2020
DOI: 10.1134/s1075701520010018
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Mesozoic Acid Magmatites of Southeastern Transbaikalia: Petrogeochemistry and Relationship with Metasomatism and Ore Formation

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Cited by 13 publications
(8 citation statements)
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“…These are the quartz-hübnerite-sulfide Bom-Gorhon, quartz-cassiterite-wolframite Dedovogorskoye, greisen tin-tungsten Spokoyninskoye, mercury-antimony-wolframite Barun-Shiveya, as well as vein tin-tungsten Bukuka, Belukha, and Antonovogorskoye deposits (Figure 1). The ore objects, with the exception of the Barun-Shiveya deposit, are associated with areas of development of Proterozoic, Paleozoic, and Mesozoic sand-shale deposits, intruded by Mesozoic granitoid intrusions [1,[4][5]. The main ore mineral of the deposits is wolframite.…”
Section: Methodsmentioning
confidence: 99%
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“…These are the quartz-hübnerite-sulfide Bom-Gorhon, quartz-cassiterite-wolframite Dedovogorskoye, greisen tin-tungsten Spokoyninskoye, mercury-antimony-wolframite Barun-Shiveya, as well as vein tin-tungsten Bukuka, Belukha, and Antonovogorskoye deposits (Figure 1). The ore objects, with the exception of the Barun-Shiveya deposit, are associated with areas of development of Proterozoic, Paleozoic, and Mesozoic sand-shale deposits, intruded by Mesozoic granitoid intrusions [1,[4][5]. The main ore mineral of the deposits is wolframite.…”
Section: Methodsmentioning
confidence: 99%
“…The lowest uranium and thorium contents are characteristic of waters formed in the areas of the Dedovogorskoye, Barun-Shiveya, and Belukha deposits. The anomalously high accumulation of radioactive elements in the waters of the Spokoyninskoye, Bom-Gorkhon, and Bukuka deposits is likely due to their increased content in the enclosing leucocratic and Li-F granitoids [1].…”
Section: E3s Web Of Conferences 463 01018 (2023) Eeste2023mentioning
confidence: 99%
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“…[Bortnikov and Petrov, 2020]. Most of the ore deposits are associated with the Late Mesozoic tectonomagmatic activation, which was the most productive in the manifestation of tectonotermal events and ore-genetic processes that determine metallogenic territory's image [Andreeva et al, 2020;Petrov et al, 2017a]. However, the territory is not provided with a system of continuous observations after lithosphere deformation, although further prospects of MRB development are linked here with work on deep horizons of longterm exploitable deposits under complicated geological and mining conditions.…”
Section: Improvement Of Methods For Forecasting and Preventing Technogenic Accidentsmentioning
confidence: 99%
“…Geological structure and ore-bearing volcano-plutonic complexes of the southern Argun area evolved during the Proterozoic (which ended about 600 million years ago), Caledonian (520-410 million years ago), and Hercynian tectonomagmatic cycles (360-120 million years ago), in the process of tectonomagmatic activation in the late Mesozoic (160-100 million years ago) and at the neotectonic phase of the region's development. Late Mesozoic tectonomagmatic activation is most productive in the form of ore-genetic processes that determined the metallogenic appearance of the territory [30,31].…”
Section: Geological Settingmentioning
confidence: 99%