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Mineral composition of Albazinskoe deposit ores as an indicator of its belonging to the gold-rare metallic ore-formational type
Composición mineral de menas del depósito Albazinskoe como un indicador de su pertenencia al tipo formativo de mineral metálico poco común de oro
DOI:
https://doi.org/10.15446/esrj.v26n3.71479Keywords:
gold -bearing deposits, rare metals, Sikhote-Alin, transform continental margin. (en)depósitos de oro, metales raros, Sikhote-Alin, transformación del margen continental (es)
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The paper presents new data on mineral composition and geochemical peculiarities of ores from the Albazinskoe gold-bearing deposit (Khabarovsk region, Far East of Russia). Excepting earlier known ore minerals represented by sulfides of iron, arsenic, lead, zinc, and copper, authors have established about two tens of ore minerals, new for this deposit. Among them are sulfides of antimony, bismuth and molybdenum, native bismuth, copper, nickel, silver, tellurides of bismuth, cobalt sulphoarsenite, nickel sulphoantimonite, silver sulphobismuthites, lead-antimony-bismuth sulphosalts, oxides of tin, titanium, tungsten and some others. The revealed specificity of the ores' material composition indicates this deposit belongs to the gold-rare metallic ore-formational type. The sets of geological and structural data show that gold-bearing deposits of this ore-formational type are spatially and genetically associated with the granitoid magmatism, which is exhibited within transform continental margin and related to the geodynamic mode of sliding of the continental and oceanic lithospheric plates.
Este artículo presenta nueva información sobre la composición mineral y las características geoquímicas del depósito aurífero de Albazinskoe (región de Jabárovsk, extremo oriente de Rusia). A excepción de vetas minerales conocidas previamente y representadas por sulfuros de hierro, arsénico, plomo, zinc y cobre, los autores encontraron una veintena de minerales nuevos para este depósito. Entre estos se cuentan los sulfuros de antimonio, bismuto y molibdeno, bismuto autóctono, cobre, níquel, plata, telurios de bismuto, sulfoarsenito de cobalto, sulfoantimonita de níquel, sulfobismutitas de plata, sulfosales de plomo-antimonio-bismuto, óxidos de estaño, titanio, tungsteno, entre otros. Las características encontradas en la composición de los materiales de mena indican que este depósito pertenece al tipo formativo de mineral metálico poco común de oro. La configuración de información geológica y estructural muestra que los depósitos auríferos de este tipo están espacial y genéticamente asociados con el magmatismo granitoide, el cual se observa en el margen de transformación continental y que se relaciona con el modo geodinámico de deslizamiento de las placas litosféricas continentanles y oceánicas.
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