Zharcha Massif

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Model for the Sr-isotope evolution of the Early Paleozoic crust in the SSMA...

in ISOTOPE GEOCHRONOLOGY OF PALEOZOIC GRANITOIDS FROM THE SELENGA-STANOVOY MOUNTAINOUS AREA > Russian Geology and Geophysics

Published: 01 November 2011

Fig. 6. Model for the Sr-isotope evolution of the Early Paleozoic crust in the SSMA. Open squares show the compositions of Early Paleozoic granitoids; gray symbols, Carboniferous granitoids (squares — Zharcha Massif, diamonds — veined leucogranites and aplites); and filled circles, dome

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SiO 2 –(Na 2 O + K 2 O) classification diagram for Paleozoic granitoids of ...

in GEOCHEMISTRY OF PALEOZOIC GRANITOID MAGMATISM IN THE WEST STANOVOY ZONE OF TRANSBAIKALIA > Russian Geology and Geophysics

Published: 01 March 2004

— Marekta-Bereya Massif; UN — Ul’durga-Nercha batholith; Zh — Zharcha Massif; avlg — aplite-like veined leucogranites; a — aplites.

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Study granitoids on the Pearce trace-element discrimination diagram [ 22 ]....

in GEOCHEMISTRY OF PALEOZOIC GRANITOID MAGMATISM IN THE WEST STANOVOY ZONE OF TRANSBAIKALIA > Russian Geology and Geophysics

Published: 01 March 2004

Fig. 8. Study granitoids on the Pearce trace-element discrimination diagram [ 22 ]. Qd — quartz diorites, Gd — granodiorites, G — group I granites, Zh — granites and leucogranites of the Zharcha Massif, OChVB — granitoids of the Okhotsk-Chukchi volcanic belt [ 19 ], SN-T — granitoids

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Upper-crust-normalized average chemical compositions of Paleozoic granitoid...

in GEOCHEMISTRY OF PALEOZOIC GRANITOID MAGMATISM IN THE WEST STANOVOY ZONE OF TRANSBAIKALIA > Russian Geology and Geophysics

Published: 01 March 2004

Fig. 3. Upper-crust-normalized average chemical compositions of Paleozoic granitoids from the West Stanovoy SFZ (digits below the abscissa are the norms, after [ 15 ]). Zh-g and Zh-lg — granites and leucogranites of the Zharcha Massif, respectively, D-gn — diorite- and granodiorite-gneisses

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Schematic geologotectonic map of the study area (after [ 6 ], simplified). ...

in GEOCHEMISTRY OF PALEOZOIC GRANITOID MAGMATISM IN THE WEST STANOVOY ZONE OF TRANSBAIKALIA > Russian Geology and Geophysics

Published: 01 March 2004

complex (PZ 1 ); 5 Precambrian (AR–PR 1 ) crystalline basement; 6 — geologic boundaries (a) and faults (b). Objects: LIB — Lower Ingoda batholith, UT — Ulentui-Torga site, VD — Vershino-Darasunsky Massif, Ya — Yamnaya Massif, MB — Marekta-Bereya Massif, UN — Ul’durga-Nercha batholith, Zh — Zharcha

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Geologo-tectonic scheme of occurrence of Paleozoic granitoids in the center...

in ISOTOPE GEOCHRONOLOGY OF PALEOZOIC GRANITOIDS FROM THE SELENGA-STANOVOY MOUNTAINOUS AREA > Russian Geology and Geophysics

Published: 01 November 2011

, Ar — Argun’; 3 — areas of occurrence of Paleozoic granitoids in the SSMA; 4 — faults; 5 — location of dated objects (Ya — gneiss-granite domes of the Yablonovyi Range, K — Kruchina dome, MBM — Marekta-Bereya Massif, ZhM — Zharcha Massif, VDM — Vershino-Darasunskii Massif, UT — Ulentui-Torgo

Journal Article

GEOCHEMISTRY OF PALEOZOIC GRANITOID MAGMATISM IN THE WEST STANOVOY ZONE OF TRANSBAIKALIA

M.E. Kazimirovsky

Journal: Russian Geology and Geophysics

Publisher: Novosibirsk State University

Published: 01 March 2004

Russ. Geol. Geophys. (2004) 45 (3): 347–362.

... — Marekta-Bereya Massif; UN — Ul’durga-Nercha batholith; Zh — Zharcha Massif; avlg — aplite-like veined leucogranites; a — aplites. ...

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Journal Article

ISOTOPE GEOCHRONOLOGY OF PALEOZOIC GRANITOIDS FROM THE SELENGA-STANOVOY MOUNTAINOUS AREA

M.E. Kazimirovsky, G.P. Sandimirova, E.V. Bankovskaya

Journal: Russian Geology and Geophysics

Publisher: Novosibirsk State University

Published: 01 November 2011

Russ. Geol. Geophys. (2002) 43 (11): 973–989.

...Fig. 6. Model for the Sr-isotope evolution of the Early Paleozoic crust in the SSMA. Open squares show the compositions of Early Paleozoic granitoids; gray symbols, Carboniferous granitoids (squares — Zharcha Massif, diamonds — veined leucogranites and aplites); and filled circles, dome...

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Journal Article

Petrology of the Early Mesozoic ultramafic-mafic Luchina massif (southeastern periphery of the Siberian craton)

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

Journal: Russian Geology and Geophysics

Publisher: Novosibirsk State University

Published: 01 August 2008

Russ. Geol. Geophys. (2008) 49 (8): 570–581.

DOI: https://doi.org/10.1016/j.rgg.2007.12.008

...-sulfide Cu-Pd-Pt mineralization. A belt of layered massifs of this type is traceable in the eastern direction along the Mongolo-Okhotsk suture up to the Zharcha massif in Transbaikalia ( Izokh et al., 1998 ) and, possibly, father eastward. On geological schemes and maps, these massifs are dated either...

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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

...–Pt mineralization. A belt of layered massifs of this type is traceable in the eastern direction along the Mongol–Okhotsk suture up to the Zharcha massif in Transbaikalia ( Izokh et al., 1998 ) and, probably, father eastward. The association of the Lukinda massif with within-plate deposits...

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