Отражение позднекиммерийской блоковой структуры в рельефе Днестровско-Прутского междуречья
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РОМАНОВ, Леонид. Отражение позднекиммерийской блоковой структуры в рельефе Днестровско-Прутского междуречья . In: Buletinul Institutului de Geologie şi Seismologie al AŞM, 2006, nr. 1, pp. 162-168. ISSN 1857-0046.
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Buletinul Institutului de Geologie şi Seismologie al AŞM
Numărul 1 / 2006 / ISSN 1857-0046

Отражение позднекиммерийской блоковой структуры в рельефе Днестровско-Прутского междуречья

Pag. 162-168

Романов Леонид
 
Институт геологии и сейсмологии АНМ
 
 
Disponibil în IBN: 16 decembrie 2013


Rezumat

The ring microstructure heat villages Kongaz and Bolshaya Kysylia is divided on two segments, which have been displaced in meridian-wise direction for 8 km. The displacement is not due to the horizontal movements. It is due to the Block structure of the area, which has been formed an late Cimmerian stage of tectogenesis.

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