Harmonization of structurally-geological and aerospace research to clarify and developmental Orekhovo-Pavlograd interblock zone of Ukrainian shield
2010; Linguagem: Inglês
10.3997/2214-4609.201402855
ISSN2214-4609
AutoresО.М. Пономаренко, A. T. Azimov, L. S. Os′mačko,
Tópico(s)Geotechnical and Geomechanical Engineering
ResumoOrekhovo-Pavlograd interblock zone (OPIZ) has evolved in few stages fault change rocks when sheared deformation in P-T conditions fixed their substance. Most intensively been submeridional the strike, subvertikal fall shifts in lower Proterozoic all the time and formed a final structural contour zone. Lineations deciphered according to RSE, within the OPIZ record not only sections of contemporary tectogenesis phases and repeat (to what extent segregationist) lower Pre-Cambrian structural anisotropy. Many of them in conjunction with the pivotal parts of ancient structures and boundaries between them. This mainly lower Proterozoic viscous fault zone. In General, with interblock zone differed uŝ megablocks thickness network submeridional fractures as ancient and modern phases tectogenesis. Polygonal and close ringwave deciphered objects surround block-relicts such within marked sliding zones. Internal anatomy of such blocks hybrid.
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