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Федосеев, Д. Г. (2019) Особенности вещественного состава руд и генезиса шеелит-сульфидного месторождения кордонное (Приморский край, Россия) [Features of the material composition of ores and the genesis of the scheelite-sulfide deposit Kordonnoye (Primorsky Krai, Russia)].

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Reference TypeBook
Book TitleОсобенности вещественного состава руд и генезиса шеелит-сульфидного месторождения кордонное (Приморский край, Россия)
[Features of the material composition of ores and the genesis of the scheelite-sulfide deposit Kordonnoye (Primorsky Krai, Russia)]
AuthorsФедосеев, Д. Г.Author
Year2019
URL
Download URLhttps://www.geokniga.org/sites/geokniga/../../bookfiles/geokniga-dissfedoseev.pdf
LanguagesRussian
Classification
Not set
LoC
Not set
Mindat Ref. ID15623144Long-form Identifiermindat:1:5:15623144:4
GUID0
Full ReferenceФедосеев, Д. Г. (2019) Особенности вещественного состава руд и генезиса шеелит-сульфидного месторождения кордонное (Приморский край, Россия) [Features of the material composition of ores and the genesis of the scheelite-sulfide deposit Kordonnoye (Primorsky Krai, Russia)].
Plain TextФедосеев, Д. Г. (2019) Особенности вещественного состава руд и генезиса шеелит-сульфидного месторождения кордонное (Приморский край, Россия) [Features of the material composition of ores and the genesis of the scheelite-sulfide deposit Kordonnoye (Primorsky Krai, Russia)].
Abstract/NotesSkarn scheelite deposits of the Primorsky Territory of the Far Eastern Region of Russia belong to priority objects that ensure the replenishment and expansion of the mineral resource base of tungsten and associated metals (copper, bismuth, gold, silver, and other elements) in the Russian Federation. A detailed study of specific tungsten deposits is essential for clarifying the general conditions for the formation and patterns of localization of endogenous mineralization. Modern models of the formation of such
deposits are based on different concepts. The best known among them are orthomagmatic, lateral secretion, and through magmatic. There is ambiguity in assessing the role of granitoids in ore formation even in relation to well-studied greisen-vein deposits, although the features of their spatiotemporal relationships with meso- and hypabyssal granite intrusions are empirically reliably established facts.
In recent decades, deposits of stratiform and stockwork types, known in Australia (King Island), France (Salo), the North Caucasus (Kti-Teberda) and many other regions of the world, are considered the most promising for industrial mining of tungsten ores. The exploited scheelite deposits of the skarn genetic type account for more than half of the tungsten production. The Primorsky Territory is no exception, where mining and processing plants operate on the basis of the skarn scheelite-sulfide deposits of Lermontovskoye and Vostok-2. Requiring an expansion of the resource base, since the volume of ore mining at these sites is steadily declining in dynamics. The need for resuscitation of the industry is obvious, which implies involvement in the study of new ore regions and deposits of the region. In Primorye, the most promising area is the Malinovskaya ore area (region), where tungsten deposits of various genetic types are known. One of them is the poorly explored Kordonnoye deposit.


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