Get 20M+ Full-Text Papers For Less Than $1.50/day. Start a 14-Day Trial for You or Your Team.

Learn More →

The West Black Sea passive continental margin in the east part of Balkan Peninsula

The West Black Sea passive continental margin in the east part of Balkan Peninsula AbstractThe Black Sea Neozoic passive continental margin marks the natural „bridge” between the Moesian and Bulgarian continental microplates and the Black Sea oceanic microplatte. It was coming in to being after the saturation between the terrains which are composed the Neo Europe south east part during the Early Paleogene. The subaerial part of the margin includes the most east parts of the South Moesian, Hemus, and Upper Thracian and Sakar-Strandzha morphostructural zones. The subaquatic part of the margin is composed by the consequently orderly step lower to the Black Sea bottom: high shelf zone, lover shelf zone, continental slope and continental foot. The Black Sea Neozoic passive continental margin is characterized by low seismic activity. It is concentrated in some fault zones. http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Acta Scientifica Naturalis de Gruyter

The West Black Sea passive continental margin in the east part of Balkan Peninsula

Loading next page...
1
 
/lp/degruyter/the-west-black-sea-passive-continental-margin-in-the-east-part-of-vXr22wjPAz

References (17)

Publisher
de Gruyter
Copyright
© 2018 Svetla Stankova et al., published by De Gruyter Open
eISSN
2367-5144
DOI
10.2478/asn-2018-0014
Publisher site
See Article on Publisher Site

Abstract

AbstractThe Black Sea Neozoic passive continental margin marks the natural „bridge” between the Moesian and Bulgarian continental microplates and the Black Sea oceanic microplatte. It was coming in to being after the saturation between the terrains which are composed the Neo Europe south east part during the Early Paleogene. The subaerial part of the margin includes the most east parts of the South Moesian, Hemus, and Upper Thracian and Sakar-Strandzha morphostructural zones. The subaquatic part of the margin is composed by the consequently orderly step lower to the Black Sea bottom: high shelf zone, lover shelf zone, continental slope and continental foot. The Black Sea Neozoic passive continental margin is characterized by low seismic activity. It is concentrated in some fault zones.

Journal

Acta Scientifica Naturalisde Gruyter

Published: Mar 1, 2018

There are no references for this article.