Results 141 to 148 of about 630 (148)

THE “LEMVA CONGLOMERATES” OF THE SUBPOLAR URALS AND THEIR ERUPTIVE ORIGIN

International Geology Review, 1990
(1990). THE “LEMVA CONGLOMERATES” OF THE SUBPOLAR URALS AND THEIR ERUPTIVE ORIGIN. International Geology Review: Vol. 32, No. 11, pp. 1108-1119.
L. V. Makhlayev, A. M. Pystin
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The age of relief in northern, subpolar and polar Urals

International Geology Review, 1967
Reexamination of geological data available for the Northern, Subpolar and Polar Urals indicate that the relief of the area, originally considered to be ancient, is much younger in age. The absence of weathered crusts, Neogene deposits and other indirect evidence suggest a regional uplift of the area during the Neogene. -- IGR Staff.
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Thermometry saturation of apatite (the Kuzpuayu massif, the Subpolar Urals)

№ 27
The study of accessory minerals allows us to solve many questions of geology. Apatite can be used as a geochronometer (track method) and a geothermometer (apatite-biotite Ludington geothermometer, apatite Watson-Harrison geothermometer). Saturation thermometry of E. Watson and T. Harrison with the correction of F.
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Connoisseur's Choice: Brookite, Dodo Mine, Subpolar Urals, Russia

Rocks & Minerals, 2003
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History of accessory minerals from igneous rocks Subpolar Ural

ТЕНДЕНЦИИ РАЗВИТИЯ НАУКИ И ОБРАЗОВАНИЯ, 2019
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Upper Ludfordian black shales as indicators of euxinic conditions, Subpolar Urals

Geochemistry International, 2012
A. I. Antoshkina, O. V. Valyaeva, S. I. Isaenko, O. S. Prots’ko   +3 more
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Givetian deepwater sediments in the western slope of the Subpolar Urals

Doklady Earth Sciences, 2006
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The Inclusions in Zircon of the Kozhim Massif (The Subpolar Urals)

2023
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