite, heyrovskyite, vikingite, berryite and matildite) were identified. Minerals of the Cu-Sn-Bi associations were formed mainly in massive aggregates of chalcopyrite in quartz veins, less of ten in magnetite or sphalerite in skarns. In the Sudeten Mts., the presence of various tin and bismuth associations is rare and usually represents accessory mineralization.

Název v anglickém jazyce

Mineralogy and geochemistry of Cu-Sn-Bi ores from the Miedzianka-Ciechanowice deposit, Sudety Mts., Poland

Popis výsledku anglicky

Miedzianka-Ciechanowice is a hydrothermal vein-type quartz and quartz-carbonate-sulphide deposit in the eastern metamorphic cover of the Karkonosze Granite in the Sudeten Mts. Within this diverse deposit, polymetallic Cu-Sn-Bi mineralization was identified. Two ore mineral stages of precipitation were recognised: I - a high-temperaure mineralization stage in skarn; and II - a medium and low-temperature stage of vein mineralization. Stage I, associated with skarns, is represented by rutile, magnetite I and II, cassiterite and minor amounts of sulphides (sphalerite, pyrite, chalcopyrite and galena). Stage II, associated with quartz or quartz-carbonate veins, is represented by pyrrhotite, pyrite, arsenopyrite, cobaltite, gersdorffite, sphalerite, chalcopyrite, minerals of the tetrahedrite-group, roquesite, bornite and galena. In addition a wide range of tin sulphides: stannoidite, mawsonite, ferrokesterite and bismuth sulphosalts (bismuthinite, aikinite, ikunolite, gustavite, lillianite, heyrovskyite, vikingite, berryite and matildite) were identified. Minerals of the Cu-Sn-Bi associations were formed mainly in massive aggregates of chalcopyrite in quartz veins, less of ten in magnetite or sphalerite in skarns. In the Sudeten Mts., the presence of various tin and bismuth associations is rare and usually represents accessory mineralization.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10504 - Mineralogy

Projekt

—

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2025

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Geological Quarterly

ISSN

1641-7291

e-ISSN

—

Svazek periodika

69

Číslo periodika v rámci svazku

1

Stát vydavatele periodika

PL - Polská republika

Počet stran výsledku

6

Strana od-do

1-16

Kód UT WoS článku

001525634400003

EID výsledku v databázi Scopus

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