Мақаланы E-mail арқылы жіберу Ilei fluorite-phenakite ore phenomenon (Eastern Sayan): contribution of Devonian riftogenic magmatism to formation of Eastern Sayan rare metal metallogenic zone
- Авторлар: Lykhin D.A.1, Vorontsov A.A.2, Yarmolyuk V.V.1
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Мекемелер:
- Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry, Russian Academy of Sciences
- A.P. Vinogradov Institute of Geochemistry, Siberian Branch of the Russian Academy of Sciences
- Шығарылым: Том 514, № 2 (2024)
- Беттер: 251-262
- Бөлім: METALLOGENY
- ##submission.dateSubmitted##: 31.01.2025
- ##submission.datePublished##: 12.09.2024
- URL: https://vestnik.nvsu.ru/2686-7397/article/view/650085
- DOI: https://doi.org/10.31857/S2686739724020087
- ID: 650085
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Fig. 1. Scheme of distribution of Early Devonian volcanoplutonic associations in the Kropotkin Ridge area according to [7]. 1 – loose sediments; 2 – Quaternary basalts; 3–5 – Early Devonian igneous associations: 3 – trachyrhyolite-comendite, 4 – basaltic and bimodal basalt-trachyrhyolite-comendite, 5 – subalkaline and alkaline granites and syenites; 6 – pre-Devonian gneissogranites, gabbroids, granodiorites and plagiogranites; 7 – faults; 8 – position of the Snezhnoye deposit (1) and the Ileyskoye ore occurrence (2); 9–14 – conditional for insertion: 9 – volcanic depressions and grabens, 10 – area of distribution of mafic intrusions at the base of the Bodaibo trough, 11 – Siberian platform, 12 – territory of the paleocontinent, 13 – Paleoasian ocean, 14 – supposed contours of the Devonian rift system. VRS – Vilyui rift system, ASO – Altai-Sayan rift region. Grabens and depressions: Mn – Minusinsk, Tv – Tuva, Dzh – Dzhida-Khasuritsky, Toch – Tochersky, Bd – Bodaibo. The territory of the Kropotkin Ridge is highlighted with a rectangular contour.
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Fig. 2. Structure of the Ilei ore occurrence. a – photograph, dotted line shows outcrops of limestones of the Mongoshinskaya suite; b – geological plan of the Ilei ore occurrence. 1 – glacial deposits; 2 – limestones of the Upper Proterozoic Mongoshinskaya suite; 3–8 – Devonian volcano-plutonic complex: 3–6 – Ognitsky complex: 3 – dikes: a – granite-porphyry, quartz porphyry, b – altered porphyrites, 4 – fine-grained leucocratic granites, 5 – medium- and coarse-grained porphyry-like leucocratic granosyenites and quartz syenites, 6 – leucocratic syenite-porphyry; 7–8 – Ileiskaya sequence: 7 – felsites, 8 – lava breccias; 9 – fluorite veins: a – mapped, b – assumed; 10 – faults; 11 – ore body numbers.
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Fig. 3. a – vein of massive ores with sharp contacts from the central section of the ore occurrence; b – vein-disseminated ores from the western section.
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Fig. 4. Graphs of the normalized distribution of rare and rare-metal elements in igneous rocks and ores of the Ilei ore occurrence according to [11]. Granitoids are solid lines; volcanics of the Ilei formation are dotted lines; ores are highlighted in gray.
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Fig. 5. Rb‒Sr isochron diagram for volcanics of the Ilei sequence. Ar‒Ar geochronological studies were carried out on arfvedsonite isolated from subalkaline granites. The study was carried out at the Institute of Geology and Mineralogy SB RAS using the technique described in [17]. The plateau, constructed in three steps with 43.8% of isolated 39Ar, is characterized by an age value of 381±5 Ma (Table 3, Fig. 6). On the isochron diagram for linear regression by 4 points, the age value calculated was 387±6 Ma, which is consistent with the age of the plateau (Fig. 6 b). Thus, the value 387±6 Ma can be considered to correspond to the time of closure of the amphibole isotope system and the time of formation of subalkaline granites.
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Fig. 6. Results of Ar‒Ar studies of arfvedsonite from subalkaline granites of the Ileyskoye ore occurrence. a – studies of arfvedsonite using the step-heating method; b – isochron diagram for linear regression, constructed using four points.
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