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One example of such a tectonostratigraphy is the Scandinavian Caledonides. [1] Within the entire exposed 1800 km length of this orogenic belt the following sequence is recognised from the base upwards: Autochthon; undisturbed foreland of the Baltic plate. Parautochthon
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Geology portal; This article is within the scope of WikiProject Geology, an attempt at creating a standardized, informative, comprehensive and easy-to-use geology resource. . If you would like to participate, you can choose to edit this article, or visit the project page for more informati
The Svecofennian orogeny developed as a succession of four orogenies which by chronological order are: the Lapland-Savo orogeny, the Fennian orogeny, the Svecobaltic orogeny and the Nordic orogeny. [6]
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