Massive Sulfides from Ancient and Modern Margins of the Asian Paleo-ocean and Pacific: Textures, Mineralogy and Fluid Inclusion Data

I. Yu. Melekestseva N. N. Ankusheva G. A. Tret’yakov V. V. Zaykov V. A. Simonov

Organization:: International Marine Minerals Society
Pages:: 12
File Size:: 1600 KB
Publication Date:

Abstract

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The Kyzyl-Tashtyg massive sulfide polymetallic deposit is situated 120 km north-east of Kyzyl (the capital of Tuva Republic, Russia). It is located in the Ulug-O volcanic zone which is interpreted as the northern segment of the Kaa-Khem rift in Sayano-Tuva marginal sea, one of the Paleoasian Ocean margin (Fig. 1) [Zaykov, 2006]. Since its discovery in 1946 the deposit has been studied by many researchers. Significant information was published by Kuzebny et al. [2001] and Zaykov [2006] who proposed volcanogenic-sedimentary genesis. A single reference in English about Kyzyl-Tashtyg is available [Herrington et al., 1999].

Citation

APA: I. Yu. Melekestseva N. N. Ankusheva G. A. Tret’yakov V. V. Zaykov V. A. Simonov Massive Sulfides from Ancient and Modern Margins of the Asian Paleo-ocean and Pacific: Textures, Mineralogy and Fluid Inclusion Data

MLA: I. Yu. Melekestseva N. N. Ankusheva G. A. Tret’yakov V. V. Zaykov V. A. Simonov Massive Sulfides from Ancient and Modern Margins of the Asian Paleo-ocean and Pacific: Textures, Mineralogy and Fluid Inclusion Data. International Marine Minerals Society,

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