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Konder Massif

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Journal Article
Published: 01 May 2004
Russ. Geol. Geophys. (2004) 45 (5): 588–599.
...A.S. Karetnikov Ultrabasites of the Konder Massif (57°36′ N, 134°37′ E) occupy up to 90% of its exposed area. Their K-Ar isotope ages show a broad scatter. Moreover, the Konder ultrabasites, first of all dunites, might actually be significantly older. Direct data suggest only that the rocks...
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Journal Article
Published: 01 April 2005
The Canadian Mineralogist (2005) 43 (2): 637–654.
...Ivan Ya. Nekrasov; Alexander M. Lennikov; Boris L. Zalishchak; Rostislav A. Oktyabrsky; Vladimir V. Ivanov; Valery I. Sapin; Vladimir I. Taskaev Abstract The platinum-group minerals (PGM) of the Konder zoned alkali-ultrabasic massif, located east of the Aldan Shield, in far-eastern Russia...
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Diagram representing solid solutions of Os–Ir–Ru–Pt system of <span class="search-highlight">Konder</span> <span class="search-highlight">massif</span>...
Published: 01 April 2005
F ig . 3. Diagram representing solid solutions of Os–Ir–Ru–Pt system of Konder massif. 1) Data of Table 2 , 2) after Mochalov (1994) , 3) fields of solid-solution compositions of PGE from alpine-type ultrabasic rocks (after Dmitrenko et al. 1985 ), 4) the same from the massifs of alkali
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Compositions of PGE thiospinels. 1) PGE thiospinel of <span class="search-highlight">Konder</span> <span class="search-highlight">massif</span> accordi...
Published: 01 April 2005
F ig . 4. Compositions of PGE thiospinels. 1) PGE thiospinel of Konder massif according to our data ( Table 5 ); 2) fields of PGE thiospinel compositions (after Rudashevsky et al. 1985 ).
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Compositions of sulfoarsenide of Rh–Ir–Ru system of <span class="search-highlight">Konder</span> <span class="search-highlight">massif</span>. 1) PGE s...
Published: 01 April 2005
F ig . 7. Compositions of sulfoarsenide of Rh–Ir–Ru system of Konder massif. 1) PGE sulfarsenides of the Konder massif according to our data (after Nekrasov et al. 1994 ); 2) fields of sulfarsenide compositions from alpine-type ultrabasic rocks (after Dmitrenko et al. 1985 ).
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Compositions of the gold solid-solution of <span class="search-highlight">Konder</span> <span class="search-highlight">massif</span>: Au–Cu, Au–Cu–Ag a...
Published: 01 April 2005
F ig . 10. Compositions of the gold solid-solution of Konder massif: Au–Cu, Au–Cu–Ag and Au–Ag (1), Au–Cu–Pt (2), Au–Cu–Pd (3), Au–Cu–Pt–Pd (4), Au–Cu–Pt with Ag (5), and Au–Cu–Pd with Ag (6). See text for other explanations.
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Schematic geological map of the <span class="search-highlight">Konder</span> <span class="search-highlight">Massif</span> (compiled by G.V. Andreev, A....
Published: 01 May 2004
Fig. 1. Schematic geological map of the Konder Massif (compiled by G.V. Andreev, A.A. El’yanov, and A.N. Mil’to and slightly changed by A.S. Karetnikov), with sampling localities of oriented ultrabasites. 1 — Quaternary loose deposits; 2 , 3 — Upper Proterozoic, Totta Formation: hornfelsed
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Thermal demagnetization of ultrabasite samples from the <span class="search-highlight">Konder</span> <span class="search-highlight">Massif</span>: Zijd...
Published: 01 May 2004
Fig. 4. Thermal demagnetization of ultrabasite samples from the Konder Massif: Zijderveld diagrams ( A ), stereograms of I n distribution during T -cleaning (in the modern frame of reference) ( B ), and thermal demagnetization curves I n ( T ) ( C ). A — Black (light) circles
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Paleomagnetic poles for three types of ultrabasites from the <span class="search-highlight">Konder</span> <span class="search-highlight">Massif</span>....
Published: 01 May 2004
Fig. 5. Paleomagnetic poles for three types of ultrabasites from the Konder Massif. 1 — dunites, 2 — clinopyroxenites, 3 — koswites. Black symbols mark Precambrian directions, and light symbols, Mesozoic ones; 4 — positions of the paleopoles ( A ) of Middle-Late Riphean formations
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Geological map of <span class="search-highlight">Konder</span> alkali-ultrabasic <span class="search-highlight">massif</span>, after  Andreev (1987)  a...
