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Solovieva Gora

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Journal Article

VARIATIONS IN ELECTRICAL RESISTANCE OF DUNITES AS A FUNCTION OF TEMPERATURE AND SERPENTINIZATION DEGREE ( example of Urals )

V.V. Bakhterev, L.D. Bulykin
Published: 01 October 2002
Russ. Geol. Geophys. (2002) 43 (10): 960–967.
... in the Ural PGE-bearing belt (Solovieva Gora). The obtained functions show temperature-dependent behavior of electrical resistance in the range of 20 to 800 °C and a dependence of the activation energy of ions on the degree of early serpentinization of dunites. The serpentinization-dependent activation energy...
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Journal Article

EARLIEST ARTINSKIAN (EARLY PERMIAN) FUSULINIDS REWORKED IN THE TRIASSIC LERCARA FORMATION (NW SICILY)

Daniel Vachard, Rossana Martini, Louisette Zaninetti
Published: 01 January 2001
Journal of Foraminiferal Research (2001) 31 (1): 33–47.
DOI: https://doi.org/10.2113/0310033
... by Kahler (1980 and 1985) and Flügel (1986b). The clasts of this breccia contain numerous algae and pseudo-algae (according to Flügel 1986b), but no fusulinid. Questionable Murgabian Misellina have also been mentioned in Yugoslavia (southern Crna Gora) by Kochansky-Devidé (1975...
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Book Chapter

Russian regional Carboniferous stratigraphy

Author(s)
Alexander S. Alekseev, Svetlana V. Nikolaeva, Nataliya V. Goreva, Nina B. Donova, Olga L. Kossovaya, Elena I. Kulagina, Nadezhda A. Kucheva, Alena V. Kurilenko, Ruslan V. Kutygin, Lyudmila I. Popeko, Tatyana I. Stepanova
Book: The Carboniferous Timescale
Series: Geological Society, London, Special Publications
Publisher: Geological Society of London
Published: 13 April 2022
DOI: 10.1144/SP512-2021-134
EISBN: 9781786205827
... , p. 118; 1932 ). The type area is the western slope of the Middle Urals, the eastern part of the Perm Region. The stratotype is considered to be a section on Ivanovskaya Gora near the village of Lunevka, 3–4 km east of the city of Aleksandrovsk in the Perm Region; at present, several open pits...
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Abstract
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Abstract Several existing schemes for Carboniferous stratigraphy officially adopted in regions of the Russian Federation are summarized and discussed. These regions with different geological histories and distinct depositional settings include the Moscow Basin, the Urals, North Timan, Siberia, the Kuznetsk Basin and the Mongol–Okhotsk, Verkhoyansk–Okhotsk and Kolyma–Omolon regions. Broad correlations based on macro- and microfossils are possible between the regions, while all regional schemes are correlated to the official Russian General Stratigraphic Scheme for the Carboniferous, using zonations based on orthostratigraphic fossils. The Russian General Stratigraphic Scheme is correlated to the International Stratigraphic Scale using ammonoids, conodonts, foraminifers and palynomorphs.