Typomorphic Features of Placer Gold from the Billyakh Tectonic Melange Zone of the Anabar Shield and Its Potential Ore Sources (Northeastern Siberian Platform)
| Autor: | Vasily Beryozkin, Alexander Kravchenko, Boris Gerasimov |
|---|---|
| Jazyk: | angličtina |
| Rok vydání: | 2020 |
| Předmět: |
Placer mining
Mineralization (geology) Provenance primary source lcsh:QE351-399.2 Pluton Geochemistry Mélange mineral inclusions 010502 geochemistry & geophysics 01 natural sciences Petrography Precambrian metasomatosis Prospecting typomorphism of native gold 0105 earth and related environmental sciences Anabar shield lcsh:Mineralogy disseminated gold-sulfide mineralization Billyakh zone 010401 analytical chemistry Geology Geotechnical Engineering and Engineering Geology 0104 chemical sciences |
| Zdroj: | Minerals Volume 10 Issue 3 Minerals, Vol 10, Iss 3, p 281 (2020) |
| ISSN: | 2075-163X |
| DOI: | 10.3390/min10030281 |
| Popis: | Precambrian shields and outcropped Precambrian rock complexes in the Arctic may serve as the most important sources of various types of mineral raw materials, including gold. The gold potential of the Anabar shield in the territory of Siberia has, thus far, been poorly studied. A number of primary and placer gold occurrences have been discovered there, but criteria for the prediction of and search for gold mineralization remain unclear. The main purpose of this paper was to study the typomorphic features of placer gold in the central part of the Billyakh tectonic mé lange zone in the Anabar shield and to compare them to mineralization from primary sources. To achieve this, we utilized common methods for mineralogical, petrographic, and mineragraphic analyses. Additionally, geochemical data were used. As a result of this investigation, important prospecting guides were identified, and essential criteria for the prediction of and search for gold deposits were elucidated. The characteristics of the studied placer gold were specific for gold derived from a proximal provenance. These characteristics included the poor roundness of the native gold grains, a cloddy&ndash angular and dendritic form, an uneven surface, and a high content of coarse-fraction native gold (0.5&ndash 2 mm), which was as high as 24% of the volume of analyzed native gold. In addition, we conducted a study on the mineralogical features of the gold-sulfide mineralization that was disseminated throughout a small exposure area of paleo-Proterozoic para- and orthogneisses in the Anabar shield basement. A comparison of mineral inclusions in the coarse-fraction native gold and mineral assemblages in the ore deposits showed that one of the possible primary sources for placer gold might be small bodies of metasomatically altered orthogneisses associated with large granitoid plutons. |
| Databáze: | OpenAIRE |
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