prikaz prve stranice dokumenta Clay mineralogy, geochemistry and pollen of the Ričice clay deposit, Croatia, a paleo-environmental reconstruction
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Clay mineralogy, geochemistry and pollen of the Ričice clay deposit, Croatia, a paleo-environmental reconstruction
U: Abstracts / 4th Mid-European Clay Conference 2008. / Górniak, Katarzyna (ur.). Kraków: Mineralogical Society of Poland, 2008. str. 96. urn:nbn:hr:169:377240
Kruk, Boris; Mileusnić, Marta; Bakrač, Koraljka; Tibljaš, Darko; Kastmüller, Željko; Ilijanić, Nikolina; Kruk, Ljiljana

Institucijski repozitorij: Repozitorij Rudarsko-geološko-naftnog fakulteta Sveučilišta u Zagrebu

Citirajte ovaj rad

Kruk, B., Mileusnić, M., Bakrač, K., Tibljaš, D., Kastmüller, Ž., Ilijanić, N. i Kruk, Lj. (2008). Clay mineralogy, geochemistry and pollen of the Ričice clay deposit, Croatia, a paleo-environmental reconstruction. U K. Górniak, (Ur.), Abstracts / 4th Mid-European Clay Conference 2008 (str. 96). Kraków: Mineralogical Society of Poland. Preuzeto s https://urn.nsk.hr/urn:nbn:hr:169:377240

Kruk, Boris, et al. "Clay mineralogy, geochemistry and pollen of the Ričice clay deposit, Croatia, a paleo-environmental reconstruction." Abstracts / 4th Mid-European Clay Conference 2008, Ur. Katarzyna Górniak, Mineralogical Society of Poland, 2008, str. 96. https://urn.nsk.hr/urn:nbn:hr:169:377240

Kruk, Boris, Marta Mileusnić, Koraljka Bakrač, Darko Tibljaš, Željko Kastmüller, Nikolina Ilijanić i Ljiljana Kruk. "Clay mineralogy, geochemistry and pollen of the Ričice clay deposit, Croatia, a paleo-environmental reconstruction." U Abstracts / 4th Mid-European Clay Conference 2008, 96. Kraków: Mineralogical Society of Poland, 2008. Citirano 29.12.2024.. https://urn.nsk.hr/urn:nbn:hr:169:377240

Kruk, B., et al. (2008) 'Clay mineralogy, geochemistry and pollen of the Ričice clay deposit, Croatia, a paleo-environmental reconstruction', u Górniak, K. (ur.), Abstracts / 4th Mid-European Clay Conference 2008, Mineralogical Society of Poland, Kraków, str. 96. Preuzeto s: https://urn.nsk.hr/urn:nbn:hr:169:377240 (Datum pristupa: 29.12.2024.)

Kruk B, Mileusnić M, Bakrač K, Tibljaš D, Kastmüller Ž, Ilijanić N, i sur.. Clay mineralogy, geochemistry and pollen of the Ričice clay deposit, Croatia, a paleo-environmental reconstruction. U: K. Górniak, ur. Abstracts / 4th Mid-European Clay Conference 2008. Kraków: Mineralogical Society of Poland; 2008. Str. 96-96. [pristupljeno 29.12.2024.] Dostupno na: https://urn.nsk.hr/urn:nbn:hr:169:377240

B. Kruk, et al., "Clay mineralogy, geochemistry and pollen of the Ričice clay deposit, Croatia, a paleo-environmental reconstruction", Abstracts / 4th Mid-European Clay Conference 2008, K. Górniak, Ur. Kraków: Mineralogical Society of Poland, 2008. [Online] Dostupno na: https://urn.nsk.hr/urn:nbn:hr:169:377240 [Citirano: 29.12.2024.]

Za citiranje koristite ovu mrežnu adresu: https://urn.nsk.hr/urn:nbn:hr:169:377240
Podaci o radu
Naslov (engleski)Clay mineralogy, geochemistry and pollen of the Ričice clay deposit, Croatia, a paleo-environmental reconstruction
AutorBoris Kruk
AutorMarta Mileusnić https://orcid.org/0000-0003-3776-3661
AutorKoraljka Bakrač
AutorDarko Tibljaš
AutorŽeljko Kastmüller
AutorNikolina Ilijanić
AutorLjiljana Kruk
UrednikKatarzyna Górniak
Autorova ustanovaHrvatski geološki institut
Autorova ustanovaSveučilište u Zagrebu
Rudarsko-geološko-naftni fakultet
(Zavod za mineralogiju, petrologiju i mineralne sirovine)
Autorova ustanovaSveučilište u Zagrebu
Prirodoslovno-matematički fakultet
(Geološki odsjek)
Znanstveno / umjetničko
područje, polje i grana		PRIRODNE ZNANOSTI
Geologija
Sažetak (engleski)
The Ričice deposit, as well as the whole of the Crna Mlaka Basin, is mostly composed of Quaternary clay beds, intercalated with layers and lenses of sands and fine-grained conglomerates, developed in the Pliocene-Pleistocene period. The Rečica clay deposit is represented by a seried of sub-parallel and gently inclined, almost horizontal, layers of silty clay, which are laterally continuous. The major part of the clays is represented by the alternation of brown and grey, sometimes yellow clays that are underlain by greenish-grey and grey-blue clays. The clay deposits are 8-12 m thick. Clays from the Rečica deposit can be classified as a montmorillonite-illite variety, in accordance with their genetic type. The main mineral constituents are quartz, 10 Å phyllosilicate (illite and/or mica) and smectite group minerals, while goethite, kaolinite, chlorite, feldspars and dolomite are subordinate to accessory minerals. The Rečica deposit can be classified as a montmorillonite-illite variety, in accordance with their genetic type. The main mineral constituents are quartz, 10 Å phyllosilicate (illite and/or mica) and smectite group minerals, while goethite, kaolinite, chlorite, feldspars and dolomite are subordinate to accessory minerals. The clay deposit is of an allochthonous fluviatile-swamp type. The sediments with clay were deposited during the Holocene under fluviatile conditions, as well as in areas in which ponds, swamps and small lakes prevailed.
Jezikengleski
Vrsta publikacijeZnanstveni rad - Sažetak
Status objaveObjavljen
Vrsta recenzijeRecenziran - međunarodna recenzija
Verzija publikacijeObjavljena verzija rada (izdavačev PDF)
Naslov zbornikaAbstracts / 4th Mid-European Clay Conference 2008
Naslov serijeMineralogia. Special papers
Brojčani podacivol. 33, str. 96
p-ISSN1896-2203
URN:NBNurn:nbn:hr:169:377240
Datum objave publikacije2008
SkupNaziv: 4th Mid-European Clay Conference 2008
Kratica: MECC'08
Lokacija: Zakopane, Poljska
Organizator: Mineralogical Society of Poland - Polish Clay Group
Organizator: Faculty of Geology, Geophysics and Environmental Protection, AGH University of Science and Technology
Organizator: Stanisław Staszic Scientific Association
Datum početka: 2008-09-22
Datum završetka: 2008-09-27
Vrsta izlaganja: Predavanje
URL dokumentahttp://www.ptmin.agh.edu.pl/mpsp30/mpsp33.pdf
Vrsta resursaTekst
IzdavačMineralogical Society of Poland
Mjesto izdavanjaKraków
Prava pristupaOtvoreni pristup
Uvjeti korištenjaIkona licence Imenovanje-Nekomercijalno-Bez prerada 4.0 međunarodna (CC BY-NC-ND 4.0)
Datum i vrijeme pohrane2020-08-24 08:33:49