Results 171 to 180 of about 455 (191)
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ANISOTROPY OF ATTENUATION OF HIGH-FREQUENCY BODY WAVES IN THE SOUTHERN EXTERNAL DINARIDES

2018
The Dinarides are a part of the complex Alpine– Carpathian–Dinaric orogenic system characterised by NW trend and SW vergence of compressional and imbricated structures. The External Dinarides, their western part, is derived from the Adriatic microplate, i.e. the Adriatic carbonate platform.
Herak, Marijan   +2 more
openaire   +1 more source

Attenuation of high-frequency body waves and its anisotropy in the External Dinarides

2016
The Dinarides are situated in the broad Africa- Eurasia convergent plate boundary zone and are a part of the complex Alpine–Carpathian–Dinaric orogenic system. Due to the push of the African plate, the Adriatic microplate collides with the European plate in the north (the Alps), which has resulted in the formation of the Dinarides to the northeast. The
Dasović, Iva   +5 more
openaire   +1 more source

Structure and tectonic evolution of the Velebit Mt. in the central part of the External Dinarides

2019
Detailed outcrop-scale analysis of fault-slip data, in combination with data presented on published geological maps, were used for a reconstruction of the structural architecture and tectonic evolution of the Velebit Mt., the most prominent geomorphological structure in the central part of the External Dinarides in Croatia.
Tomljenović, Bruno   +7 more
openaire   +1 more source

Intrinsic and scattering attenuation of high-frequency S-waves in the central part of the External Dinarides

Physics of the Earth and Planetary Interiors, 2017
Josipa Majstorovic   +2 more
exaly  

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