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Dzheltula Massif

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Geological structure scheme of the Central Aldan ore district (modified from (Maksimov et al., 2010)). 1, Upper and Middle Jurassic terrigenous deposits; 2, Vendian–lower Cambrian platform cover; 3, early Cambrian crystalline basement; 4–5, alkaline and moderately alkaline magmatic manifestations: intrusions (4), diatremes (5a), and dikes (5b); 6, faults: proven (a), predicted (b); 7, outlines of structural blocks: uplifts (7a), troughs (7b); 8–9, deposits of formations: sulfide gold (8a), porphyry gold (8b), gold–argillisite–K-feldspar–quartz (9a), gold–molybdenite–brannerite–gumbaite (9b); 10a, Yakokut valley graben, 10b, outer interface of the Central Aldan ore-magmatic system (CAOMS). Major intrusive massifs: 1, Inagli, 2, Tommot, 3, Yakokut, 4, Dzhekonda, 5, Yllymakh, 6, Yukhta, 7, Ryabinovyi. The insert shows locations of massifs and ore districts: a, Malyi Murun massif; b, Central Aldan ore district; c, Dzheltula massif; d, Ket-Kap–Yuna district; e, Konder massif.
Published: 01 January 2019
and ore districts: a, Malyi Murun massif; b , Central Aldan ore district; c , Dzheltula massif; d, Ket-Kap–Yuna district; e , Konder massif.
Journal Article
Published: 01 February 2023
Russ. Geol. Geophys. (2023) 64 (2): 175–191.
.... Magmatism of this stage was of limited occurrence in the CAOD and did not produce alkali syenites, monzonite–syenites, and ores. At the same time, rocks with an age of 121.1 ± 1.3—115.5 ± 1.6 Ma are widespread in the large (120 km 2 ) Dzheltula ring massif of the Tyrkanda ore district, located east...
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Journal Article
Published: 01 April 2025
Russ. Geol. Geophys. (2025) 66 (4): 424–449.
... and Evolution of Mesozoic Alkaline Magmatism of the Aldan–Stanovoy Shield (Example of the Yllymakh, Inagli, Dzheltula, and Upper Amga massif) . PhD Thesis [in Russian]. IGM SO RAN , Novosibirsk . Popov , N. , Smelov , A. ( 1996 ). The Aldan shield metamorphic assemblages . Geologiya i...
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Journal Article
Published: 01 January 2019
Russ. Geol. Geophys. (2019) 60 (1): 33–44.
... and ore districts: a, Malyi Murun massif; b , Central Aldan ore district; c , Dzheltula massif; d, Ket-Kap–Yuna district; e , Konder massif. ...
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Journal Article
Published: 01 January 2010
Russ. Geol. Geophys. (2010) 51 (1): 98–111.
... region, it is reasonable to develop depleted ores and tailings (mining dumps at the Noril’sk and Talnakh deposits). However, the key solution consists in new large discoveries within the Dzheltula and Kharaelakh volcanic and plutonic complexes. Gold production enhancement may be associated with black...
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Journal Article
Published: 01 October 1996
Russ. Geol. Geophys. (1996) 37 (10): 84–93.
... granite-gneissic dome, massifs of granites and syenites being related to the latter (the Yakokut cluster of Mesozoic tectonomagmatic activity, TMA). A typical negative gravimetric anomaly is a site of rock development corresponding to the Dzheltula cluster of TMA (see Fig. 3 , D ), where intrusions...
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Journal Article
Published: 01 March 2024
Russ. Geol. Geophys. (2024) 65 (3): 302–325.
... distributed in the Ulakhan ( Fig. 1 ) and Konder massifs of the KKYuIP (possibly also in the Usmun-Dar’ya, Bukinda massifs, and some others); а pyroclastic stratum (insignificant in volume and area) observed in the west of the Ulakhan massif, is composed of thin horizons of phonolitic tuffs (not marked...
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