Peculiarities of the composition of the high-titanium ultramafite dyke in the Andriivka open pit (the Eastern Azov area of the Ukrainian shield)

Author:

Gatsenko V.O., ,Kryvdik S.G.,Kushnir S.V., ,

Publisher

National Academy of Sciences of Ukraine (Co. LTD Ukrinformnauka)

Reference10 articles.

1. 1. Hatsenko V., Andrieiev O. (2018). Pyroxenes from the rocks of Pokrovo-Kyryivskyi massif: features of morphology and chemical composition. Mineralogical collection. Iss. 68, No. 1, pp. 99-102 [in Ukranian].

2. 2. Glevassky E.B., Krivdik S.G. (1985). The Belt of Pre-Cambrian Dikes of Alkaline Metaultrabasites in the Western Part of the Azov Area. Geol. Journ. 45, No. 4, pp. 58-63 [in Russian].

3. 3. Kryvdik, S.G. and Tkachuk, V.I. (1990). Petrology of alkaline rocks of the Ukrainian Shield. Kyiv, Nauk. dumka. 408 p. [in Russian].

4. The impact of the contact subalkaline gabbroids (mafites) of Pocrovo- Kyriyv massif in alkaline granites;Kryvdik;Geol,2016

5. 5. Kryvdik S.G., Sharygin V.V., Gatsenko V.O., Lunev E.S. (2016). Pyroxene of the Pokrovo-Kyriyivo massif (Azov Sea region, Ukraine). Mineral. Journ. (Ukraine). 38, No. 3, pp. 24-38 [in Ukranian].

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