On the role of secondary dolomitization of limestones in karst formation
Abstract
The formation of voids in rocks during the development of karst is usually explained by the dissolving action of water and mechanical destruction of rocks with the removal of particles by groundwater. The study of deep karst at the Leningrad oil shale deposit shows that the formation of voids in carbonate rocks can also go at metasomatic processes - as a result of secondary dolomitization of limestone.
Область исследования:
(Archived) Without section
Funding:
None
References
- Gazizov M. S. Investigation of the regularity of development and manifestation of deep karst in the Baltic shale basin. PH A. A. Skochinsky IHD, M., 1964.
- Gatalsky M. A. Karst of Silurian and Ordovician carbonate rocks of the Baltic. STA VNIGRI, Geology and Geochemistry, vol. 1, 1957.
- Levykin V. V. Karst and false karst phenomena at the Leningrad oil shale deposit. Coll.: Special questions of Karstology (hydrogeology, hydrology and minerals). PH AS USSR, 1962.
- Mayorov N. F. Gas-volume method of analysis of carbonate rocks. Journal of Mining Institute, vol. XLIII, iss. 2, 1962.
- Perelman A. I. Geochemistry of Epigenetic Processes. Nedra, 1965.
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