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MAFIC INCLUSIONS (SOBSKY COMPLEX, POLAR URAL): U‐Pb (SIMS) DATA

https://doi.org/10.5800/GT-2019-10-2-0414

Abstract

The rocks of the Sobsky complex, composing the bulk of the Sobsky batholith in the Polar Urals, contain mafic inclusions. The geological, petrographic and petro‐geochemical data show that the mafic inclusions of the Sobsky rocks belong to igneous formations, which are similar in their characteristics to autoliths. According to all the characteristics, these are the structures non‐contrasting to host rocks and having different structural‐textural features, a more basic composition of minerals and a more basic composition of rocks. The contact with the rocks of the complex is sharp and clear. The rocks of the complex in contact with autoliths are medium‐grained massive diorite rocks, quartz diorites, tonalites, mafic inclusions rocks – fine‐grained gabbros, gabbro‐diorites, and diorites. Isotopicgeochemical (U‐Pb, SIMS) data on zircons from the mafic inclusions suggest that their age is close, within the error limits, to the age of zircons from the enclosing Sobsky complex rocks.

About the Authors

О. V. Udoratina
N.P. Yushkin Institute of Geology of Komi Science Center, Ural Branch of RAS; Tomsk State University
Russian Federation

Oksana V. Udoratina - Candidate of Geology and Mineralogy

54 Pervomayskaya street, Syktyvkar 167982, 

50 Lenin ave., Tomsk 634050



М. A. Coble
Stanford University
United States

Matthew A. Coble - PhD, Research and Development Scientist and Engineer

Department of Geological Sciences Stanford, California 94305



A. S. Shuyskiy
N.P. Yushkin Institute of Geology of Komi Science Center, Ural Branch of RAS
Russian Federation

Aleksander S. Shuyskiy

54 Pervomayskaya street, Syktyvkar 167982



V. A. Kapitanova
N.P. Yushkin Institute of Geology of Komi Science Center, Ural Branch of RAS
Russian Federation

Valentina A.Kapitanova  

54 Pervomayskaya street, Syktyvkar 167982



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For citations:


Udoratina О.V., Coble М.A., Shuyskiy A.S., Kapitanova V.A. MAFIC INCLUSIONS (SOBSKY COMPLEX, POLAR URAL): U‐Pb (SIMS) DATA. Geodynamics & Tectonophysics. 2019;10(2):265-288. (In Russ.) https://doi.org/10.5800/GT-2019-10-2-0414

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