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Shubutuy Formation

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Journal Article
Published: 01 October 2017
Russ. Geol. Geophys. (2017) 58 (10): 1188–1198.
...S.I. Shkol’nik; V.A. Makrygina Abstract New data have been obtained on major- and trace-element compositions and Sm–Nd isotope systematics of clastic metasediments that belong to the Kornilova and Shubutui Formations in the Khamar-Daban terrane. The Kornilova Formation flysch derived from felsic...
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Geological position and structure of Solzan massif in the Khamar-Daban Ridg...
Published: 01 February 2014
Fig. 1. Geological position and structure of Solzan massif in the Khamar-Daban Ridge, borrowed from ( Makrygina et al., 2013 ). 1 , allochthonous granites; 2 , para-autochthonous granites; 3 , basic schists of the Shubutui Formation; 4 , aluminous schists of the Kornilova Formation; 5
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Kornilova and <span class="search-highlight">Shubutui</span> clastic metasediments in K 2 O&#x2F;Na 2 O– SiO 2 &#x2F;Al 2 O...
Published: 01 October 2017
Fig. 3. Kornilova and Shubutui clastic metasediments in K 2 O/Na 2 O– SiO 2 /Al 2 O 3 diagram. 1 , Kornilova Formation schists; 2 , Shubutui Formation schists. See fields of Phanerozoic graywacke-schist series with different quartz contents and post-Archean Australian Shale (PAAS) ( Taylor
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Patterns of trace elements ( a ) and REE ( b ) in Khamar-Daban Group clasti...
Published: 01 October 2017
Formation rocks; 2 , Shubutui Formation rocks.
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Bhatia diagram ( Bhatia and Crook, 1986 ) for metagraywacke.  1  — metapeli...
Published: 01 January 2007
metagraywackes of the Shubutui Formation, 6 — metapelites of the Kornilovka Formation of the Khamar-Daban Group. Arcs: A — oceanic, B — mature; margins: C — active, D — passive.
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ε Nd  age of clastic metasediments in Khamar-Daban and Dzhida terranes.  1–...
Published: 01 October 2017
Fig. 10. ε Nd age of clastic metasediments in Khamar-Daban and Dzhida terranes. 1–4 , Khamar-Daban terrane: Sludyanka Group ( 1 ), Khangarul Group ( Kovach et al., 2013 ) ( 2 ), Kornilova Formation, Khamar-Daban Group ( 3 ), Shubutui Formation, Khamar-Daban Group ( 4 ); 5 , Dzhida terrane, Zun
Journal Article
Published: 01 February 2014
Russ. Geol. Geophys. (2014) 55 (2): 177–189.
...Fig. 1. Geological position and structure of Solzan massif in the Khamar-Daban Ridge, borrowed from ( Makrygina et al., 2013 ). 1 , allochthonous granites; 2 , para-autochthonous granites; 3 , basic schists of the Shubutui Formation; 4 , aluminous schists of the Kornilova Formation; 5...
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Journal Article
Published: 01 January 2007
Russ. Geol. Geophys. (2007) 48 (1): 107–119.
... metagraywackes of the Shubutui Formation, 6 — metapelites of the Kornilovka Formation of the Khamar-Daban Group. Arcs: A — oceanic, B — mature; margins: C — active, D — passive. ...
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Simplified geology of Sludyanka–Utulik river catchments, simplified after (...
Published: 01 October 2017
Fig. 2. Simplified geology of Sludyanka–Utulik river catchments, simplified after ( Shafeev, 1970 ) ( a ) and stratigraphy of Khamar-Daban terrane ( b ). a : 1 , Cenozoic sediments; 2 , 3 , Khamar-Daban Group: Shubutui ( 2 ) and Kornilova ( 3 ) Formations; 4 , 5 , Khangarul Group
Journal Article
Published: 01 July 2016
Russ. Geol. Geophys. (2016) 57 (7): 1027–1039.
... of a narrow synclinal structure, is a vivid example of the relationship between the Early Paleozoic granitoids of the Khamar-Daban complex and the highly metamorphosed rocks of the Shubutui and Kornilova Formations. The eastern part of the massif, where migmatites and granitoids alternate with the metamorphic...
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Journal Article
Published: 01 February 2001
Russ. Geol. Geophys. (2001) 42 (2): 267–287.
... on the southern margin of the batholith. Sphene, apatite, magnetite, and zircon are abundant among the accessory minerals in monzogranitoids and granites of the main stage of batholith formation. The silica content does not exceed 65–67 % , potassium is predominant over sodium. Higher Ba, Sr, and LREE...
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