PUKLINOVÁ MINERALIZACE ALPSKÉHO TYPU V METAGRANITOIDECH NA ŠPIČÁKU U VERNÍŘOVIC
Roč.7,(2000)
Abstrakt
Klíčová slova:
Desná Crystalline Complex; metagranitoids; Alpine-type veins; mineralogy
The mineralization of the Alpine-type has been found in metagranitoids that outcrop at the locality Špičák near Vernířovice in the Desná Crystalline Complex. The Alpine-type mineralization occurs here chiefly as veinlets composed mainly of chlorite but also as a typical fissure-mineralization composed of prehnite, K-feldspar, calcite, epidote, albite, quartz and chlorite of the clinochlorechamosite series. The studied fissure-mineralization is very similar to that in amphibolites and related rocks of the Sobotín Massif.
Desná Crystalline Complex; metagranitoids; Alpine-type veins; mineralogy