Malinovka deposit—A new type of gold mineralization in Primorye, Russia: Geology, mineralogy, and genesis


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Original data on the ore composition are obtained by studying samples from mining workings. In terms of mineral composition, gold-productive veinlets are subdivided into three types: sulfide–quartz, sulfide–carbonate–quartz, and sulfide. The wall-rock metasomatites and typomorphic features of the minerals are studied and the genetic problems of the ores and deposit are discussed. It is established that the Malinovka deposit is ascribed to the gold–tourmaline type (gold–quartz formation), which is identified for the first time in Primorye. In terms of many parameters, the ores of this type are close to those of the large deposits from the Transbaikalian and Amur regions (Klyuchevsky, Kariy, Kirov, Darasun, and others), which are genetically related to granitoid magmatism.

Sobre autores

V. Gvozdev

Far East Geological Institute, Far East Branch

Autor responsável pela correspondência
Email: gvozdev@fegi.ru
Rússia, pr. 100-letiya Vladivostoka 159, Vladivostok, 690022

K. Dobroshevsky

ZAO Primorzoloto

Email: gvozdev@fegi.ru
Rússia, ul. Verkhneportovaya 46, Vladivostok, 690003

A. Vakh

Far East Geological Institute, Far East Branch

Email: gvozdev@fegi.ru
Rússia, pr. 100-letiya Vladivostoka 159, Vladivostok, 690022

N. Goryachev

Northeast Interdisciplinary Scientific Research Institute, Far East Branch

Email: gvozdev@fegi.ru
Rússia, ul. Portovaya 16, Magadan, 685000

V. Stepanov

Research Geotechnological Center, Far East Branch

Email: gvozdev@fegi.ru
Rússia, Severo-Vostochnoe sh. 30, Petropavlovsk Kamchatskii, 683002

D. Fedoseev

Far East Geological Institute, Far East Branch

Email: gvozdev@fegi.ru
Rússia, pr. 100-letiya Vladivostoka 159, Vladivostok, 690022

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