2015
Metamorphosed gold deposit from Orlik near Humpolec, Czech Republic
BUŘIVAL, Zbyněk a Lenka LOSERTOVÁZákladní údaje
Originální název
Metamorphosed gold deposit from Orlik near Humpolec, Czech Republic
Autoři
BUŘIVAL, Zbyněk a Lenka LOSERTOVÁ
Vydání
13TH SGA BIENNAL MEETING NANCY - FRANCE, 2015. 2015
Další údaje
Jazyk
angličtina
Typ výsledku
Prezentace na konferencích
Obor
10500 1.5. Earth and related environmental sciences
Stát vydavatele
Francie
Utajení
není předmětem státního či obchodního tajemství
Označené pro přenos do RIV
Ano
Kód RIV
RIV/00216224:14310/15:00084032
Organizační jednotka
Přírodovědecká fakulta
Klíčová slova anglicky
Humpolec; Orlik; gold; deposit; metamorphic; sulfides
Změněno: 28. 9. 2015 14:10, Mgr. Zbyněk Buřival, Ph.D.
Anotace
V originále
The paper presents mineralogic considerations about gold ores in the Orlik deposit (Czech Republic). Data have been obtained on samples coming from medieval pit. Studies of sulfidic ores revealed typical pyrrhotite-löllingite-arsenopyrite and gold textures. These aggregates were recently linked to certain conditions of LP/MP-HT metamorphic evolution. Documented textures confirm the premetamorphic origin of gold-bearing ores and serious remobilisation of gold. The conditions of older (~329 Ma) migmatite metamorphism with temperatures up to 730 oC and pressure about 6 kbar were sufficient to decompose premetamorphic gold bearing arsenopyrite and form löllingite-pyrrhotite assemblages with the younger generation of arsenopyrite and gold. Also significant remobilisation of gold and sulfides into wall rock was observed. Consequent periplutonic metamorphosis (~327 Ma) with only 500 oC and 2,5 kbars was too weak to significantly affect sulphidic textures, but might be connected with the the decomposition of maldonite into the gold-bismuth myrmekite structures and secondary Bi-minerals.