Published: 01 April 2005
F ig . 1. Geological map of Konder alkali-ultrabasic massif, after Andreev (1987) and Sushkin (1995) , with simplifications and additions. 1) Granodiorite, monzonite, monzodiorite; 2) dunite cut by dikes of syenite and nepheline syenite in the southern half of the dunite core; 3) olivine
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REE pattern for melt inclusions in accessory Cr-spinels from the Guli massi...
Published: 01 December 2016
Fig. 15. REE pattern for melt inclusions in accessory Cr-spinels from the Guli massif dunites. 13, melt inclusions in Cr-spinels from the Guli massif dunites ( 1 ), olivines from meimechites ( 2 ), and Cr-spinels from the Konder massif dunites ( 3 ). Chondrite-normalized, according to ( Boynton
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Compositions of PGE disulfide of the erlichmanite–laurite series. 1) PGE di...
Published: 01 April 2005
F ig . 6. Compositions of PGE disulfide of the erlichmanite–laurite series. 1) PGE disulfides of Konder massif according to our data (after Nekrasov et al. 1994 ); 2) fields of mineral compositions of laurite (A) – erlichmanite (B) series from alpine-type ultrabasic rocks (after Dmitrenko
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Diagram MgO–SiO 2  for heated multiphase silicate inclusions in accessory C...
Published: 01 June 2016
Tagil massif; 3 , melt inclusions in Cr-spinels from dunites of the Konder massif; 4 , tylaites of the Nizhnii Tagil massif. Rock fields: 1, picrite; 2, picrobasalt. Compiled using data from ( Bogatikov, 1983 ; Fershtater and Pushkarev, 1992 ; Shmelev et al., 2010 ).
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Composition diagrams of Cr-spinels from dunites ( 1 ) and wehrlites ( 2 ) o...
Published: 01 November 2018
of the ultramafites of the Inagli massif are given according to Simonov et al. (2011) ( 5 ), Mues-Schumacher et al. (1996) ( 6 ); fields of Cr-spinels compositions of the Konder massif ( 7 ), the Nizhnetagilsky massif ( 8 ), the trend for Cr-spinels of the rocks of ophiolite complexes ( 9 ), the region
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Diagram MgO–SiO 2  for melt inclusions in accessory Cr-spinels from the Gul...
Published: 01 December 2016
Fig. 11. Diagram MgO–SiO 2 for melt inclusions in accessory Cr-spinels from the Guli massif dunites. 1–3 , glasses ( 1 ) and calculated bulk compositions of the entire inclusion ( 2 ) and groundmass with a “spinifex” texture ( 3 ); 4 , melt inclusions in Cr-spinels from dunites of the Konder
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Fe–Ni diagram showing the compositional variations of minerals related to k...
Published: 01 December 2022
); the Jicheng area, China ( 6 ) ( Yü et al., 2011 ), the Konder massif ( 7 ) ( Nekrasov et al., 2005 ), the Nizhny Tagil massif ( 8 ) ( Begizov and Zavyalov, 2016 ), as well as the placers and ore deposits from Miass ( 9 ), Sisim ( 10 ) and Seyba ( 11 ) areas ( Barkov et al., 2018a , b , 2019 ).
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Harker diagrams (wt.%) for heated multiphase silicate inclusions in accesso...
Published: 01 June 2016
; 2 , melt inclusions in Cr-spinels from dunites of the Konder massif; 3 – 5 , rocks of the Nizhnii Tagil massif: wehrlites and clinopyroxenites ( 3 ), tylaites ( 4 ), gabbro ( 5 ); 6 – 8 , ankaramites of the Lesser Antilles ( 6 ), Mariana island arc and New Zealand ( 7 ), and Hawaii ( 8 ). Straight
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Composition of native accessory isoferroplatinum from chromite-bearing duni...
Published: 01 April 2005
F ig . 2. Composition of native accessory isoferroplatinum from chromite-bearing dunite of more (1) and less (2) eroded and other (3) parts of the dunite core of the Konder massif; massive chromite veins and schlieren in dunite (4), and ferroan platinum from phlogopite–magnetite pyroxenites (5
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Geological structure scheme of the Central Aldan ore district (modified fro...
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 June 2016
Russ. Geol. Geophys. (2016) 57 (6): 868–890.
... Tagil massif; 3 , melt inclusions in Cr-spinels from dunites of the Konder massif; 4 , tylaites of the Nizhnii Tagil massif. Rock fields: 1, picrite; 2, picrobasalt. Compiled using data from ( Bogatikov, 1983 ; Fershtater and Pushkarev, 1992 ; Shmelev et al., 2010 ). ...
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