The structure of the Orekhovo-Pavlograd suture zone by paleogeographic, geological and geophysical data

Authors

  • Stanislav Yesypovych Scientific Centre for Aerospace Research of the Earth Institute of Geological Science National Academy of Sciences of Ukraine, Kyiv, Ukraine
  • Zinaida Tovstyuk Scientific Centre for Aerospace Research of the Earth Institute of Geological Science National Academy of Sciences of Ukraine, Kyiv, Ukraine
  • Olena Golovashchuk Scientific Centre for Aerospace Research of the Earth Institute of Geological Science National Academy of Sciences of Ukraine, Kyiv, Ukraine
  • Olena Rybak Scientific Centre for Aerospace Research of the Earth Institute of Geological Science National Academy of Sciences of Ukraine, Kyiv, Ukraine
  • Olena Skopenko Scientific Centre for Aerospace Research of the Earth Institute of Geological Science National Academy of Sciences of Ukraine, Kyiv, Ukraine
  • Galina Romashko Scientific Centre for Aerospace Research of the Earth Institute of Geological Science National Academy of Sciences of Ukraine, Kyiv, Ukraine
  • Iryna Lazarenko Scientific Centre for Aerospace Research of the Earth Institute of Geological Science National Academy of Sciences of Ukraine, Kyiv, Ukraine

DOI:

https://doi.org/10.36023/ujrs.2017.12.96

Keywords:

ooidringed stage, lineament analysis, seam rift zone, the cyclical geological processes, anomalies in the gravitationaland magnetic fields, radar satellite imagery

Abstract

The tectonic structure of the Orekhov-Pavlograd interblock zone of the Ukrainian shield is studied in this paper. This one has emerged since the 3600 million years ago, during the Katarchean/Archaean, ooidringed stage of the continental crust evolution. Its internal structure is described and anomalous features for future research are highlighted by comprehensive analysis of geological, geophysical, morphometric and remote sensed data.

References

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Published

2017-05-11

Issue

No. 12 (2017)

Section

Earth observation data applications: Challenges and tasks

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