Diagenetic and lithification processes of Recent hypersaline dolomites on the Duna-Tisza interfluve

Molnár Béla and Szónoky Miklós and Kovács Sándor: Diagenetic and lithification processes of Recent hypersaline dolomites on the Duna-Tisza interfluve. In: Acta mineralogica-petrographica, (24) 2. pp. 315-337. (1980)

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Abstract

In the hypersaline lacustrine dolomite and dolomite mud profiles of the Danube-Tisza-Interfluve four members can be distinguished on the basis of formation, composition, diagenesis and lithification. In the three lower members, i. e. in the dolomitic limestone and dolomite the starting phase of anadiagenesis, in the upper dolomite mud the syndiagenesis take place. The latter lithification is one of the most important factor of syndiagenesis. The formation, evolution, filling processes of pores, the chemical composition of the filling material as well as their crsytal forms depend on these processes and change according to their affects.

Item Type: Article
Journal or Publication Title: Acta mineralogica-petrographica
Date: 1980
Volume: 24
Number: 2
ISSN: 0365-8066
Page Range: pp. 315-337
Language: English
Publisher: University of Szeged, Department of Mineralogy, Geochemistry and Petrology
Place of Publication: Szeged
Related URLs: http://acta.bibl.u-szeged.hu/39399/
Uncontrolled Keywords: Kőzettan, Ásványtan, Földtan
Additional Information: Bibliogr.: p. 329-331. ; ill. ; összefoglalás angol nyelven
Subjects: 01. Natural sciences
01. Natural sciences > 01.05. Earth and related environmental sciences
Date Deposited: 2016. Oct. 17. 09:25
Last Modified: 2022. Jul. 25. 14:18
URI: http://acta.bibl.u-szeged.hu/id/eprint/24663

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