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Lukinda Massif

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Journal Article
Published: 01 July 2012
Russ. Geol. Geophys. (2012) 53 (7): 636–648.
...I.V. Buchko; A.A. Sorokin; V.A. Ponomarchuk; A.E. Izokh Abstract The Lukinda dunite–troctolite–gabbro massif in the Selenga–Stanovoy superterrane on the southeastern framing of the Siberian Platform was earlier considered Precambrian. The performed 40 Ar/ 39 Ar dating of the massif plagioclase...
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Journal Article
Published: 01 July 2018
Russ. Geol. Geophys. (2018) 59 (7): 709–717.
...I.V. Buchko; A.A. Sorokin; A.B. Kotov; A.V. Samsonov; Yu.O. Larionova; V.A. Ponomarchuk; A.M. Larin Abstract Results of integrated 40 Ar/ 39 Ar, Rb–Sr, and Sm–Nd geochronological studies of the Lukinda dunite–troctolite–gabbro–anorthosite massif in the northeast of the Selenga–Stanovoi superterrane...
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Petrochemical variation diagrams for the <span class="search-highlight">Lukinda</span> <span class="search-highlight">massif</span> rocks.  1 , ultraba...
Published: 01 July 2012
Fig. 4. Petrochemical variation diagrams for the Lukinda massif rocks. 1 , ultrabasites; 2 , pyroxenites; 3 , gabbroids; 4 , anorthosites; 5 , 6 , fields of peridotites, after Reverdatto et al. (2008) : 5 , mantle, 6 , crustal. Arrows show differentiation trends.
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Y–Nb·2–Zr&#x2F;4 discrimination diagram for rocks of the <span class="search-highlight">Lukinda</span> <span class="search-highlight">massif</span>. Composi...
Published: 01 July 2012
Fig. 8. Y–Nb·2–Zr/4 discrimination diagram for rocks of the Lukinda massif. Composition fields are after Pearce and Cann (1973) : AI, within-plate alkali basalts, AII, within-plate alkali basalts and within-plate tholeiitic basalts, B, enriched mid-ocean basalts (E-MORB), C, volcanic-arc
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Ti&#x2F;Y–Nb&#x2F;Y diagram for rocks of the <span class="search-highlight">Lukinda</span> <span class="search-highlight">massif</span>. Composition fields are a...
Published: 01 July 2012
Fig. 9. Ti/Y–Nb/Y diagram for rocks of the Lukinda massif. Composition fields are after Pearce (1982) ; Thol, tholeiitic series, Trans, transitional series; Alk, alkaline series. Designations follow Fig. 8 .
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Schematic occurrence of the <span class="search-highlight">Lukinda</span> dunite–troctolite–gabbro layered <span class="search-highlight">massif</span>...
Published: 01 July 2012
Fig. 1. Schematic occurrence of the Lukinda dunite–troctolite–gabbro layered massif, after Karsakov (1984) and Milai (1970) . 1 , amphibole gabbro, amphibolites, and schists of the Upper Archean(?) Dzhigdala Formation; 2 , late-Stanovoy granitoids; 3 , deposits of the Upper Proterozoic
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( a ) Stepwise heating and ( b ) the reverse isochron for plagioclase from ...
Published: 01 July 2018
Fig. 5. ( a ) Stepwise heating and ( b ) the reverse isochron for plagioclase from anorthosite (sample S-3-84) from the upper stratified series of the Lukinda massif.
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Isochrons for rock-forming minerals of gabbronorite (sample S-3-148/2) from...
Published: 01 July 2018
Fig. 6. Isochrons for rock-forming minerals of gabbronorite (sample S-3-148/2) from the lower stratified series of the Lukinda massif: ( a ) Rb–Sr and ( b ) Sm–Nd.
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Distribution of rare elements in anorthosite (sample S-3-84) and gabbronori...
Published: 01 July 2018
Fig. 4. Distribution of rare elements in anorthosite (sample S-3-84) and gabbronorite (sample S-3-148/2) used in geochronological studies and in rocks of the upper and lower stratified series of the Lukinda massif according to ( Buchko et al., 2012 b) as amended by the authors. The primitive
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Primitive-mantle-normalized ( Sun and McDonough, 1989 ) trace-element patte...
Published: 01 July 2012
Fig. 6. Primitive-mantle-normalized ( Sun and McDonough, 1989 ) trace-element patterns of the Lukinda massif rocks. Rocks of the upper ( A ) and lower layered series ( B ). The composition fields of typical island-arc, trap, and continental-rift basalts are given after Velikoslavinskii
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Chondrite  C  1 -normalized ( McDonough and Sun, 1995 ) REE patterns of the...
