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Eesti Stratigraafia Komisjon (ESK)
Estonian Commission on Stratigraphy
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[EST] [ENG]
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ESK » Kannuka kihistikingl. k. Kannuka Member
Stratotüübidholostratotüüp: Meriküla F-169 puurauk (90.00..100.50 m) | Mens, 1992 (comp) | KirjeldusFrom Mens, K., & Pirrus, E. (1997): The Kannuka Member consists entirely of light weakly cemented fine- to medium-grained quartzose sandstones with a few thin interlayers of multicoloured clayey siltstones, which are similar to the underlying deposits of the Sirgala Member. The clay fraction is dominated by kaolinite. Increase in the maturity in minerals upward the section is indicative of the redeposition of older sediments. ViitedMeidla, T. 2017. Ediacaran and Cambrian stratigraphy in Estonia: an updated review. Estonian Journal of Earth Sciences 66(3), p. 152–160. https://doi.org/10.3176/earth.2017.12 PDF Mens, K., Pirrus, E. 1997. Vendian. Geology and mineral resources of Estonia. Estonian Academy Publishers, Tallinn. p. 35-38. Mens, K. (comp.) 1992. Каталог стратотипов венда и кембрия Прибалтики [Catalogue of Vendian and Cambrian stratotypes of the East Baltic areas]. p. 1-25. PDF Mens, K., Pirrus, E. 1980. К стратиграфической номенклатуре вендских отложений Эстонии [On stratigraphical nomenclature of Vendian beds of Estonia]. Eesti NSV Teaduste Akadeemia Toimetised. Geoloogia / Известия Академии наук Эстонской ССР. Геология 29(2), p. 49-54. https://doi.org/10.3176/geol.1980.2.01 PDF |
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Eesti Stratigraafia Komisjon 2006-2026. Siin lehel leiduvad materjalid on kõigile vabaks kasutamiseks vastavalt Creative Commons CC-BY litsentsile |
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