The nature and age of the Suroyam clinopyroxenite massif (Middle Urals)

The nature and age of the Suroyam clinopyroxenite massif (Middle Urals)

The Suroyam alkaline ultrabasite syenite (mainly pyroxenite) massif, including the Suroyam apatite titanomagnetite deposit, is a part of the Nyazepetrovsk structural-formational zone located on the western slope of the Middle Urals, within the Ufimskii promontory of the East European Platform. The s...

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Bibliographic Details
Published in:Doklady earth sciences Vol. 431; no. 1; pp. 294 - 298
Main Authors: Puchkov, V. N., Zhilin, I. V., Ronkin, Yu. L., Volchenko, Yu. A., Lepikhina, O. P.
Format: Journal Article
Language:English
Published: Dordrecht SP MAIK Nauka/Interperiodica 01-03-2010
Springer
Springer Nature B.V
Subjects:
Basalt
Earth and Environmental Science
Earth Sciences
Geology
Mineralogy
Petrology
Phosphate minerals
Phosphate rock
Sedimentation & deposition
Siliceous rocks
Stratigraphy
Tectonics (Geology)
Ural Mountains
Apatite
Devonian
Ordovician
DOKLADY Earth Science
86Sr
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Summary:The Suroyam alkaline ultrabasite syenite (mainly pyroxenite) massif, including the Suroyam apatite titanomagnetite deposit, is a part of the Nyazepetrovsk structural-formational zone located on the western slope of the Middle Urals, within the Ufimskii promontory of the East European Platform. The stratigraphic section of the Nyazepetrovsk zone is represented by volcanic and volcanogenic sedimentary formations with subordinate siliceous rocks, siltstone, and sandstones. The section is distinguished into three formations (from ancient to young): basalt, basalt-andesite-basalt, and trachybasalt-trachyte.
ISSN:1028-334X
1531-8354
DOI:10.1134/S1028334X10030062