Zobrazeno 1 - 10
of 21
pro vyhledávání: '"Jožica Zupanič"'
Autor:
Ljubomir Babić, Jožica Zupanič
Publikováno v:
Geologia Croatica, Vol 65, Iss 1, Pp 1-27 (2012)
The Palaeogene Promina Beds (PB), exposed in the Dinaric coastal range, is about a 2km thick heterogeneous succession representing a late sedimentary fill of the North Dalmatian foreland basin. The paper focuses on the middle part of the PB represen
Externí odkaz:
https://doaj.org/article/b38b2555bf8640118a44fad4c978ef03
Autor:
Jožica Zupanič, Ljubomir Babić
Publikováno v:
Geologia Croatica, Vol 64, Iss 2, Pp 101-120 (2011)
Mt. Promina became famous for its coal mines, vertebrate remains and fossil flora, and for the use of its name in denoting sediments covering a wide area of the Dinaric coastal range. Up to 1 km thick Promina Beds of the type area, Mt. Promina, evolv
Externí odkaz:
https://doaj.org/article/3131c04dbbe049969f333095920fe272
Publikováno v:
Geologia Croatica, Vol 46, Iss 1, Pp 107-123 (2010)
The Eocene clastics of the NW part of the island of Pag overlie carbonate platform deposits and are dominantly sandy. Besides minor components, they include cross-laminated and cross-bedded sandstones produced by marine tractive flows, mostly directe
Externí odkaz:
https://doaj.org/article/e1f41b86452342a5a99c30acbec7fa1d
Publikováno v:
Geologia Croatica, Vol 48, Iss 1, Pp 33-48 (2010)
The upper part of the Promina Beds at their western extent is represented by two alluvial units: the Kunovac Beds and the Upper Alluvial Unit. The Kunovac Beds contain a high proportion of fine-grained sediments, and generally lacks debris flow depos
Externí odkaz:
https://doaj.org/article/e165302f55c148cab49d0bb6c9d4bbd4
Nearshore Deposits in the Middle Eocene Clastic Succession in Northern Dalmatia (Dinarides, Croatia)
Autor:
Ljubomir Babić, Jožica Zupanič
Publikováno v:
Geologia Croatica, Vol 51, Iss 2, Pp 175-193 (2010)
The Middle Eocene clastic sliccess ion in the Radovin Syncline isapproximate ly 900 m thick and consists of hemipelag ic and nyschtypedepos its in its lower part, and shallow-marine sediments in itsupper portio n. The upper portion embraces a unit of
Externí odkaz:
https://doaj.org/article/25fad50952c247148df872de991de827
Publikováno v:
Geologia Croatica, Vol 55, Iss 1, Pp 25-37 (2002)
The following types of calcified deposits characterize Holocenewaterfall tufas in the Zrmanja river: mossy deposits, algally laminatedcrusts and algally coated grains. Petrological examination revealed,that abundant organic remains belonging to mosse
Externí odkaz:
https://doaj.org/article/12b36a320d4a4b55ae6e922b8846511d
This study deals with sand beaches of the SE Adriatic archipelago and Peljesac Peninsula. The beaches themselves, as well as their genetically related surroundings are taken into consideration, as both are critical for understanding beach features an
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::232d095b5123fb3778c11dad613a8acc
https://doi.org/10.1016/j.ecss.2019.106294
https://doi.org/10.1016/j.ecss.2019.106294
Autor:
Jožica Zupanič, Ljubomir Babić
Publikováno v:
Natura Croatica. 25:55-71
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f092f36819f6a72e6ca664e8f9f01a84
https://doi.org/10.20302/nc.2016.25.3
https://doi.org/10.20302/nc.2016.25.3
Sand beaches of the Eastern Adriatic Croatian coast present an important natural and economic resource, which is under increasing pressure from development. The composition of sand from 13 pocket beaches of SE Adriatic islands and neighboring Pelješ
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e8272f7f4eed719a124ec4a015025780
https://www.bib.irb.hr/999049
https://www.bib.irb.hr/999049
Autor:
Ljubomir Babić, Jožica Zupanič
Publikováno v:
Natura Croatica : Periodicum Musei Historiae Naturalis Croatici
Volume 25
Issue 1
Volume 25
Issue 1
The paper provides a description of the poorly known Upper Nummulitic Limestones exposed in the North Dalmatian foreland basin of the Outer Dinarides in Croatia. This formation originated on a land-attached ramp-type platform with a temperate sedimen
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______951::437998bb64b0408dec326e530b97693c
https://hrcak.srce.hr/160558
https://hrcak.srce.hr/160558