Науковий вісник НГУ

Activation periods of Kirovohrad protoplatform block (Ukrainian shield) and formation of diamond-bearing rocks

• 
• 

User Rating:  / 0

PoorBest 

Details

Category: Geology

Last Updated on 08 February 2016

Published on 08 February 2016

Hits: 4163

Authors:

O.V. Haiovskyi, Ivan Franko National University of Lviv, Assistant Lecturer of the Department of Mineral Deposits Geology, Lviv, Ukraine

Abstract:

Purpose. Reconstruction of the endogenous diamond-bearing formation stages in the geologic history of the Kirovohrad block (Ukrainian shield) protoplatform structure development for determination of possible diamonds sedimentary reservoirs geological age.

Methodology. Deep geological and geophysical studies of the lithosphere, the structural-tectonic analysis of the Precambrian basement, complex structural-formational division of geological bodies.

Findings. The Kirovohrad block of the Ukrainian shield refers to promising protoplatform diamond blocks due to localization of diamond structures and formations. It has been established that the geological and structural-tectonic preconditions of endogenous diamond-bearing rocks formation were laid in the Early Precambrian at the stage of protoplatform regime. They appeared on the stages of activation, which occurred from Middle Proterozoic till Paleocene in the Kirovohrad block. It is evidenced with lithological, structural and formational features, and age characteristics of rocks which are associated with diamond formations. Alluvial diamond concentration associated with young and modern Phanerozoic sedimentary formations have been caused by the destruction of ancient endogenous sources.

Originality. Geological, structural and epoch conditions of the Kirovohrad block diamond-bearing rocks formation have been considered through the general background of direct evolution development of the Earth crust in the Precambrian and Phanerozoic. Special attention is paid to the Precambrian period, because of favorable geological and structural-tectonic conditions for diamond-bearing rocks formations.

Practical value. Allocation of activation and diamond-bearing rocks formation epochs allows orienting forecast metallogenic studies and applying a number of important control factors during the search and exploration of this type of mineralization: geological-structural, geochronological, stratigraphic, lithological, paleogeographic. Taking into account space-time regular position of diamond-bearing formations while analyzing protoplatform structures it is possible to estimate the probability of diamonds presence on their territory and also to predict the diamond-bearingness of territory.

References:

1. Yatsenko, G.M., Bekesha, S.N., Hayovskiy, O.V. and Yatsenko, I.G. (2011), “Activation periods, ore-bearing structures and formations of lamproite type in the Archean and Proterozoic blocks of the Ukrainian shield. Article 2. Kirovograd block”, Mineralni Resursy Ukrainy, no 2, pp. 25–29.

Эпохи активизации, рудоносные структуры и формации лампроитового типа в архейских и протерозойских блоках Украинского щита. Статья 2. Кировоградский блок / Г.М. Яценко, С.Н. Бекеша, О.В. Гайовский, И.Г. Яценко // Мін. ресурси України – 2011. – № 2. – С. 25–29.

2. Haletskyi, L. and Naumenko, U. (2009), “End-to-end ore-concentrated megazones of activation: Ukrainian shield–Folded Carpathians”, Visnyk Lvivskoho Universytetu, seriya heolohichna, is. 23, pp. 71–81.

Галецький Л. Наскрізні рудоконцентрувальні мегазони активізації: Український щит–Складчасті Карпати / Л. Галецький, У. Науменко // Вісник Львів. ун-ту. Сер. геол. – 2009. – Вип. 23. – С. 71–81.

3. Fedoryshyn, Yu.I. (2007), “The model of forecast and search of native diamond bearingness sources and its realization on the territory of the Ukrainian shield”, Abstract of the Dissertation on competition of a scientific degree of the Doctor of Geological Sciences, Kyiv, 44 p.

Федоришин Ю.І. Модель прогнозу та пошуків джерел корінної алмазоносності і її реалізація на території Українського щита: автореф. дис. на здобуття наук. ступеня д-ра геол. наук / Федоришин Юрій Іванович. – К., 2007. – 44 с.

4. Kiryanov, N.N., Chernov, V.Yu. and Makivchuk, O.F. (1998), “Kimberlites of Kirovograd geoblock of the Ukrainian shield”, Abstracts of Ukr. Interagency Meeting “Geology and Stratigraphy of the Precambrian of the Ukrainian Shield”, Kyiv, pp. 96–98.

Кимберлиты Кировоградского геоблока Украинского щита / Н.Н. Кирьянов, В.Ю. Чернов, О.Ф. Макивчук [и др.] : Всеукр. міжвід. нарада: тези доп. // Геологія і стратиграфія докембрію Українського щита – К., 1998. – С. 96–98.

5. Yatsenko, G.M., Rosihina, A.I. and Slivko, E.M. (1997), “Problem of explosive ore formation in Krivoy Rog region”, Vidomosti AGN Ukrayiny, no 4, pp. 105–108.

Яценко Г.М. Проблема эксплозивного рудогенеза в Криворожье / Г.М. Яценко, А.И. Росихина, Е.М. Сливко // Відомості АГН України. – 1997. – № 4. – С. 105–108.

6. Nixon, P. and Leahy, K. (1997), “Diamond-bearing volcanoclastic kimberlites in Cretaceous marine sediments (Saskatchewan, Canada)”, Geologiya i Geofizika, vol. 38, no. 1, pp. 19–24.

2015_06_haiovskyi
2016-02-08  1001.97 KB  1224

• < Prev
• Next >