Pregled bibliografske jedinice broj: 39360
Lias carbonate platform deposits of Velebit Mt. (Croatia)
Lias carbonate platform deposits of Velebit Mt. (Croatia) // Harold Readings IAS Lecture Tour 99 - Croatia, Field-trip Guidebook Some carbonate and clastic successions of the External Dinarides - Velebit Mt., Island of Rab, / Reading, H. (ur.).
Zagreb: Institut za geol.istraž.Zagreb i Hrv. Geol.društvo, 1999. str. 9-22 (ostalo, domaća recenzija, cjeloviti rad (in extenso), znanstveni)
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Naslov
Lias carbonate platform deposits of Velebit Mt. (Croatia)
Autori
Vlahović, Igor ; Velić, Ivo ; Tišljar, Josip ; Matičec, Dubravko
Vrsta, podvrsta i kategorija rada
Radovi u zbornicima skupova, cjeloviti rad (in extenso), znanstveni
Izvornik
Harold Readings IAS Lecture Tour 99 - Croatia, Field-trip Guidebook Some carbonate and clastic successions of the External Dinarides - Velebit Mt., Island of Rab,
/ Reading, H. - Zagreb : Institut za geol.istraž.Zagreb i Hrv. Geol.društvo, 1999, 9-22
Skup
Harold Readings IAS Lecture Tour 99 (Croatia)
Mjesto i datum
Zagreb, Hrvatska, 29.09.1999. - 03.10.1999
Vrsta sudjelovanja
Ostalo
Vrsta recenzije
Domaća recenzija
Ključne riječi
Shallow-water carbonates; lithofacies; biofacies; carbonate platform; Lias; Mt. Velebit; Croatia
Sažetak
At the Kubus-pass there are the sedimentary continuity from the uppermost part of the Lower Lias to the Middle and Upper Lias with a total thickness of ca 270 m. Liassic carbonates are divided into 5 lithofacies units: A = Rhythmically alternating mudstone/wackestone and ooid grainstone interpreted as a typical peritidal deposits with migration of ooid sand from neighbouring shallows during stronger tidal currents and/or storm waves ; B = Lagoonal to shallow subtidal black mudstones with packestone/greinstone intercalations ; C = Rhytmically alternating mudrone/wackestone and grainstone/rudstones deposited in restricted shallow-water areas with periodical agitated water ; D = shalow subtidal lagoonal limestones with Lithiotid tempestite coquinas and E = Bioturbated "spotty limestones" deposited with a low sedimentation rate in a calm large shallows beneth the fair-weather wave base.
Izvorni jezik
Engleski
Znanstvena područja
Geologija