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Chiney Massif

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Journal Article
Published: 01 March 2000
European Journal of Mineralogy (2000) 12 (2): 431–440.
...Nadezhda D. TOLSTYKH; Aleksandr P. KRIVENKO; Yuriy G. LAVRENT'EV; Oleg N. TOLSTYKH; Vladimir N. KOROLYUK Abstract Pd-Sb-Bi oxides occur in the exocontact sulphide ores of the Chiney anorthosite-gabbronorite massif. Three types of oxides have been distinguished: Pb-Sb, Pd-Sb-Bi, and Pd-Bi oxides. Pd...
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Reconstructed distribution of mafic dikes dated as 1865–1880 Ma in Siberia ...
Published: 01 May 2016
Fig. 6. Reconstructed distribution of mafic dikes dated as 1865–1880 Ma in Siberia and Laurentia ( Ernst et al., 2015 , 2016 ). 1, Malozadoisky intrusion; 2, Chiney massif; 3, Kalar-Nimnyr dike swarm; 4, Ghost dike swarm. Position of continents taken from ( Evans and Mitchell, 2011 ) with minor
Journal Article
Published: 01 May 2016
Russ. Geol. Geophys. (2016) 57 (5): 822–833.
...Fig. 6. Reconstructed distribution of mafic dikes dated as 1865–1880 Ma in Siberia and Laurentia ( Ernst et al., 2015 , 2016 ). 1, Malozadoisky intrusion; 2, Chiney massif; 3, Kalar-Nimnyr dike swarm; 4, Ghost dike swarm. Position of continents taken from ( Evans and Mitchell, 2011 ) with minor...
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Geologic structure of the western Aldan Shield, the Chara ring structure ( ...
Published: 01 July 2015
Phanerozoic rocks; 11 , faults. Structure–metamorphic zones: Central Aldan (A), Kalar–Nyukzha (B), Chara–Olekma (C), and granulites of the Stanovoi fault (D). Circled numbers: 1, Olondo trough; 2, Chinei massif; 3, Kalar massif; 4, Amga fault; 5, front of the Kalar tectonic wedge in the Stanovoi suture zone
Journal Article
Published: 01 April 2002
The Canadian Mineralogist (2002) 40 (2): 679–692.
... inférieur du massif intrusif de Chiney, en Sibérie, et contiennent amphibole(s), mica(s), chlorite, sulfures disséminés ou massifs (surtout la chalcopyrite), maucherite palladifère, nickeline, sperrylite, mertieïte-II ou stibiopalladinite (ou les deux), isomertieïte, majakite, et michenerite. Nous...
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Journal Article
Published: 01 July 2014
Russ. Geol. Geophys. (2014) 55 (7): 842–853.
... part of their sections is accessible for study. Several ultramafic–mafic massifs are known in northern Transbaikalia. The Chinei massif is the best studied ( Gongal’skii, 2012 ; Gongal’skii and Krivolutskaya, 1993 ; Tolstykh et al., 2008 ). This pluton, formed in the Early Proterozoic (1880...
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Position of Proterozoic platiniferous mafic-ultramafic <span class="search-highlight">massifs</span> in the struc...
Published: 01 May 2016
Fig. 1. Position of Proterozoic platiniferous mafic-ultramafic massifs in the structures of the Siberian Cration and its folded framework. 1 , sedimentary cover; 2 , uplifts of basement; 3 , collision structures. Numbers denote massifs: 1, Chiney; 2, Malozadoisky; 3, Srednecheremshansky; 4
Journal Article
Published: 01 March 2015
Russ. Geol. Geophys. (2015) 56 (3): 411–434.
... mantle might have been the massif protolith. Thus, the Dovyren parental magmas formed from a much older (sub)lithospheric source in the Late Riphean. The source was initially enriched in a mafic component with a low Sm/Nd ratio and was isolated from the convecting mantle and mantle melting processes...
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Journal Article
Published: 01 December 2006
Russ. Geol. Geophys. (2006) 47 (12): 1227–1241.
... and Luktur intrusions show that these intrusions are coeval and can date from the Early Proterozoic platiniferous epoch (1900–1850 Ma). Thus, for biotite from the gabbroids of the Chinei massif the Ar/Ar age is 1880±16 Ma, and for biotite from the Luktur gabbro, 1890±5 Ma. Geochemical data show...
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Geologo-metallogenic scheme of the Udokan–<span class="search-highlight">Chinei</span> ore district ( A ) and geo...
Published: 01 July 2014
Fig. 3. Geologo-metallogenic scheme of the Udokan–Chinei ore district ( A ) and geological map of the Chinei layered massif ( B ), after Gongal’skii (2012) , Gongal’skii and Krivolutskaya (1993) , and Rutshtein et al. (2005) , simplified. A : 1 , Cenozoic undivided lacustrine, river
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Schematic location of platiniferous layered intrusions of the southeastern ...
