2013
DOI: 10.1134/s107570151304003x
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Lead isotope ore provinces of eastern Transbaikalia and their relationships to regional structures: Results of high-precision MC-ICP-MS study of Pb isotopes

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Cited by 20 publications
(3 citation statements)
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“…The high‐magnesium monzonite magma that generated the K‐adakites associated with the ore deposits is considered to have formed through delamination of crustal material and mantle melting (Berzina et al, ). A similar conclusion was also arrived at by Chugaev et al () on the gold and molybdenum mineralization where the authors invoked the presence of geochemical reservoirs in the mantle. Based on Pb isotope modeling, the involvement of subducted oceanic crust was inferred in the formation of gold deposits in Darasun belt and the molybdenum ores in Bugdaya.…”
Section: Spatial Distribution and Mantle Connectionsupporting
confidence: 81%
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“…The high‐magnesium monzonite magma that generated the K‐adakites associated with the ore deposits is considered to have formed through delamination of crustal material and mantle melting (Berzina et al, ). A similar conclusion was also arrived at by Chugaev et al () on the gold and molybdenum mineralization where the authors invoked the presence of geochemical reservoirs in the mantle. Based on Pb isotope modeling, the involvement of subducted oceanic crust was inferred in the formation of gold deposits in Darasun belt and the molybdenum ores in Bugdaya.…”
Section: Spatial Distribution and Mantle Connectionsupporting
confidence: 81%
“…These conclusions are supported by seismic tomographic data that show stagnant oceanic slab in the mantle transition zone at a depth of 410–670 km. A similar situation was also envisaged for the Akatui and Noion‐Tologoi deposits based on Pb isotope ratios of galena (Chugaev et al, ; Sasim et al, ). The formation of uranium deposits of Streltsovka type is also correlated to a similar mechanism (Shatkov, ).…”
Section: Spatial Distribution and Mantle Connectionsupporting
confidence: 59%
“…More than 5800 published analyses of lead ores were compiled as reference data (sources: Moorbath and Vokes 1963;Wedepohl et al 1978;Bjørlykke and Thorpe 1982;Johansson 1983Johansson , 1984Johansson , 1985Johansson and Rickard 1985;Höhndorf and Dill 1986;Billström 1990;Bjørlykke et al 1990Bjørlykke et al , 1993Bielicki and Tischendorf 1991;Le Guen et al 1991;Nilsen and Bjørlykke 1991;Lévêque and Haack 1993;Sundblad 1994;Petersen et al 1995;Rohl 1996;Rohl and Needham 1998;Sayre et al 2001;Wagner and Schneider 2001;Durali-Müller 2005;Höppner et al 2005;Téreygeol et al 2005;Baron et al 2006;Bode 2008;Chernyshev et al 2008;Guénette-Beck et al 2009;Stos-Gale and Gale 2009;Chugayev et al 2010Chugayev et al , 2013Mirnejad et al 2011;Chen et al 2012;Kirnbauer et al 2012;Huelga-Suarez et al 2014a-b; OXALID database: http://oxalid.arch.ox.ac.uk/). Analysis of samples was compared with the database with minimum Euclidian distance in 3D lead isotope space as a criterion of similarity, using a VBA routine in Microsoft® Excel® 2003.…”
Section: Lead Isotope Analysismentioning
confidence: 99%