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

Institutional repository: Faculty of Mining, Geology and Petroleum Engineering Repository, University of Zagreb

Cite this document

Kruk, B., Mileusnić, M., Bakrač, K., Tibljaš, D., Kastmüller, Ž., Ilijanić, N. & Kruk, Lj. (2008). Clay mineralogy, geochemistry and pollen of the Ričice clay deposit, Croatia, a paleo-environmental reconstruction. In K. Górniak, (Ed.), Abstracts / 4th Mid-European Clay Conference 2008 (p. 96). Kraków: Mineralogical Society of Poland. Retrieved from 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, edited by Katarzyna Górniak, Mineralogical Society of Poland, 2008, p. 96. https://urn.nsk.hr/urn:nbn:hr:169:377240

Kruk, Boris, Marta Mileusnić, Koraljka Bakrač, Darko Tibljaš, Željko Kastmüller, Nikolina Ilijanić and Ljiljana Kruk. "Clay mineralogy, geochemistry and pollen of the Ričice clay deposit, Croatia, a paleo-environmental reconstruction." In Abstracts / 4th Mid-European Clay Conference 2008, 96. Kraków: Mineralogical Society of Poland, 2008. Accessed 2024 November 22. 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', in Górniak, K. (ed.), Abstracts / 4th Mid-European Clay Conference 2008, Mineralogical Society of Poland, Kraków, p. 96. Available at: https://urn.nsk.hr/urn:nbn:hr:169:377240 (Accessed 22 November 2024)

Kruk B, Mileusnić M, Bakrač K, Tibljaš D, Kastmüller Ž, Ilijanić N, and sur.. Clay mineralogy, geochemistry and pollen of the Ričice clay deposit, Croatia, a paleo-environmental reconstruction. In: K. Górniak, ed. Abstracts / 4th Mid-European Clay Conference 2008. Kraków: Mineralogical Society of Poland; 2008. Pp. 96-96. [cited 2024 November 22] Available at: 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, Ed. Kraków: Mineralogical Society of Poland, 2008. [Online] Available at: https://urn.nsk.hr/urn:nbn:hr:169:377240 [Accessed: 22 November 2024]

Metadata
Title (english)Clay mineralogy, geochemistry and pollen of the Ričice clay deposit, Croatia, a paleo-environmental reconstruction
AuthorBoris Kruk
AuthorMarta Mileusnić https://orcid.org/0000-0003-3776-3661
AuthorKoraljka Bakrač
AuthorDarko Tibljaš
AuthorŽeljko Kastmüller
AuthorNikolina Ilijanić
AuthorLjiljana Kruk
EditorKatarzyna Górniak
Author's institutionCroatian Geological Survey
Author's institutionUniversity of Zagreb
Faculty of Mining, Geology and Petroleum Engineering
(Department of Mineralogy, Petrology and Mineral Resources)
Author's institutionUniversity of Zagreb
Faculty of Science
(Department of Geology)
Scientific / art field,
discipline and subdiscipline		NATURAL SCIENCES
Geology
Abstract (english)
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.
Languageenglish
Publication typeScientific paper - Abstract
Publication statusPublished
Peer reviewPeer review - international
Publication versionPublished version
Publication titleAbstracts / 4th Mid-European Clay Conference 2008
Series titleMineralogia. Special papers
Numberingvol. 33, p. 96
p-ISSN1896-2203
URN:NBNurn:nbn:hr:169:377240
Publication2008
ConferenceTitle: 4th Mid-European Clay Conference 2008
Acronym: MECC'08
Location: Zakopane, Poland
Organizer: Mineralogical Society of Poland - Polish Clay Group
Organizer: Faculty of Geology, Geophysics and Environmental Protection, AGH University of Science and Technology
Organizer: Stanisław Staszic Scientific Association
Start date: 2008-09-22
End date: 2008-09-27
Assembly type: Lecture
Document URLhttp://www.ptmin.agh.edu.pl/mpsp30/mpsp33.pdf
Type of resourceText
PublisherMineralogical Society of Poland
Publishing placeKraków
Access conditionsOpen access
Terms of useLicence Attribution-NonCommercial-NoDerivatives 4.0 International (CC BY-NC-ND 4.0) icon
Created on2020-08-24 08:33:49