Year: 2022
Pages: 53-64
UDC: 553.411.071
Number: 3
Type: scientific article
DOI: 10.31084/2619-0087/2022-3-5
Topic: ARTICLES AND PUBLICATIONS
Authors: Nurieva, Kamilla R., Snachev, Akexander V., Latypov, Fanir F., Gataullin, Ruslan A., Rassomakhin, Mikhail A.
The article considers the Golenkie Gorki gold ore occurrence, which is part of the Siratur ore field. It is located in the northern part of the South Ural segment of the Main Ural Fault, in the junction zone of the Bashkir meganticlinorium with the northern closure of the Magnitogorsk megazone. Carbonaceous and carbonaceous-chlorite-quartz shales have areal distribution, form independent packs and have a predominantly granoblastic structure and a massive, rarely spotted texture. The results of thermal analysisshow the temperature of the onset of the exothermic effect of carbon in the range of 500–640°С, which correspondsto the high-temperature subfacies ofthe greenschistfacies ofregional metamorphism. The average content of Corg is about 2.4 %, which makes it possible to attribute these rocks to the carbonaceous type. It is shown that gold ore mineralization is confined to the contact zone of a rather thick sequence of carbonaceous shales of the Polyakovka Formation with serpentinites of the Nurali gabbro-ultramafic massif. A zone of listwanites 1400 m long and up to 30 m wide was established within the contact. Testing of all types of rocks for gold revealed its increased content in ferruginous and silicified carbonaceouschlorite-quartz schists and veined quartz, as well as near-ore values in silicified listwanites. The analysis of gold grains made it possible to refer them to the low-quality type. Significant silver impurities indicate the gold-sulfide type of mineralization. Along the periphery of the grains, the purification of gold grains from impurity elements in the hypergenesis zone was noted.
the Southern Urals, Main Ural fault, Magnitogorsk megasynclinorium, Nurali massif, Golenkie Gorki, Siratur deposit, Polyakovka Formation, gold, silver, sulfides, ophiolite association, carbonaceous schists, ultramafic rocks, listwanites