Pregled bibliografske jedinice broj: 402894
Cyclicity of Barremian Tidal Flat Deposits of Southern Adriatic Platform, Croatia
Cyclicity of Barremian Tidal Flat Deposits of Southern Adriatic Platform, Croatia // GSA Annual Convention, Abstracts with Program
Houston (TX), 2008. (poster, međunarodna recenzija, sažetak, znanstveni)
CROSBI ID: 402894 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Cyclicity of Barremian Tidal Flat Deposits of Southern Adriatic Platform, Croatia
Autori
Sweeney, Rafferty, J. ; Harman, Charles ; Husinec, Antun ; Read, J. Fred
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni
Izvornik
GSA Annual Convention, Abstracts with Program
/ - Houston (TX), 2008
Skup
2008 Joint Meeting of The Geological Society of America, Soil Science Society of America, American Society of Agronomy, Crop Science Society of America, Gulf Coast Association of Geological Societies with the Gulf Coast Section of SEPM
Mjesto i datum
Houston (TX), Sjedinjene Američke Države, 05.10.2008. - 09.10.2008
Vrsta sudjelovanja
Poster
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
Barremian; cycles; tidal flat; facies; Adriatic Platform
Sažetak
The Adriatic Platform provides a window into carbonate deposition spanning the Jurassic-Cretaceous transition in the western Tethys. The sediments exposed on the islands of southern Croatia are highly cyclic. The Barremian section is characterized by extensive microbial laminite facies that is by far the best preserved tidal flat facies compared to any Lower Cretaceous interval of the Adriatic platform. Three logged sections, each between 150 and 200 m thick, display superbly developed peritidal parasequences. The parasequences are composed of shallow subtidal (lime mudstone and peloid-intraclast-skeletal packstone-grainstone) to intertidal (microbial laminites and fenestral lime mudstone) and subaerial exposure facies (greenish clay sheets or breccia with greenish clay or mud matrix). The majority of the cycles may have been formed by high-frequency changes in sea level perhaps related to orbital forcing ; possible durations of the interval and its component parasequences are being evaluated to see if these are compatible with a precessional vs longer term obliquity or eccentricity signals. Some parasequences probably also formed by autocyclic processes and local tectonics. Presence of platform-wide subaerial exposure surfaces capping some cycles suggest a relative sea level falls affected the platform over wide areas.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
POVEZANOST RADA
Projekti:
181-1811096-1093 - Osnovna geološka karta Republike Hrvatske 1:50.000 (Belak, Mirko, MZOS ) ( CroRIS)
181-1953068-0241 - Odraz paleoklimatskih promjena u jursko-krednim sedimentima Krških Dinarida (Hajek-Tadesse, Valentina, MZOS ) ( CroRIS)
Ustanove:
Hrvatski geološki institut
Profili:
Antun Husinec
(autor)