Published: 01 December 2006
-Cambrian Eravna island-arc system; 5 — Late-Paleozoic-Mesozoic Mongolo-Okhotsk belt; 6 — Pt-bearing massifs: 1 — Yoko-Dovyren (Baikal-Patom trough), 2 — Chinei, Luktur, Upper Sakukan, etc. (Kodar-Udokan area).
Journal Article
Published: 01 September 2020
Russ. Geol. Geophys. (2020) 61 (9): 951–963.
... ; Donskaya et al., 2019 ; Ivanov et al., 2019 ). Gabbroids of the large Chinei massif (1.87 Ga) are localized in the Chara–Olekma terrane ( Gongalsky et al., 2008a , b , 2016 ; Popov et al., 2009 ). In the Baikal salient, basaltoids are present among volcanics of the Akitkan Group of the North Baikal...
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Schematic tectonic map of the Siberian craton and position of the South Sib...
Published: 01 September 2020
, gabbroids of the Ust’-Ignok massif of the Urik–Iya graben; 3, dike gabbrodolerites of the Sharyzhalgai salient in the Kitoi River area; 4, gabbroids of the Malyi Zadoi massif of the Sharyzhalgai salient; 5, dolerites and lamprophyres of small massifs of the Sharyzhalgai salient in the Kitoi River area; 6
Journal Article
Published: 01 May 2024
Russ. Geol. Geophys. (2024) 65 (5): 609–622.
... are represented by granitoids of the Kemen massif of the Kodar complex, which penetrate the sedimentary strata in the central part of the Udokan subzone; by the Ingamakit granite massif in its southern part; by the Chiney massif rocks of the Chiney gabbro–anorthosite complex; by gabbros, diabase, and lamprophyre...
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Journal Article
Published: 01 May 2016
Russ. Geol. Geophys. (2016) 57 (5): 809–821.
..., Luktur, Verkhnii Sakukan). They are well correlated by age with plume magmatism in Canada ( Polyakov et al., 2008 ). The Chinei massif has a polyphase composition and bears Fe–Ti–V and Cu–PGE mineralization. In the composition of layered-intrusion rocks it is similar to the upper part of the Bushveld...
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Journal Article
Published: 01 June 2017
Mineralogical Magazine (2017) 81 (3): 679–688.
... . Tolstykh , N.D. , Krivenko , A.P. , Lavrent'ev , Y.G. , Tolstykh , O.N. and Korolyuk , V.N. ( 2000 ) Oxides of the Pd-Sb-Bi system from the Chiney massif (Aldan Shield, Russia) . European Journal of Mineralogy , 12 , 431 – 440 . As noted, the presently discovered...
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Journal Article
Published: 01 October 2023
Russ. Geol. Geophys. (2023) 64 (10): 1141–1160.
... and dolerite dikes of the Baikal inlier ( Shokhonova et al., 2010 ) and the Chinei gabbroid massif ( Gongalsky et al., 2008 ; Popov et al., 2009 ), Seligdar magnesian carbonatites ( Doroshkevich et al., 2018 ), dolerites of the Kalar–Nimnyr swarm ( Ernst et al., 2016 ), and diabase dikes of the Kuranakh...
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Journal Article
Published: 01 April 2004
The Canadian Mineralogist (2004) 42 (2): 689–694.
... multielement spectra and its application to thin-film problems . Nucl. Instrum. Methods Phys. Res . B140 , 243 – 250 . Tolstykh , N.D. , Krivenko , A.P. , Lavrent’ev , Y.G. , Tolstykh , O.N. & Korolyuk , V. ( 2000 ): Oxides of the Pd–Sb–Bi system from the Chiney massif...
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Journal Article
Journal: Economic Geology
Published: 01 August 2000
Economic Geology (2000) 95 (5): 1173–1176.
.... Martin, G. Poirier, M. Tarkian, Y.A. Pakhomovskii, and Y.P. Men’shikov 391 Selective depth analyses of the alteration products of bornite, chalcopyrite and pyrite performed by XPS, AES, RBS— G. Pratesi and C. Cipriani 397 Oxides of the Pd-Sb-Bi system from the Chiney Massif (Aldan Shield...
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(Na 2 O + K 2 O)–SiO 2  (Sharpenok et al., 2008) ( a ), Th/Yb–Nb/Yb ( Pearc...
Published: 01 September 2020
); 5 , gabbro and gabbrodiorites of the Ust’-Ignok massif of the Urik-Iya graben (this paper); 6 , gabbroids of the Chinei complex of the Aldan Shield ( Gongalsky et al., 2008a , 2016; Gongalskiy, 2010 ); 7 , gabbroids of the Malyi Zadoi massif of the Sharyzhalgai salient ( Mekhonoshin et al., 2016