A New Model of a Unique Schlema-Alberoda Five-Element Deposit, Federal Republic of Germany


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Abstract

The paper completes a series of works about the unique Schlema-Alberoda deposit. The data on sources of vein and ore minerals and their relation to the processes of regressive alteration of rocks from the contact metamorphism zone are refined. The correlation between stages of mineral formation and their directed change are shown. A general scheme for the sequences in formation stages of the deposit’s hydrothermal ores is oriented on a joint analysis of geological and mineralogical–geochemical evolution of potentially ore-bearing provinces.

About the authors

G. B. Naumov

Vernadsky State Geological Museum, Russian Academy of Sciences

Email: olgamir18@mail.ru
Russian Federation, Moscow, 125009

B. P. Vlasov

Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry,
Russian Academy of Sciences

Email: olgamir18@mail.ru
Russian Federation, Moscow, 119017

O. F. Mironova

Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences

Author for correspondence.
Email: olgamir18@mail.ru
Russian Federation, Moscow, 119991

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