The Baltoscandian margin detrital zircon signatures of the central Scandes
In central parts of the Scandinavian Caledonides, detrital zircon signatures provide evidence of the change in character of the Baltoscandian crystalline basement, from the characteristic Late Palaeoproterozoic granites of the Transscandinavian Igneous Belt (TIB, c. 1650–1850 Ma) in the foreland Aut...
Main Authors: | , , , , , , |
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Format: | Dataset |
Language: | unknown |
Published: |
Geological Society of London
2016
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Subjects: | |
Online Access: | https://dx.doi.org/10.6084/m9.figshare.3453581 https://geolsoc.figshare.com/articles/dataset/The_Baltoscandian_margin_detrital_zircon_signatures_of_the_central_Scandes/3453581 |