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Inner Dinarides revisited: Opening and closure of a Neotethys branch in Western Serbia
The Dinarides mountain belt of south-east Europe represents a segment of a complex Mesozoic large-scale foldand thrust belt situated between the Southern Alps in the NW and the Hellenides in the SE. The Dinaride foldand thrust belt contains continental units of Adriatic/Apulian affinity, as well as several Neotethyan ophiolitecomplexes situated in ...Barjaktarovic, Miljan +3 more
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Palaeogeography, Palaeoclimatology, Palaeoecology, 2007
Abstract In the Jurassic, the Caucasus, presently located in the southwest of Russia, Georgia, Armenia and Azerbaijan, was located on the northern active margin of the Neotethys Ocean. Facies interpretation in all 62 areas, distinguished by differences in facies, allows to semi-quantitatively evaluate Jurassic regional transgressions and regressions ...
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Abstract In the Jurassic, the Caucasus, presently located in the southwest of Russia, Georgia, Armenia and Azerbaijan, was located on the northern active margin of the Neotethys Ocean. Facies interpretation in all 62 areas, distinguished by differences in facies, allows to semi-quantitatively evaluate Jurassic regional transgressions and regressions ...
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Planktonic foraminifera from the Oligocene deposits of the Central Neotethys
2012Za detaljna mikropaleontološka istraživanja odabrani su uzorci iz tri duboke istražne bušotine (Istra more-3 i Istra more-4, jugoistočni dio Venecijanskog bazena i bušotina Jadran-252/1, Dugootočki bazen). Iz uzoraka krhotina stijena sa sita i iz jezgrovanih intervala izdvojene su i opisane dobro sačuvane zajednice foraminifera.
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Metamorphic soles consist of metamorphosed oceanic crustal and pelagic sedimentary rocks that structurally underlie the mantle section of supra-subduction zone (SSZ) ophiolites. Both are considered geological records of subduction initiation: soles record the juvenile history of a subduction plate interface and the overlying SSZ ophiolites record the ...
Kalijn Peters +11 more
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Kalijn Peters +11 more
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Late Cretaceous to Oligocene Larger Miliolids in the Neotethys and in the Caribbean
2005Larger miliolids are defined by having trematophores aligned according to a single apertural axis. There are two minly groups of larger miliolids characterized by a different architecture of the endoskeleton in the microscopic generation: the lacaziniform genera by a compact basal layer bearing ribs, rows of radial pillars or continuous septula ...
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