The Two Stages of Structural Formation of the Coastal Belt of the External Dinarides
Item
Title (Dublin Core)
eng
The Two Stages of Structural Formation of the Coastal Belt of the External Dinarides
Description (Dublin Core)
eng
Two successive stages of tectonism have been responsible for the formation of structures in the coastal part of the External Dinarides. As a result, Dinaride- and Hvar-striking structures formed, showing NW-SE and E-W strike orientation, respectively. Besides the great diversity in the geological and geophysical characteristics and intensive disruption, the coastal area represents a cohesive geotectonic unit, showing a uniform geodynamic evolution that is here confirmed by laboratory modelling.
Creator (Dublin Core)
Blašković, I.
Subject (Dublin Core)
eng
Tectonics; Dinaride-striking structures; Hvar-striking structures; Mt. Velebit; External Dinarides; Croatia
Publisher (Dublin Core)
Croatian Geological Survey
Date (Dublin Core)
1998
Type (Dublin Core)
text
info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
Format (Dublin Core)
application/pdf
Identifier (Dublin Core)
https://hrcak.srce.hr/3916
eng
https://hrcak.srce.hr/file/6417
Source (Dublin Core)
Geologia Croatica
ISSN 1330-030X (Print)
ISSN 1333-4875 (Online)
Volume 51
Issue 1
Language (Dublin Core)
eng
Rights (Dublin Core)
info:eu-repo/semantics/openAccess
Full text of articles are freely accessable. Subscription to print issue is 500,00 Kn (80 Eur) per volume.