Published: 01 July 2012
Fig. 5. Chondrite C 1 -normalized ( McDonough and Sun, 1995 ) REE patterns of the Lukinda massif rocks. The composition fields of typical island-arc, trap, and continental-rift basalts are given after Velikoslavinskii and Glebovitskii (2005) , and those of N-MORB, E-MORB, and OIB, after Sun
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Chondrite  C  1 -normalized ( McDonough and Sun, 1995 ) PGE, Ni, Au, Cu, an...
Published: 01 July 2012
Fig. 7. Chondrite C 1 -normalized ( McDonough and Sun, 1995 ) PGE, Ni, Au, Cu, and Re patterns of the Lukinda massif rocks. For comparison, the element patterns of Pt-bearing layered intrusions, chromitities, and ophiolites are given. 1 , dunites (Rh type); 2 , gabbroids (Pt type); 3
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Tectonic map of the southeastern margin of the North Asian craton. Data by ...
Published: 01 July 2018
, Kupuri; LR, Larba; ML, Mul’muga; ST, Sivaki–Tok. The asterisk in the inset map indicates the Lukinda massif. SV, Selenga–Vitim volcanoplutonic belt, according to ( Parfenov et al., 1999 ).
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Section of the <span class="search-highlight">Lukinda</span> dunite–troctolite–gabbro–anorthosite <span class="search-highlight">massif</span> (borehol...
Published: 01 July 2018
Fig. 3. Section of the Lukinda dunite–troctolite–gabbro–anorthosite massif (borehole 3): 1 , dunites; 2 , plagiodunites; 3 , pyroxenites; 4 , troctolites; 5 , olivine gabbro and gabbronorites; 6 , gabbro; 7 , leucogabbro; 8 , anorthosites; 9 , granites; 10 , sampling sites
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Schematic geologic structure of the <span class="search-highlight">Lukinda</span> dunite–troctolite–gabbro <span class="search-highlight">massif</span>...
Published: 01 July 2012
Fig. 2. Schematic geologic structure of the Lukinda dunite–troctolite–gabbro massif, according to our materials and data from Balykin et al. (1986) . 1 , Neoarchean amphibolites, schists, gneisses, and gneiss-granites; 2 – 4 , rocks of the Lukinda complex: 2 , lower layered series
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Schematic occurrence of layered ultramafic-mafic <span class="search-highlight">massifs</span> on the southeaster...
Published: 01 August 2008
— ultramafic-mafic massifs. Massifs: 1 — Lukinda, 2 — Kengurak, 3 — Mongoli, 4 — Veselyi, 5 — Nyukzha, 6 — Luchina, 7 — Il’deus. In the inset, the position of the Luchina massif is asterisked. Hatched area is the Mongolo-Okhotsk fold belt (MOFB).
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Schematic occurrence of layered ultrabasic-basic <span class="search-highlight">massifs</span> in the Selenga-Sta...
Published: 10 December 2007
— Nyukzha, 2 — Kengurak-Sergach, 3 — Mongoli, 4 — Petropavlovsk, 5 — Lukinda, 6 — Veselyi, 7 — Srednii Urkan. On the inset, the hatched area marks the Mongolo-Okhotsk fold belt (MOFB). Asterisks mark the position of the above massifs.
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Schematic occurrence of ultramafic-mafic <span class="search-highlight">massifs</span> of the Dzhugdzhur–Stanovoi...
Published: 01 November 2010
-mafic massifs: 1, Lukinda, 2, Kengurak, 3, Mongolii, 4, Veselkin, 5, Nyukzha, 6, Lucha, 7, Il’deus, 8, Ul’degit, 9, Chek-Chikan. Inset: Asterisks mark the position of the Ul’degit and Chek-Chikan massifs. Hatched area is the Mongol-Okhotsk fold belt.
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Relationship between age of different types of peridotite-gabbro <span class="search-highlight">massifs</span> an...
Published: 01 November 2004
(Yoko-Dovyren massif (15), northern Baikal region, Marinka (16), northern Transbaikalia, Lukinda (17), East Siberia, Kokpeta (18), Kempirsai ophiolite association of South Urals, Nuyen Chu (19), northern Vietnam); 5 — olivinite-troctolite-gabbro, olivinite-lherzolite-websterite-gabbronorite
Journal Article
Published: 10 December 2007
Russ. Geol. Geophys. (2007) 48 (12): 1026–1036.
... — Nyukzha, 2 — Kengurak-Sergach, 3 — Mongoli, 4 — Petropavlovsk, 5 — Lukinda, 6 — Veselyi, 7 — Srednii Urkan. On the inset, the hatched area marks the Mongolo-Okhotsk fold belt (MOFB). Asterisks mark the position of the above massifs. ...
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