Features of development, lithology and minerals of apt-lower cretaceous and eocene continental deposits of the central part of ukrainian shield

Authors

  • Юлия Владимировна Крошко Institute of geological sciences, NAS of Ukraine Str. O. Honchar, 55-b, Kyiv, Ukraine, 01054, Ukraine
  • Мирон Степанович Ковальчук Head of the Department of lithology Str. O. Honchar, 55-b, Kyiv, Ukraine, 01054, Ukraine

DOI:

https://doi.org/10.15587/2313-8416.2015.47235

Keywords:

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.

Author Biographies

Юлия Владимировна Крошко, Institute of geological sciences, NAS of Ukraine Str. O. Honchar, 55-b, Kyiv, Ukraine, 01054

Department of Lithology

Junior Researcher

Мирон Степанович Ковальчук, Head of the Department of lithology Str. O. Honchar, 55-b, Kyiv, Ukraine, 01054

Doctor of geological Sciences 

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Published

2015-07-27

Issue

Section

Geological and geographical sciences