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...

Full description

Bibliographic Details
Main Authors: Gee, David G., Ladenberger, Anna, Dahlqvist, Peter, Jarosław Majka, Be'eri-Shlevin, Yaron, Frei, Dirk, Thomsen, Tonny
Format: Dataset
Language:unknown
Published: Geological Society of London 2016
Subjects:
Online Access:https://dx.doi.org/10.6084/m9.figshare.3453581.v1
https://geolsoc.figshare.com/articles/dataset/The_Baltoscandian_margin_detrital_zircon_signatures_of_the_central_Scandes/3453581/1