Limits on Arbitration Outside Croatia: According to the Croatian Arbitration Act

Babić, Davor

doi:10.2139/ssrn.1974413

Cited by 1 publication

(5 citation statements)

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“…It comprises Upper Triassic to Upper Cretaceous shallow marine, slope and deep-marine carbonates which are unconformably overlain by Upper Cretaceous clastics (Blanchet et al 1970;Babic ´1973, 1974; Dragic ˇevic ´and Velic ´2002). Here, siliciclastic deposition was initiated earlier than in the External Dinarides further SW (Blanchet et al 1970;Babic ´1974). In the Central Dinarides these clastics have been designated as the Ugar Formation, which is dominated by clastic carbonate, typically consisting of thin-bedded marls, calcarenites and sandstones, as well as thick carbonate mass flow deposits.…”

Section: Geological Outline Of the Dinaridesmentioning

confidence: 90%

“…2; Babic ´1974; Zupanic ˇ1981). Babic ´(1974) reported an Albian-Cenomanian age for the Kravljak Formation deposits, which overlie various Upper Triassic to Lower Cretaceous carbonates (Fig. 3).…”

Section: Stratigraphy Sedimentology and Composition Of The Cretaceous...mentioning

confidence: 99%

“…11b). Various lithoclasts of Triassic, Jurassic and Lower Cretaceous carbonate rocks within the Barremian to Cenomanian calcarenites and calcirudites of the NW Dinarides (Os ˇtrc and Kravljak formations) prove that the Mesozoic cover of the imbricated Adriatic basement was actively eroded during pro-wedge deposition (Babic ´1974;. This compares well to evidence from other parts of the Eastern Alps-Dinarides (Csontos et al 2005; see also Charvet 1978Charvet , 1980; Csa ´sza ´r and A ´rgyela ´n 1994; Gardin et al 1996;Mikes et al 2008;Schlagintweit et al 2008;Marroni et al 2009).…”

Section: Early Cretaceous To Cenomanianmentioning

confidence: 99%

“…Nappe propagation caused siliciclastic sedimentation to migrate towards more external parts of the Adria plate (Kravljak Formation), reaching the margin of the Adriatic Carbonate Platform in the Albian-Cenomanian (Fig. 11b; Babic ´1974;Luz ˇar-Oberiter, 2009). It is possible that parts of the Early Cretaceous clastic basins (Os ˇtrc and Bistra formations) were incorporated into the propagating nappes, although in light of the heavy mineral and ZFT data, Late Cretaceous recycling of Lower Cretaceous clastics was not significant.…”

Section: Early Cretaceous To Cenomanianmentioning

confidence: 99%

“…The remnants of these basins, exposed in northern Croatia, document the early evolution of the Dinaride orogen which has been heavily masked by Cenozoic deformation. Based on detailed petrography, litho-and biostratigraphy, previous work has already assessed the general paleogeography and sedimentary provenance of these basins, suggesting that they represent different paleogeographic settings (Babic ´et al , 2002Babic ´1974;Crnjakovic ´1979, 1981Crnjakovic ´1979, , 1989Luz ˇar-Oberiter 2009). More recently, detrital Cr-spinel chemistry revealed additional details with respect to the ophiolites obducted onto the margin of the Adria plate (Luz ˇar-Oberiter et al 2009).…”

Section: Introductionmentioning

confidence: 99%

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Provenance of Cretaceous synorogenic sediments from the NW Dinarides (Croatia)

Lužar-Oberiter

Mikes

Dunkl³

et al. 2012

Swiss J Geosci

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Scarce basin remnants of Cretaceous synorogenic sediments exposed in the Medvednica, Ivans ˇc ˇica, Z ˇumberak Mts. and Samobor Hills of northern Croatia record the early orogenic history of the NW Dinarides. The provenance of sandstones from five clastic formations (Os ˇtrc, Bistra, Kravljak, Vivodina and Glog) which cover a time span from Early to late Late Cretaceous was studied by combining petrography, whole-rock geochemistry, heavy mineral chemistry and detrital zircon fission track dating. These sediments record at least two major regional thermotectonic events which correlate well with those affecting both the Alps and the Tisza-Dacia unit to the north and east, and the central Dinaride region to the south. Short zircon fission track lag times in Barremian to Albian sediments indicate that continental fragments of the distal Adria plate margin underwent relatively fast, synsedimentary exhumation in the Early Cretaceous. Moreover, a clear dominance of Campanian zircon cooling ages (80-73 Ma) in Maastrichtian sandstones indicates detritus deriving from the erosion of newly and rapidly exhumed basement units which had undergone Late Cretaceous metamorphism in the Eastern Alps and/or the Tisza-Dacia region. Probably, the rapid Maastrichtian erosion generating metamorphic detritus occurred to a great extent on neighbouring Austroalpine basement units, and/or on the upper plate Tisza-Dacia unit during the subduction stage or the initial stages of the continent-continent collision with Adria. Development of the accretionary wedge probably resulted in a renewed availability of ophiolites for erosion within small and/or dynamically changing catchments, which can be deduced from the notable differences in reconstructed source lithologies for the coeval Glog and Vivodina formations. Combined evidence from sedimentary provenance indicators precludes the Dinaride (Adriatic) basement as a significant source for the Maastrichtian sediments.

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Section: Geological Outline Of the Dinaridesmentioning

confidence: 90%

Section: Stratigraphy Sedimentology and Composition Of The Cretaceous...mentioning

confidence: 99%