Pregled bibliografske jedinice broj: 146693
The Eocene Bioherms and the Associated Lithofacies in Western Herzegovina (Yugoslavia)
The Eocene Bioherms and the Associated Lithofacies in Western Herzegovina (Yugoslavia) // Proceedings - 8th IAS Regional Meeting of Sedimentology / -- (ur.).
Tunis: International Association of Sedimentologists (IAS), 1987. str. 199-204 (poster, nije recenziran, sažetak, znanstveni)
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Naslov
The Eocene Bioherms and the Associated Lithofacies in Western Herzegovina (Yugoslavia)
Autori
Dragičević, Ivan ; Blašković, Ivan ; Tišljar, Josip ; Papeš, Josip
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni
Izvornik
Proceedings - 8th IAS Regional Meeting of Sedimentology
/ -- - Tunis : International Association of Sedimentologists (IAS), 1987, 199-204
Skup
8th IAS Regional Meeting of Sedimentology, Tunis-87
Mjesto i datum
Tunis, 01.04.1987. - 03.04.1987
Vrsta sudjelovanja
Poster
Vrsta recenzije
Nije recenziran
Ključne riječi
Coaral-Bryozoan-Corallinacea Bioherm; Eocene; Western Herzegovina; Karst Dinarides
Sažetak
Eocene sedimentary rocks of complex litology and large thickness are widespread in western Herzegovina located in middle parts of the Dinaride carbonate platform. They are unconformably underlain by varous types of limestones of the Upper Cretaceous, mostly of the Cenomanian-Turonian. Coral-bryozoan-corallinacean biohermal limestones are represented by well preserved autochthonous reef, i. e. by typical bioherm consisting of pleanty of reef-forming organisms in the live position. The reef can be horizontally traced for kilometres, and its thickness is up to several ten of meters. Smaller reefs with less lateral stretching and thickness in the area of Sobač and Podsnježnica, and they can be unterpreted as patch reefs. At the base of reef body occur commonly hermatypic corals and bryozoans with larger amount of corallinaceans and in places with calcisponges. Generation of corals characterized by predominat vertical growth is covered by generation of bryozoans and corallinaceans with distinct horizontal component. They alternate in vertical direction. The most common reef-dwellers in the reef itself and particularly in its marginal parts are numerous large foraminifera (alveolines and nummulites) as well as numerous mullusks, mostly pelecypods and gastropods.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
POVEZANOST RADA
Ustanove:
Rudarsko-geološko-naftni fakultet, Zagreb