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1-4 OF 4 RESULTS FOR
Tissa-Sarkhoy region
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Journal Article
Composition and conditions of formation of gold-telluride mineralization in the Tissa-Sarkhoi gold-bearing province (East Sayan)
B.B. Damdinov, A.G. Mironov, A.A. Borovikov, B.B. Guntypov, N.S. Karmanov, A.S. Borisenko, B.L. Garmaev
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 August 2007
Russ. Geol. Geophys. (2007) 48 (8): 643–655.
...B.B. Damdinov; A.G. Mironov; A.A. Borovikov; B.B. Guntypov; N.S. Karmanov; A.S. Borisenko; B.L. Garmaev Abstract The structure and petrologic composition of new gold-ore provinces in southeastern East Sayan (Tissa-Sarkhoi cluster) are considered. Several morphogenetic types of gold mineralization...
Journal Article
TUVA-MONGOLIA TERRANE (in the context of microcontinents in the Paleoasian ocean)
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 June 2003
Russ. Geol. Geophys. (2003) 44 (6): 531–541.
... in regular transition from shallower to deeper-water complexes. Deposits on the northernmost extremity of the microcontinent (Bokson Group in the Khayt-Tissa interfluve) [ 27 ] facially and lithologically differ from the reference section of the Bokson Group in the Sarkhoi-Urik interfluve...
Journal Article
THE MINERALOGY OF THE BELLEROPHON-NELSON TELLURIDE-BEARING GOLD DEPOSIT, ST. IVES CAMP, YILGARN CRATON, WESTERN AUSTRALIA
Journal: The Canadian Mineralogist
Publisher: Mineralogical Association of Canada
Published: 15 June 2015
The Canadian Mineralogist (2014) 52 (6): 981–1006.
... of formation of gold telluride mineralization in the Tissa Sarkhoi gold bearing province (East Sayan) . Russian Geology and Geophysics 48 , 643 – 655 . Duuring , P. , Hagemann , S.G. , & Groves , D.I. ( 2000 ) Structural setting, hydrothermal alteration, and gold mineralization...
Journal Article
Noble-metal ore genesis and mantle–crust interaction
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 February 2014
Russ. Geol. Geophys. (2014) 55 (2): 252–258.
..., and/or rock contrast zones ( Groves et al., 2003 ). The main difference between orogenic and granitoid-related gold deposits is that the former originate synchronously with the evolution of penetrating plastic deformations of the enclosing rocks (crush, folds, regional cleavage) or somewhat later, whereas...