Pregled bibliografske jedinice broj: 264938
Altered tephra layers in the Upper Jurassic Lemeš deposits near Maovice (Dalmatia, Croatia): Clay mineralogy and basic soil mechanic properties
Altered tephra layers in the Upper Jurassic Lemeš deposits near Maovice (Dalmatia, Croatia): Clay mineralogy and basic soil mechanic properties // 3rd Mid-European Clay Conference (MECC 06) : Abstracts Book / Vlahović, Igor, Tibljaš, Darko, Durn, Goran, Biševac, Vanja (ur.) (ur.).
Zagreb: Faculty of Science ; Faculty of Mining, Geology and Petroleum Engineering, 2006. str. 104-104 (predavanje, domaća recenzija, sažetak, znanstveni)
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Naslov
Altered tephra layers in the Upper Jurassic Lemeš deposits near Maovice (Dalmatia, Croatia): Clay mineralogy and basic soil mechanic properties
Autori
Šegvić, Branimir ; Toševski, Aleksandar ; Števanić, Danijela ; Biševac, Vanja ; Lugović, Boško
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni
Izvornik
3rd Mid-European Clay Conference (MECC 06) : Abstracts Book
/ Vlahović, Igor, Tibljaš, Darko, Durn, Goran, Biševac, Vanja (ur.) - Zagreb : Faculty of Science ; Faculty of Mining, Geology and Petroleum Engineering, 2006, 104-104
ISBN
953-6076-09-8
Skup
Mid-European Clay Conference (3 ; 2006)
Mjesto i datum
Opatija, Hrvatska, 18.09.2006. - 20.09.2006
Vrsta sudjelovanja
Predavanje
Vrsta recenzije
Domaća recenzija
Ključne riječi
clay mineralogy; soil mechanics properties; crystalloclasts; origin; Maovice (Dalmatia; Croatia)
Sažetak
Two bentonite layers in the vicinity of Maovice village in the Dalmatian hinterland intercalate within typical Lemeš deposits. These layers were subjected to mineralogical and geochemical research in order to reveal its mineralogical properties and possible origin of clay material. Standards soil mechanics tests were performed as well. Preliminary results from two localities (Bunarić and Gornji Ždanj) are displayed in Abstract (PDF file, attached) and herein briefly reported. The XRD analysis of global samples reveals montmorillonite as the principal mineral in both samples accompanied by calcite, cristobalite, plagioclase (albite ?), quartz and biotite in the Bunarić sample and calcite, quartz, clinoptilolite and cristobalite in Gornji Ždanj sample. In the grain size fraction 63-125 μ m, the sample from Bunarić locality contains comparatively high amount of volcanic crystalloclasts (biotite, sanidine, quartz, augite etc.). Volcanoclastic mineral composition and mineral chemistry of analyzed tephra layers strongly suggest a high-K calc-alkaline (rhyolitic?) volcanic arc as the source of tephra. Grain size composition and content of calcite classify Bunarić sample as clayey silt and Gornji Ždanj sample as calcareous silty clay (KONTA, 1969 classification scheme). Performed soil mechanic tests data clearly imply high compressibility, high swell aptitude and wide range of plastic state of analyzed bentonites.
Izvorni jezik
Engleski
Znanstvena područja
Geologija, Građevinarstvo, Rudarstvo, nafta i geološko inženjerstvo
POVEZANOST RADA
Ustanove:
Fakultet građevinarstva, arhitekture i geodezije, Split,
Prirodoslovno-matematički fakultet, Zagreb,
Rudarsko-geološko-naftni fakultet, Zagreb
Profili:
Branimir Šegvić
(autor)
Boško Lugović
(autor)
Aleksandar Toševski
(autor)
Danijela Števanić
(autor)
Vanja Biševac
(autor)