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Lukinda Massif

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Journal Article

Geochemical features and geodynamic setting of formation of the Lukinda dunite–troctolite–gabbro massif ( southeastern framing of the Siberian Platform )

I.V. Buchko, A.A. Sorokin, V.A. Ponomarchuk, A.E. Izokh

Journal: Russian Geology and Geophysics

Publisher: Novosibirsk State University

Published: 01 July 2012

Russ. Geol. Geophys. (2012) 53 (7): 636–648.

DOI: https://doi.org/10.1016/j.rgg.2012.05.002

...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

The age and tectonic setting of the Lukinda dunite–gabbro–anorthosite massif in the east of the Selenga–Stanovoi superterrane, Central Asian Fold Belt

I.V. Buchko, A.A. Sorokin, A.B. Kotov, A.V. Samsonov, Yu.O. Larionova, V.A. Ponomarchuk, A.M. Larin

Journal: Russian Geology and Geophysics

Publisher: Novosibirsk State University

Published: 01 July 2018

Russ. Geol. Geophys. (2018) 59 (7): 709–717.

DOI: https://doi.org/10.1016/j.rgg.2018.07.001

...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...

Petrochemical variation diagrams for the Lukinda massif rocks. 1 , ultraba...

in Geochemical features and geodynamic setting of formation of the Lukinda dunite–troctolite–gabbro massif ( southeastern framing of the Siberian Platform ) > Russian Geology and Geophysics

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/4 discrimination diagram for rocks of the <span class="search-highlight">Lukinda</span> <span class="search-highlight">massif</span>. Composi...

Y–Nb·2–Zr/4 discrimination diagram for rocks of the Lukinda massif. Composi...

in Geochemical features and geodynamic setting of formation of the Lukinda dunite–troctolite–gabbro massif ( southeastern framing of the Siberian Platform ) > Russian Geology and Geophysics

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/Y–Nb/Y diagram for rocks of the <span class="search-highlight">Lukinda</span> <span class="search-highlight">massif</span>. Composition fields are a...

Ti/Y–Nb/Y diagram for rocks of the Lukinda massif. Composition fields are a...

in Geochemical features and geodynamic setting of formation of the Lukinda dunite–troctolite–gabbro massif ( southeastern framing of the Siberian Platform ) > Russian Geology and Geophysics

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>...

Schematic occurrence of the Lukinda dunite–troctolite–gabbro layered massif...

in Geochemical features and geodynamic setting of formation of the Lukinda dunite–troctolite–gabbro massif ( southeastern framing of the Siberian Platform ) > Russian Geology and Geophysics

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 ...

in The age and tectonic setting of the Lukinda dunite–gabbro–anorthosite massif in the east of the Selenga–Stanovoi superterrane, Central Asian Fold Belt > Russian Geology and Geophysics

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...

in The age and tectonic setting of the Lukinda dunite–gabbro–anorthosite massif in the east of the Selenga–Stanovoi superterrane, Central Asian Fold Belt > Russian Geology and Geophysics

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...

in The age and tectonic setting of the Lukinda dunite–gabbro–anorthosite massif in the east of the Selenga–Stanovoi superterrane, Central Asian Fold Belt > Russian Geology and Geophysics

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...

in Geochemical features and geodynamic setting of formation of the Lukinda dunite–troctolite–gabbro massif ( southeastern framing of the Siberian Platform ) > Russian Geology and Geophysics

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...

in Geochemical features and geodynamic setting of formation of the Lukinda dunite–troctolite–gabbro massif ( southeastern framing of the Siberian Platform ) > Russian Geology and Geophysics

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...

in Geochemical features and geodynamic setting of formation of the Lukinda dunite–troctolite–gabbro massif ( southeastern framing of the Siberian Platform ) > Russian Geology and Geophysics

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 ...

in The age and tectonic setting of the Lukinda dunite–gabbro–anorthosite massif in the east of the Selenga–Stanovoi superterrane, Central Asian Fold Belt > Russian Geology and Geophysics

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...

Section of the Lukinda dunite–troctolite–gabbro–anorthosite massif (borehol...

in The age and tectonic setting of the Lukinda dunite–gabbro–anorthosite massif in the east of the Selenga–Stanovoi superterrane, Central Asian Fold Belt > Russian Geology and Geophysics

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>...

Schematic geologic structure of the Lukinda dunite–troctolite–gabbro massif...

in Geochemical features and geodynamic setting of formation of the Lukinda dunite–troctolite–gabbro massif ( southeastern framing of the Siberian Platform ) > Russian Geology and Geophysics

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...

Schematic occurrence of layered ultramafic-mafic massifs on the southeaster...

in Petrology of the Early Mesozoic ultramafic-mafic Luchina massif (southeastern periphery of the Siberian craton) > Russian Geology and Geophysics

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...

Schematic occurrence of layered ultrabasic-basic massifs in the Selenga-Sta...

in The Late Jurassic age and geochemistry of ultramafic-mafic massifs of the Selenga-Stanovoy superterrane ( southern framing of the North Asian craton ) > Russian Geology and Geophysics

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...

Schematic occurrence of ultramafic-mafic massifs of the Dzhugdzhur–Stanovoi...

in The Triassic stage of mafic magmatism in the Dzhugdzhur–Stanovoi superterrane ( southern framing of the North Asian craton ) > Russian Geology and Geophysics

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...

Relationship between age of different types of peridotite-gabbro massifs an...

in INITIAL MAGMAS OF PROTEROZOIC TROCTOLITE-ANORTHOSITE MASSIFS OF NORTH AMERICA AND EVOLUTIONARY TREND OF TIME-DEPENDENT VARIABILITY OF COMPOSITION OF PERIDOTITE-GABBRO MASSIFS > Russian Geology and Geophysics

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

The Late Jurassic age and geochemistry of ultramafic-mafic massifs of the Selenga-Stanovoy superterrane ( southern framing of the North Asian craton )

I.V. Buchko, A.A. Sorokin, E.B. Sal’nikova, A.B. Kotov, A.M. Larin, A.E. Izokh, S.D. Velikoslavinsky, S.Z. Yakovleva

Journal: Russian Geology and Geophysics

Publisher: Novosibirsk State University

Published: 10 December 2007

Russ. Geol. Geophys. (2007) 48 (12): 1026–1036.

DOI: https://doi.org/10.1016/j.rgg.2007.11.005

... — 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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