SVIBOR - Papers quoted in CC - project code: 1-09-084

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SVIBOR - Collecting Data on Projects in Croatia

Papers quoted in Current Contents on project 1-09-084

Quoted papers: 4
Other papers: 70
Total: 74

Title: Sekvencijalno stratigrafski razvoj i biostratigrafija miocensko-?pliocenskih klastita (Promina-slojevi) u sjevernoj Dalmaciji, Hrvatska.

Authors:: Marjanac, Tihomir (108851); Marjanac, Ljerka (138720); Ćosović, Vlasta (99886); Babac, Darinka

Journal: Palaeogeography, Palaeoclimatology, Palaeoecology
Number: ??
ISSN: 0031-0182
Volume: ??
Year: 1996
Pages: from ??? to ???
Number of references: 52
Language: engleski
Summary: The age of 'Eocene' clastics near the Ljubač village in Ravni Kotari is dated as the Late Tortonian - Early Pliocene after small benthic foraminifers. This sediments are lithologically identical to Promina-beds, and composed of 6 depositional sequences bounded by erosional unconformities. One complete sequence comprises conglomerate in the lower part, hybrid arenites in the middle- and marine silty marls in the upper part. The basal unconformities are recognized as sequence boundaries and interpreted as the incised valleys created in response to major falls in sea-level, hence the conglomerates were deposited during sea-level lowstands and early transgressions. Marls were deposited during marine incursions and probably correspond to the highstand sequence tracts. Coarse debris composed of Cretaceous and Eocene sediments testifies on uplift and unroofing of Dinarides, probably during Oligocene.
Keywords: Eocene, Miocene, Pliocene, Foraminifers, Paleoclimate, Ravni Kotari, Conglomerates, Promina-beds, Sea-level change, Stratigraphy

Title: Taloženje megaslojeva (megaturbidita) i promjene razine mora u proksimalnom dijelu eocensko-miocenskog fliša srednje Dalmacije (Hrvatska).

Authors:: Marjanac, Tihomir (108851)

Journal: Geology
Number: ??
ISSN: 0091-4613
Volume: ??
Year: 1996
Pages: from ??? to ???
Number of references: 33
Language: engleski
Summary: Some megabeds of the Dalmatian Eocene-Miocene flysch are underlain and overlain by conglomeratic fan-deltas which interfinger with thinner turbidites. Deposition of fan-deltas and thinner turbidites is attributed to lowstands and early sea-level rises. Deposition of megabeds is attributed to accelerated sea-level rise which aborted the growth of fan deltas, because: 1) they overlie conglomeratic fan deltas, 2) skeletal and lithical debris in megabeds originated by weathering of older sediments, 3) their large thickness indicates a high primary accumulation of debris and low frequency of flows. Sea-level changes inferred from megabeds are different from that of thinner turbidites, and distinction of the two is important for sequence stratigraphy of basnal sediments.
Keywords: Dalmatia, Megabeds, Sea-level changes, Fan-deltas, Flysch

Title: Paleoekološko značenje morfologije ortofragminida sa Istarskog poluotoka (Hrvatska i Slovenija).

Authors:: Ćosović, Vlasta (99886); Drobne, Katica

Journal: Geobios
Number: 1
ISSN: 0013-6995
Volume: 18
Year: 1995
Pages: from ??? to ???
Number of references: 25
Language: engleski
Summary: Orthophragminids collected on several sections in Istria, ranging in age from the Upper Cuisian to the Early-Middle Lutetian, were studied. Morphostructural characteristics of foraminiferal tests and content of glaucony grains in sediments allowed the differentiation of three fossil associations with paleoenvironmental significance.
Keywords: Orthophragminids, Eocene, Istrian Peninsula, Paleoenvironment, Glaucony

Title: Sekvencijalna stratigrafija Dunlin grupe u sjevernom Sjevernom Moru: taložni model ya Cook pješčenjake.

Authors:: Marjanac, Tihomir (108851); Steel, Ronald

Journal: The American Association of Petroleum Geologists Bulletin
Number: ?
ISSN: 0149-1423
Volume: ?
Year: 1996
Pages: from ??? to ???
Number of references: 31
Language: engleski
Summary: Description of the Dunlin Group sandstones, interpretation of their genesis and reconstruction of the geometries of the sedimenatry bodies. Sandstones are interpreted as incised valley fills, whose morphology controlls the distribution and thickness of thesandstone collectors.
Keywords: Jurassic, North Sea, Oil collectors, Sequence stratigraphy, Sandstones, Incised valley fills


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