Features of development, lithology and minerals of apt-lower cretaceous and eocene continental deposits of the central part of ukrainian shield
DOI:
https://doi.org/10.15587/2313-8416.2015.47235Keywords:
Apt-lower cretaceous, Eocene, Central part of the Ukrainian shield, continental sediments, minerals.Abstract
The Apt-lower cretaceous and the river Eocene paleovalley of Central part of the Ukrainian shield spatial and paragenetic interrelated and are characterized by a similar genesis, lithology and set of minerals, formation, spatial, microfacies and lithofacies distribution which is due to geological and tectonic structure of the territory, and the paleogeographic conditions of paleo alluvial sedimentation. It is found that the origin and development of valleys of rivers caused by tectonic structure and geological development of the territory.
References
Veklich, N. F. (1966). Paleogeology areas of the Ukrainian shield. Kyiv.: Nauk. Dumka, 119.
Gasiewski, A. A. (1977). Surface Topography of the basement of the Ukrainian shield. Kyiv : GEOL. Phys, 37 (2), 99–107.
Gursky, S. D., Esipchuk, K. E., Kalinin, V. I. et. al (2005). Metallic and nonmetallic mineral resources of Ukraine, Kyiv. Lviv.: Metallic minerals, 1, 785.
Gursky, D. S., Esipchuk, K. Ju., Kalіnіn, V. І. et. al (2006). Metallic and nonmetallic mineral resources of Ukraine, Kyiv. Lviv : Non-Metallic minerals, 2, 552.
Illicheva, I. P. (1992.). Conditions of formation of the lower Cretaceous lithofacies complexes of the southern slope of the Ukrainian Shield: Candidate thesis in Geol. Kyiv, 210.
Kovalchuk, M. S. (1993). Lithology of the lower Cretaceous continental sediments of the northern slope of the central part of the Ukrainian Shield and origin of stream gravel of heavy minerals: Candidate thesis in Geol. Kyiv, 230.
(2001). Lithofacies, paleo geographic maps and maps of minerals distribution in Ukraine. Kyiv : State geological survey of Ukraine, 150.
Gevorkian, V. H. (1981). Lithology and mineralogical-geochemical characteristics of the lower Cretaceous deposits of the South of Ukraine, Kyiv : Nauk. Dumka, 276.
Zarutskyi, K. M., Vetrov, Ju. I., Zlobenko, I. F. (1980). On the gold findings in the alluvium of the low Cretaceous buried valleys of the central part of the Ukrainian Shield. Kyiv : Geological journal, 40 (3), 149–151.
Kovalchuk, M. S., Kroshko, Ju. V. (2012). Phanerozoic paleo alluvial sedimentological genesis within the Ukrainian Shield. Volodarsk Volynskyi.: Materials of the fifth All-Ukrainian science Conference “ The mineral wealth of Ukraine: Ways to optimal use”, 19–22.
Semeniuk, N. P., Zaruckij, K. M. (1992). Paleo-geomorphological criteria for prediction of gold deposits in the central part of the Ukrainian Shield. Kyiv : DAN Ukraine, 1, 84–86.
(2007). Tectonic map of Ukraine (a set of cards and an explanatory note) scale 1:1 000 000. Kyiv : UkrSGRI.
Kovalchuk, N. S. (2001). Features migration of gold in evolutionary genetics a number of residual weathered rock and gold-bearing placers. Kyiv.: Geological journal, 2, 94–102.
Gasiewski, A. A. (1982). Tectonic conditions of formation of minerals of the sedimentary cover of the Ukrainian shield. Kyiv : Nauk. Dumka, 180.
Gasiewski, A. A., Shevchenko, O. E. (1978). Cycles Meso-Cenozoic sedimentation in the Ukrainian shield, Kyiv : GEOL. Phys, 38 (6), 1–9.
Downloads
Published
Issue
Section
License
Copyright (c) 2015 Юлия Владимировна Крошко, Мирон Ковальчук Степанович
This work is licensed under a Creative Commons Attribution 4.0 International License.
Our journal abides by the Creative Commons CC BY copyright rights and permissions for open access journals.
Authors, who are published in this journal, agree to the following conditions:
1. The authors reserve the right to authorship of the work and pass the first publication right of this work to the journal under the terms of a Creative Commons CC BY, which allows others to freely distribute the published research with the obligatory reference to the authors of the original work and the first publication of the work in this journal.
2. The authors have the right to conclude separate supplement agreements that relate to non-exclusive work distribution in the form in which it has been published by the journal (for example, to upload the work to the online storage of the journal or publish it as part of a monograph), provided that the reference to the first publication of the work in this journal is included.
