J 2008

Ore minerals from the dolomitic veins in the serpentinite rocks of the Letovice crystalline complex (Czech Republic)

FOJT, Bohuslav, Pavel DOBEŠ, Karel MALÝ a Radek ŠKODA

Základní údaje

Originální název

Ore minerals from the dolomitic veins in the serpentinite rocks of the Letovice crystalline complex (Czech Republic)

Název česky

Ore minerals from the dolomitic veins in the serpentinite rocks of the Letovice crystalline complex (Czech Republic)

Autoři

FOJT, Bohuslav (203 Česká republika, garant), Pavel DOBEŠ (203 Česká republika), Karel MALÝ (203 Česká republika) a Radek ŠKODA (203 Česká republika)

Vydání

Mineralogia Polonica - Special Papers, Kraków, Wydawnictwo Naukowe "Akapit" 2008, 1896-2203

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10500 1.5. Earth and related environmental sciences

Stát vydavatele

Česká republika

Utajení

není předmětem státního či obchodního tajemství

Kód RIV

RIV/00216224:14310/08:00036894

Organizační jednotka

Přírodovědecká fakulta

Klíčová slova anglicky

bornite; chalcocite; covellite; millerite; parkerite; wittichenite; Letovice; Czech Republic

Příznaky

Mezinárodní význam, Recenzováno
Změněno: 8. 4. 2010 17:42, doc. Mgr. Radek Škoda, Ph.D.

Anotace

ORIG CZ

V originále

Minerals found in dolomite veins cutting serpentine rocks around Letovice and its surroundings composed remarkably heterogeneous set which is different from any other locality in the Bohemian Massif. The composition of copper minerals (bornite, chalcocite, covellite, chalcopyrite), millerite, dolomite veins and magnetite is similar to the composition of their host ultrabasic rocks. Lead and bismuth (galena, native Bi) are considered in this environment as atypical. Parkerite and wittichenite are transitional - they consist of elements of both groups.

Česky

Minerals found in dolomite veins cutting serpentine rocks around Letovice and its surroundings composed remarkably heterogeneous set which is different from any other locality in the Bohemian Massif. The composition of copper minerals (bornite, chalcocite, covellite, chalcopyrite), millerite, dolomite veins and magnetite is similar to the composition of their host ultrabasic rocks. Lead and bismuth (galena, native Bi) are considered in this environment as atypical. Parkerite and wittichenite are transitional - they consist of elements of both groups.