Results 131 to 140 of about 1,323 (172)
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2007
Dan je popularni prikaz permske alge Mizzia Velebitana koja je prije točno 100 godina pronađena na Velebitu.
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Dan je popularni prikaz permske alge Mizzia Velebitana koja je prije točno 100 godina pronađena na Velebitu.
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Velebit Mt. Permian - Jurassic carbonates
2014U terenskom vodiču se opisuju stijene i facijesi u starosnom rasponu od srednjeg Perma do mlađe Jure koji su otkriveni na području srednjeg velebita.
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2007
The succession on Velebit Mt. provides evidence of shallow-marine deposition with several periods of emergence from the Late Carboniferous (Moscovian) to the Oligocene, when the dominant uplift phase took place. Quaternary deposits in highlands and valleys tell the story of the more recent geological history, including the Pleistocene glaciation.
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The succession on Velebit Mt. provides evidence of shallow-marine deposition with several periods of emergence from the Late Carboniferous (Moscovian) to the Oligocene, when the dominant uplift phase took place. Quaternary deposits in highlands and valleys tell the story of the more recent geological history, including the Pleistocene glaciation.
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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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