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Pregled bibliografske jedinice broj: 160228

Clay Minerals Within The Carbonate Sequences In Tinjan Area (Istria, Croatia)


Barudžija, Uroš; Tadej, Neven; Aljinović, Dunja; Vrkljan, Maja
Clay Minerals Within The Carbonate Sequences In Tinjan Area (Istria, Croatia) // Acta Mineralogica-Petrographica, Abstract Series / Nemeth, Tibor ; Terbocs, Attila (ur.).
Szeged (Madjarska): Department of Mineralogy, Geochemistry and Petrology, University of Szeged, 2004. (poster, nije recenziran, sažetak, znanstveni)


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Naslov
Clay Minerals Within The Carbonate Sequences In Tinjan Area (Istria, Croatia)

Autori
Barudžija, Uroš ; Tadej, Neven ; Aljinović, Dunja ; Vrkljan, Maja

Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni

Izvornik
Acta Mineralogica-Petrographica, Abstract Series / Nemeth, Tibor ; Terbocs, Attila - Szeged (Madjarska) : Department of Mineralogy, Geochemistry and Petrology, University of Szeged, 2004

Skup
2nd Mid-European Clay Conference,

Mjesto i datum
Miškolc, Madjarska, 20-24.09.2004

Vrsta sudjelovanja
Poster

Vrsta recenzije
Nije recenziran

Ključne riječi
clay minerals; carbonate sequence; Adriatic Carbonate Platform; Albian; Istria; Croatia

Sažetak
Clayey limestones in the Upper Albian shallow-marine carbonate sequences from Tinjan area in Istria (Croatia) were investigated. Two layers of clayey limestone (70-90 wt.% of calcite) overlay the sequences containing carbonate breccias, interlaminated pelsparites/ostracodal micrites and cyanobacterial limestones as well as "quartz diagenetic sediments" (BARUDŽIJA, 2003). Insoluble residues of clayey limestones predominantly contain illite and/or mixed-layer illite/smectite dominated by illite layers, illite/smectite with higher amount of smectite layers than previous and randomly interstratified minerals. Some of other phyllosilicates, probably smectites, are also present. Insoluble residues also contain quartz (10-20wt. %), feldspars (up to 5wt. %) and amorphous material. Since the appearance of the layers with clayey limestones in Upper Albian sequences in Istria is closely connected with the appearance of "quartz diagenetic sediments" (DURN et al., 2003), this mineral assemblage can be indicative of the origin of their parent material.

Izvorni jezik
Engleski

Znanstvena područja
Geologija



POVEZANOST RADA


Projekti:
0195024
0195034

Ustanove:
Rudarsko-geološko-naftni fakultet, Zagreb

Profili:

Avatar Url Uroš Barudžija (autor)

Avatar Url Dunja Aljinović (autor)

Avatar Url Neven Tadej (autor)

Avatar Url Maja Vrkljan (autor)


Citiraj ovu publikaciju

Barudžija, Uroš; Tadej, Neven; Aljinović, Dunja; Vrkljan, Maja
Clay Minerals Within The Carbonate Sequences In Tinjan Area (Istria, Croatia) // Acta Mineralogica-Petrographica, Abstract Series / Nemeth, Tibor ; Terbocs, Attila (ur.).
Szeged (Madjarska): Department of Mineralogy, Geochemistry and Petrology, University of Szeged, 2004. (poster, nije recenziran, sažetak, znanstveni)
Barudžija, U., Tadej, N., Aljinović, D. & Vrkljan, M. (2004) Clay Minerals Within The Carbonate Sequences In Tinjan Area (Istria, Croatia). U: Nemeth, T. & Terbocs, A. (ur.)Acta Mineralogica-Petrographica, Abstract Series.
@article{article, year = {2004}, pages = {12}, keywords = {clay minerals, carbonate sequence, Adriatic Carbonate Platform, Albian, Istria, Croatia}, title = {Clay Minerals Within The Carbonate Sequences In Tinjan Area (Istria, Croatia)}, keyword = {clay minerals, carbonate sequence, Adriatic Carbonate Platform, Albian, Istria, Croatia}, publisher = {Department of Mineralogy, Geochemistry and Petrology, University of Szeged}, publisherplace = {Mi\v{s}kolc, Madjarska} }
@article{article, year = {2004}, pages = {12}, keywords = {clay minerals, carbonate sequence, Adriatic Carbonate Platform, Albian, Istria, Croatia}, title = {Clay Minerals Within The Carbonate Sequences In Tinjan Area (Istria, Croatia)}, keyword = {clay minerals, carbonate sequence, Adriatic Carbonate Platform, Albian, Istria, Croatia}, publisher = {Department of Mineralogy, Geochemistry and Petrology, University of Szeged}, publisherplace = {Mi\v{s}kolc, Madjarska} }




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