Results 141 to 150 of about 542 (175)
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The Geomorphological Evolution of Dinarides

2006
Razrađena je geomorfološka problematika razvoja gorskog sustava Dinarida i razvoj zaravni u kršu.
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The problem of ophiolites of the Dinarids

International Geology Review, 1970
I. I. Belostotskiy, G. V. Kolbantsev
openaire   +1 more source

Erosional Surfaces in Outer Dinarides

2009
The present erosional surfaces on the Dinarides can be found at various levels (South-Istrian, North-Dalmatian, Zadvarska, Brotnjo-Dubrava, Lika’s, the erosional surface on Northern Velebit, on the mountain massifs of Èvrsnica, Bjelašnica, Treskavica, Durmitor, etc:) ; consequently, nearly from sea level to 1, 000 m and more than 2, 000 m above sea ...
Bognar, Andrija   +2 more
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Correlation of Neotethyan rifting related peperitic basaltic occurrences in the Dinarides, displaced fragments of the Dinarides and in the Hellenides

2010
Volcanological, mineralogical, petrological and geochemical studies on pillow lavas, peperites and hyaloclastite breccias as parts of basaltic extrusions of Triassic age into uconsolidated deep water sediments were carried out in the Jurassic mélange of the Darnó Unit (NE Hungary), which is a displaced fragment of the Dinarides.
Kiss, Gabriela   +3 more
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Metamorphic sole amphibolites from the Dinaride Ophiolite Zone (DOZ) and Sava- Vardar Zone (SVZ) of Dinarides

2001
The Dinaridic ophiolites occur in the DOZ, genetically related to MORB setting, and in the SVZ, genetically related to BARB environment. Varieties of amphibolites and related crystalline rocks are frequently associated with the Dinaridic ophiolites both in the DOZ and SVZ. In the central and north- western Dinarides, two compositionally and genetically
Balen, Dražen   +2 more
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Shear-wave velocity structure beneath the Dinarides from the inversion of Rayleigh-wave dispersion

Earth and Planetary Science Letters, 2021
Josip Stipcević, Petr Kolinsky
exaly  

Triassic Terrains of Adriatic and Dinarides (Croatia)

Bulletin of the Tethys Geological Society, 2007
Triassic terrains of Adriatic and Dinarides (Croatia) belong to the Late Pangea and Early Tethys time as proposed by Gaetani et al. (2003). They originated from area of maximum extension between Gondwana and Laurasia, i.e. future Apulia continental block.
Tari-Kovačić, Vlasta, Koch, Georg
openaire  

Triassic magmatism in Dinarides and its products

2008
Triassic rift related magmatism was dominantly of intermediate in character. It produced basalts, andesites and dacite at the extrusive level, and gabbro, diorite, granosyenite and granite in the intrusive levels and lasted at least 40 to 50 Ma. It is spatially and genetically related to the sedimentary formation of the Gondwana passive continental ...
Palinkaš, Ladislav   +2 more
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Southern Alps and Dinarides: overview

2008
A geological overview of the Southern Alps and Dinarids is provided.
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Outline of geology of Karst Dinarides

2008
U ovom radu daje se kratki prikaz geološke građe Dinarida, stratigrafija i tektonika. Prikazuju se glavne koncepcije podjele Dinarida, i njihovi argumenti.
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