CLM includes long-form articles, events listings, publication reviews, new product information and updates, reports of conferences and letters. Exceptional customer service Get specialist help and advice. Focusing on the Precambrian in the central part of the Fennoscandian Shield, the book combines the results from modern geological and geophysical research into a detailed petrologic, lithologic, and structural synthesis and interpretation of the Archean and Proterozoic of Finland. It will be of value to anyone interested in the evolution of the shield in particular and in Precambrian geology in general.
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Images Additional images. About this book Focusing on the Precambrian in the central part of the Fennoscandian Shield, the book combines the results from modern geological and geophysical research into a detailed petrologic, lithologic, and structural synthesis and interpretation of the Archean and Proterozoic of Finland.
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A Field Guide to the Geology of Madeira. The Precambrian crust of the Baltic Shield developed during four orogenies between 3. A collisional orogeny is recorded in the north of the shield by a narrow belt of early Proterozoic crust separating two Archaean crustal segments. In the central Baltic Shield, westward growth of continental crust occurred during the Svecokarelian 2.
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Intracratonic rifting simultaneously disrupted the Archaean parts of the shield. The results of recent work suggest that plate tectonic models can also be applied to the late Archaean.
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Please review our Terms and Conditions of Use and check box below to share full-text version of article. Summary The Precambrian crust of the Baltic Shield developed during four orogenies between 3. Citing Literature. Proterozic Lithospheric Evolution, Volume
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