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 |
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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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