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Paleoclimate Archives of Deep Caves of Mt. Velebit
2013Proučavanja špiljskih sedimenata kao paleoklimatskih arhiva teme su niza aktualnih studija u svijetu. Duboke jame Velebita (Paar i dr., 2008 ; Paar i dr., 2013) su kompleksni sustavi u kojima su zabilježene i sačuvane informacije o geološkim, geomorfološkim, hidrološkim i ekološkim uvjetima i procesima zbog čega predstavljaju odličnu sredinu za ...
Buzjak, Nenad +3 more
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Lias carbonate platform deposits of Velebit Mt. (Croatia)
1999At the Kubus-pass there are the sedimentary continuity from the uppermost part of the Lower Lias to the Middle and Upper Lias with a total thickness of ca 270 m. Liassic carbonates are divided into 5 lithofacies units: A = Rhythmically alternating mudstone/wackestone and ooid grainstone interpreted as a typical peritidal deposits with migration of ooid
Tišljar, Josip +3 more
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Stable isotope analysis of Mt. Velebit karst hydrological system
2015Mt. Velebit is a 145 km long mountain in the Croatian Dinaric Karst lying between Adriatic Sea and the Ličko and Gacko Polje fields. The massif is built of thick carbonate deposits from the upper Triassic, Jurassic and Cretaceous ages. In higher parts of the massif, the mentioned rocks are covered with younger Oligocene to Lower Miocene carbonate ...
Paar, Dalibor +4 more
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From doline distribution to tectonic movements (Velebit Mt. Croatia)
2001The influence of tectonic forces on the karst relief development has been studied using dolines as geomorphological markers. the strain and stress orientations have been calculated from the doline distribution applying the centre to centre method. 623 local results have been obtained which were later injected into 2D finite element model cretaed in ...
Faivre, Sanja, Reiffsteck, Philippe
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Middle Permian reef complex on the Velebit Mt.
1999The superimposed carbonate bodies are interpreted as ecological and morphological reef complex, based on their characteristic fossil association, body geometry and characteristic internal organisation. Sea level changes reflected themselves in aborting and resuming the reef growth.
Marjanac, Tihomir, Sremac, Jasenka
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Geology of the central Velebit Mt.
2004Velebit se u geološkom smislu, kao dio krških Dinarida i Jadranske karbonatne platforme, sastoji od sedimenata vrlo velikog raspona starosti: od karbona (oko 320 milijuna godina) pa do oligocena (oko 24 milujuna godina), ukupne debljine od gotovo 10.000 m.
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Some new potential subterranean glaciation research sites from Velebit Mt. (Croatia) [PDF]
, 2014 Despite the frequent reports about their shrinkage, detailed survey of the major subterranean ice deposits is still lacking in Croatia. Here we present cave maps and detailed description of cave ice accumulation from five caves of the Velebit Mt. Morphological constraints allowed ice volume estimation for four of them.
Buzjak, Nenad, Bočić, Neven
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Quaternary clastics of Jablanac cove in the foothills of the Velebit Mt.
1999Jablanac and its environs are composed of Paleogene-Neogene limestones and breccias. Quaternary sediments were deposited unconformably over thic Cenozoic basement. Quaternary sediments of Jablanac environs are represented by colluvial slope deposits, which are overlain by alluvial fans.
Marjanac, Tihomir, Marjanac, Ljerka
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Paleokarst and Caves of Velebit Mt., Dinaric karst of Croatia
2016In the Caves of North Velebit Mt. vertical shaft and meander morphology of vadose origin is largely prevailing, which points to single continuous phase of their speleogenesis. However, origin of large chambers, which are found in some of the Caves is not clear.
Paar, Dalibor +5 more
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Explorations in the region of Kita Gavranuša, Velebit Mt. Croatia.
2004We present results of speleological exploration and cave climate measurements in the caves of Kita Gavranusa region (Mt.Velebit), Croatia.
Paar, Dalibor +3 more
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