Investigation of modern geological processes in holocene lacustrine carbonates in the Danube-Tisza intefluve (Hungary)
In the middle part of Hungary, lacustrine carbonate mud was deposited along the Danube valley and on the morphologically slightly elevated drift sand ridge east of the Danube in the Holocene. Beside similarities, the carbonates of the two regions display significant differences, as indicated by grai...
Elmentve itt :
| Szerzők: | |
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| Dokumentumtípus: | Cikk |
| Megjelent: |
University of Szeged, Department of Mineralogy, Geochemistry and Petrology
Szeged
1995
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| Sorozat: | Acta mineralogica-petrographica
36 |
| Kulcsszavak: | Kőzettan, Ásványtan, Földtan |
| Tárgyszavak: | |
| Online Access: | http://acta.bibl.u-szeged.hu/24824 |
| Tartalmi kivonat: | In the middle part of Hungary, lacustrine carbonate mud was deposited along the Danube valley and on the morphologically slightly elevated drift sand ridge east of the Danube in the Holocene. Beside similarities, the carbonates of the two regions display significant differences, as indicated by grain size distribution, mineralogical and gheocemical analyses. The authors propose that these differences are due to different palaeoenvironmental conditions, and to effects of subsequent soil formation. Investigation of the carbonate section reveals modern geological processes in detail. |
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| Terjedelem/Fizikai jellemzők: | 73-87 |
| ISSN: | 0365-8066 |