{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,1,31]],"date-time":"2026-01-31T08:06:31Z","timestamp":1769846791691,"version":"3.49.0"},"reference-count":74,"publisher":"GeoScienceWorld","issue":"8","content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":[],"published-print":{"date-parts":[[2019,8,1]]},"abstract":"<jats:title>Abstract<\/jats:title>\n               <jats:p>\u2014The Kalguty Mo\u2013W ore-magmatic system (OMS) is a granite batholith (S = 70 km2, V = 12,800 km3 at the recent denudation level, according to geological and geophysical data). This batholith is cut by the East Kalguty belt of rare-metal ongonite\u2013elvan dikes spatially and temporally associated with the East Kalguty quartz-vein\u2013greisen Mo\u2013W deposit. Geological and petrogenetic studies along with published and our new results of geochronological (U\/Pb zircon, Re\/Os molybdenite, and 40Ar\/39Ar biotite and muscovite) dating made it possible to reconstruct the thermochronological history of the Kalguty OMS. Five stages have been recognized: I (215 \u00b1 1 Ma)\u2014formation of granites of major intrusive phase and of Mo-rich mineralization, which is an orebody called the Molybdenum stock; II (206 \u00b1 1 Ma)\u2014formation of leucogranite and intragranitic-pegmatite stocks in the granites of major intrusive phase; III (202 \u00b1 1 Ma)\u2014formation of most of ongonite\u2013elvan dikes composing a dike belt; IV (195 \u00b1 1 Ma)\u2014formation of long ultrarare-metal ongonite\u2013elvan dikes in the central part of the dike belt, which is spatially associated with the W-rich veins of the deposit; and V (181 \u00b1 1 Ma)\u2014formation of thin ongonite\u2013elvan dikes on the periphery of the dike belt. The recognized age stages of the Kalguty Mo\u2013W ore-magmatic system were mathematically tested based on the model of crystallization differentiation and the dynamics of heat and mass transfer in the magma chamber corresponding to the Kalguty granite batholith. The results obtained show that the formation of a granite batholith (215 \u00b1 1 Ma) and a later ongonite\u2013elvan dike complex with Mo\u2013W-rich mineralization (195 \u00b1 1 Ma) can be explained only by a two-level ore-magmatic system with the \u201cupper\u201d granite batholith at a depth of 5\u201315 km and the \u201clower\u201d granite chamber at a depth of 20\u201331 km. The total duration of ore-magmatic processes is 20 Myr (ore production stage) or 30 Myr, if we take into account occasional elvan dikes with poor quartz\u2013fluorite\u2013barite\u2013ferberite mineralization (181 \u00b1 1 Ma) on the periphery of the Kalguty deposit.<\/jats:p>","DOI":"10.15372\/rgg2019057","type":"journal-article","created":{"date-parts":[[2019,8,9]],"date-time":"2019-08-09T03:57:56Z","timestamp":1565323076000},"page":"890-910","source":"Crossref","is-referenced-by-count":8,"title":["Stages and Duration of Formation of the Kalguty Mo\u2013W Ore-Magmatic System (Altai): Thermochronology and Mathematical Modeling"],"prefix":"10.2113","volume":"60","author":[{"given":"A.G.","family":"Vladimirov","sequence":"first","affiliation":[{"name":"a V.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences, pr. Akademika Koptyuga 3, Novosibirsk, 630090, Russia"},{"name":"b Novosibirsk State University, ul. Pirogova 2, Novosibirsk, 630090, Russia"},{"name":"b Novosibirsk State University, ul. Pirogova 2, Novosibirsk, 630090, Russia"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"I.Yu.","family":"Annikova","sequence":"additional","affiliation":[{"name":"a V.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences, pr. Akademika Koptyuga 3, Novosibirsk, 630090, Russia"},{"name":"b Novosibirsk State University, ul. Pirogova 2, Novosibirsk, 630090, Russia"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"N.G.","family":"Murzintsev","sequence":"additional","affiliation":[{"name":"a V.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences, pr. Akademika Koptyuga 3, Novosibirsk, 630090, Russia"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"A.V.","family":"Travin","sequence":"additional","affiliation":[{"name":"a V.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences, pr. Akademika Koptyuga 3, Novosibirsk, 630090, Russia"},{"name":"b Novosibirsk State University, ul. Pirogova 2, Novosibirsk, 630090, Russia"},{"name":"c Tomsk State University, pr. Lenina 36, Tomsk, 634050, Russia"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"E.N.","family":"Sokolova","sequence":"additional","affiliation":[{"name":"a V.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences, pr. Akademika Koptyuga 3, Novosibirsk, 630090, Russia"},{"name":"b Novosibirsk State University, ul. Pirogova 2, Novosibirsk, 630090, Russia"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"S.Z.","family":"Smirnov","sequence":"additional","affiliation":[{"name":"a V.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences, pr. Akademika Koptyuga 3, Novosibirsk, 630090, Russia"},{"name":"b Novosibirsk State University, ul. Pirogova 2, Novosibirsk, 630090, Russia"},{"name":"c Tomsk State University, pr. Lenina 36, Tomsk, 634050, Russia"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"O.A.","family":"Gavryushkina","sequence":"additional","affiliation":[{"name":"a V.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences, pr. Akademika Koptyuga 3, Novosibirsk, 630090, Russia"},{"name":"b Novosibirsk State University, ul. Pirogova 2, Novosibirsk, 630090, Russia"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"T.A.","family":"Oitseva","sequence":"additional","affiliation":[{"name":"d East Kazakhstan State Technical University, ul. Protozanova 69, Ust\u2019-Kamenogorsk, 070004, Republic of Kazakhstan"}],"role":[{"role":"author","vocabulary":"crossref"}]}],"member":"859","reference":[{"key":"2023072116303037200_r1","first-page":"258","article-title":"The Far East province of rare-metal\u2013Li\u2013F granites and its ore potential","volume-title":"Problems of Mineralogy, Petrography, and Metallogeny. P.N. Chirvinskii Commemorative Scientific Readings [in Russian]. 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