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Akademický článek

Evolution of the Southern Margin of the Julian Basin with Emphasis on the Megabeds and Turbidites Seqence of the Southern Julian Prealps (NE Italy)

Autor: Giorgio Tunis, Sandro Venturini

Publikováno v: Geologia Croatica, Vol 45, Iss 0, Pp 127-150 (2010)

From the Maaslrichtian up to the Early Eocene, the Julian (or Slovenian) Basin is characterized by a mixed siliciclastic/carbonale deposits system which exhibit complex sedimentalion patterns depending on various controls: sea level changes; tectonic

Externí odkaz: https://doaj.org/article/67468db86b68489ab872f48f838c49e1

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Akademický článek

The Buzet Thrust Fault in Istria and overturned carbonate megabeds in

Autor: Ladislav Placer, Adrijan Košir, Tomislav Popit, Andrej Šmuc, Grega Juvan

Publikováno v: Geologija, Vol 47, Iss 2, Pp 193-198 (2004)

Detailed geological mapping undertaken in the framework of monitoring of the motorway construction works in SW Slovenia has revealed the existence of a large-scale thrust fault between Buzet and Koper (termed the Buzet Thrust Fault) and extensive thr

Externí odkaz: https://doaj.org/article/ea95bba7576f4c24908dfffb9d2c8f88

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Geological Model of Pićan Area, Istria

Autor: Petrinjak, Krešimir, Bergant, Stanislav, Belić, Nikola, Frangen, Tihomir

During geological mapping of Istria (Croatia) numerous carbonate beds (megabeds) were recorded within the informal lithostratigraphic unit Istrian flysch. Istrian flysch deposits are mostly characterized by typical alternations of hemipelagical marl

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::7a549595cb8a1a2db8eb8bb2e7d73002
https://repozitorij.hgi-cgs.hr/islandora/object/hgi:7/datastream/FILE0

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Mass-transport deposits and the onset of wedge- top basin development: An example from the Dinaric Foreland Basin, Croatia

Autor: Ervin Mrinjek, Vlasta Ćosović, Katarina Gobo

Mass-transport deposits (MTDs) represent resedimentation phenomena triggered by the combined effect of seismic shocks of regional scale, structural tilting, basin-floor gradient, relative sea-level fluctuations, and/or excess pore-water pressure and

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::15d13e47b8f35661d37da1882c748d82
https://www.bib.irb.hr/1098054

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Variability of CaCO3 content in Central Dalmatian Flysch basin turbidites

Autor: Kosanović, Hrvoje

Ovaj radi bavi se istraživanjem kako se mijenja udio CaCO3 u lutitskom dijelu megaslojeva u srednjedalmatinskom fliškom bazenu i to u Solinskom sub-bazenu. Analizirani su uzorci prikupljeni prilikom sedimentoloških istraživanja, i to olistostrome

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=od______3908::882f8bdbbee4150e1806d3b653fdf5e9
https://repozitorij.pmf.unizg.hr/islandora/object/pmf:4808

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Carbonate Olistolites and Megabeds in Middle to Upper Eocene Promina beds between Smilčić and Benkovac (Northwestern Dalmatia)

Autor: Zidar, Mislav

Srednje do gornjoecenska formacija Korlat koja se pruža se duž jugozapadnog ruba Prominskog bazena predstavlja najstariji dio Prominskih naslaga. Najveći dio od oko 600 m debele formacije su heterolitski slojevi izgrađeni od vrlo dobro uslojenih

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=od______3908::2b4a61eaf8ea3ac589c89107b4892228
https://repozitorij.pmf.unizg.hr/islandora/object/pmf:4271

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Transformation, partitioning and flow–deposit interactions during the run-out of megaflows

Autor: Paulo Sérgio Gomes Paim, Ben Kneller, Juan Pablo Milana, Claus Fallgatter

Four megabeds (I to IV) were recognized throughout the Cerro Bola inlier, a glacially influenced depositional area of the Carboniferous Paganzo Basin, south-western La Rioja Province, Argentina. Such anomalous thick beds are associated with the colla

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4181168030740da26b29b52a94eb03c2
Wiley Online Library

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Akademický článek

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Carbonate olistoliths and megabeds within Middle to Upper Eocene Promina deposits: A sedimentary response to thrusting and fold growth in the Dinaric foreland Basin

Autor: Mrinjek, Ervin, Pencinger, Vili, Vlahović, Igor, Velić, Ivo, Velić, Josipa, Bergant, Stanislav, Mikša, Goran, Matičec, Dubravko, Prtoljan, Božo

Cjeloviti sažetak priložen je upisu.

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=57a035e5b1ae::248bd3e656a7464a251d5e8022bf6000
https://www.bib.irb.hr/486658

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Late Eocene megabed with glass sphaerules and microtectites in eastern Adriatic flysch (Croatia)

Autor: Marjanac, Tihomir, Bermanec, Vladimir, Premec-Fuček Vlasta

Glass sphaerules occur at 4 levels in Late Eocene marls of Central Dalmatian (Eastern Adriatic) flysch basin. The best studied, and with most sphaerules recovered is a composite turbidite 2-7, which is the youngest in the sequence and belongs to Turb

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=57a035e5b1ae::4fd9834f4a8457576a5756e98ebbd332
https://www.bib.irb.hr/180054

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