|
Eesti Stratigraafia Komisjon (ESK)
Estonian Commission on Stratigraphy
|
|||||||||||||||||||||||||
|
|
|||||||||||||||||||||||||
[EST] [ENG]
|
ESK » Meriküla kihistikingl. k. Meriküla Member
Stratotüübidholostratotüüp: Meriküla F-169 puurauk (114.50..143.60 m) | Mens, 1992 (comp) | KirjeldusFrom Mens, K., & Pirrus, E. (1997). Vendian. In Geology and mineral resources of Estonia (pp. 35–38). Estonian Academy Publishers: The Meriküla Member is the most typical unit of the Kotlin Formation. It is represented by the “Laminarites” Clay consisting of rhytmically alternating 0.5–0.8 mm thick pairs of dark-grey fine-dispersed clay layers and light-grey laminae higher in silt. The bedding plane is covered by dark-brown shapeless organic films. Vendotaenides, small flakes of mica and siderite nodules are common. The fairly uniform mineral composition shows that the source areas must have been located relatively far from the depositional basin. 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., 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 Stumbur, K., Jõgi, S., Mardla, A., Mardla, E., Stumbur, H., Erisalu, E. 1963. Отчет о поисково-сьемочных работах в прибрежной северо-восточной части Эстонии за 1959-1961 гг. [Aruanne otsingu-kaardistamistöödest Kirde-Eesti kaldaäärses osas 1959.-1961. a]. EGV aruanne. Geoloogiafond, . p. . |
||||||||||||||||||||||||
|
Eesti Stratigraafia Komisjon 2006-2026. Siin lehel leiduvad materjalid on kõigile vabaks kasutamiseks vastavalt Creative Commons CC-BY litsentsile |
|||||||||||||||||||||||||