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A new model of a unique Schlema-Alberoda five-element deposit, Federal Republic of Germany

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1. Title Title of document A new model of a unique Schlema-Alberoda five-element deposit, Federal Republic of Germany
2. Creator Author's name, affiliation, country G. B. Naumov; Vernadsky State Geological Museum, Russian Academy of Sciences; Russian Federation
2. Creator Author's name, affiliation, country B. P. Vlasov; Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry, Russian Academy of Sciences; Russian Federation
2. Creator Author's name, affiliation, country O. F. Mironova; Vernadsky Institute of Geochemistry and Analytical Chemistry of the Russian Academy of Sciences; Russian Federation
3. Subject Discipline(s)
3. Subject Keyword(s) hydrothermal deposits; retrograde metamorphism; stages of mineralization; forming model
4. Description Abstract

This article concludes a series of works detailed the data on the Schlema-Alberoda unique deposit in order of sources of ore and gangue minerals, their association with retrograde metamorphism of rocks from the contact metamorphism zone. The relationship of stages of mineral formation is presents, as well as, their directed replacement. A general scheme of formation stages of hydrothermal ores is given, which results the joint analysis of geological and geochemical evolution of potentially ore-bearing provinces.

5. Publisher Organizing agency, location The Russian Academy of Sciences
6. Contributor Sponsor(s)
7. Date (DD-MM-YYYY) 17.12.2019
8. Type Status & genre Peer-reviewed Article
8. Type Type Research Article
9. Format File format
10. Identifier Uniform Resource Identifier https://journals.eco-vector.com/0016-7770/article/view/18715
10. Identifier Digital Object Identifier (DOI) 10.31857/S0016-777061658-66
10. Identifier Digital Object Identifier (DOI) (PDF (Rus)) 10.31857/S0016-777061658-66-15079
11. Source Title; vol., no. (year) Геология рудных месторождений; Vol 61, No 6 (2019)
12. Language English=en ru
13. Relation Supp. Files FIG. 1. The average thickness of the quartz (solid line) and carbonate (dashed) components in large veins intersecting the rocks of the main (a) and acid (b) compositions. Horizontal indicates the distance from the contact of the rocks, vertical - the power of the corresponding mineralization. (8KB) doi: 10.31857/S0016-777061658-66-18021
FIG. 2. Distribution of quartz and carbonate in small veins. 1 - quartz-micaceous schists; 2 - amphibole schists; 3 - quartz; 4 - carbonate. (19KB) doi: 10.31857/S0016-777061658-66-18022
FIG. 3. The results of mass testing of the host rocks of the deposit, placed on a profile perpendicular to the roof of granite. V - coefficient of variation V = ( / хср) • 100%. (28KB) doi: 10.31857/S0016-777061658-66-18023
FIG. 4. The structure of quartz-nasturan-calcite (kku) veins. a - a photograph of a core; b - a schematic drawing. 1 - rock, 2 - comb quartz, 3 - nasturan, 4 - calcite. (67KB) doi: 10.31857/S0016-777061658-66-18024
FIG. 5. Calcite scalehedron replaced by dolomite (in section). Dark - voids filled with hematite, sulfides, sulfosalts, arsenic, etc. (331KB) doi: 10.31857/S0016-777061658-66-18025
FIG. 6. Mutual intersections of four kku-veins. Roman numerals denote veins of the same age of the same stage in the order of their formation. Sketch of the roof, mountains. 990 (According to Barsukov, Vict. L. et al., 1991). (32KB) doi: 10.31857/S0016-777061658-66-18026
FIG. 7. The sequence diagram of the stages of hydrothermal formation of the Shlema-Alberoda deposit (a) and their layouts (b). (64KB) doi: 10.31857/S0016-777061658-66-18027
14. Coverage Geo-spatial location, chronological period, research sample (gender, age, etc.)
15. Rights Copyright and permissions Copyright (c) 2019 Russian academy of sciences