Comparative analysis of residual soils of the shields of the East-European and the Siberian platform
Authors:
A.D. Dodatko, Dr. Sci. (Geol.-Min.), Professor, Professor of the Department of General and Structural Geology, State Higher Educational Institution “National Mining University”, Dnepropetrovsk, Ukraine
K.O. Zmiyevskaya, State Higher Educational Institution “National Mining University”, Postgraduate student of the Department of General and Structural Geology, Dnepropetrovsk, Ukraine
Abstract:
Due to the frequent occurrence of residual soils in the considered area of shields and platforms we received enough material for comprehensive study of the laws of mineralization and conditions of formation of thebresidual soils.
Purpose. To generalize regularities of formation of the residual soil, peculiarities of its structure and distribution within the shields of the East-European and the Siberian platforms, and to determine mineral deposits attached.
Methodology. Analysis and synthesis of research results of domestic scientists in the field of residual soils formation within the East-European and the Siberian platforms.
Findings. The generalities and distinctive features of the residual soils have been found out; the steps of the residual soils formation in the considered area have been determined; the association of ore deposits to zones of breaks or their crossings has been established.
Originality. For the first time the comparative analysis of the main characteristics of residual soils of the East-European and the Siberian platform has been performed.
Practical value. The common determinants and stages of the residual soils formation and the influence of faults on the formation process have been considered.
References:
1. Калашник А.А. Роль систем разломов в локализации оруденения / Калашник А.А. // Науковий вісник НГУ. – Дніпропетровськ; 2003. – №8. – С. 54–58. – Библиогр.: С. 100.
Kalashnik, A.A. (2003), “The role of fault systems in the localization of mineralization”, Naukovyi visnyk Natsionalnoho hirnychoho universytetu, no.8, pp. 54–58.
2. Омельченко В.В. Коры выветривания докембрийских образований северного склона Среднеприднепровского мегаблока Украинского щита / В.В. Омельченко, П.И. Пигулевский // Науковий вісник НГУ. – Дніпропетровськ, 2010.– №11–12. – С. 10–15. – Библиогр.: С. 139.
Omelchenko, V.V. and Pigulevskiy, P.I. (2010), “Residual soil of Precambrian formations of the northern slope of the Middle Dnieper megablock of the Ukrainian shield”, Naukovyi visnyk Natsionalnoho hirnychoho universytetu, no.11–12, pp. 10–15.
3. Додатко А.Д. Древние коры выветривания и методы их изучения / Додатко А.Д. – Дніпропетровськ: НГУ, 2004. – 103 с.
Dodatko, A.D. (2004), Drevniye kory vyvetrivaniya i metody ikh izucheniya [Ancient Residual Soils and Methods of their Study], NGU, Dnepropetrovsk, Ukraine.
4. Савко А.Д. Эволюция корообразования в истории Земли / А.Д. Савко, А.Д. Додатко // Россыпи и месторождения кор выветривания: факты, проблемы, решения. – Пермь, 2005. – С. 249–252.– Библиогр.: С. 359.
Savko, A.D. and Dodatko, A.D. (2005), “Evolution of residual soils genesis in the history of the Earth”, Proc. of the 13th Int. Geol. Symposium “Placers and deposits of residual soils: facts, problems and solutions”, Perm, Russia, 2005, pp. 249–252.
5. Орлинская О.В. Анализ пространственных взаимосвязей золоторудной минерализации в зеленокаменных структурах и систем разломов Среднего Приднепровья / О.В. Орлинская, Н.В. Билан // Науковий вісник НГУ. – Дніпропетровськ, 2003. – №9. – С. 50–52. – Библиогр.: С. 100.
Orlinskaya, O.V. and Bilan, N.V. (2003), “Analysis of spatial relationships in the gold mineralization of greenstone mining structures and systems of faults of the Middle Pridnieprovie”, Naukovyi visnyk Natsionalnoho hirnychoho universytetu, no.9, pp. 50–52.
2012_4_dodatko | |
2013-08-13 347.74 KB 1700 |