The Baltoscandian margin detrital zircon signatures of the central Scandes

David G. Gee, Anna Ladenberger, Peter Dahlqvist, Jarosław Majka, Yaron Be'Eri-Shlevin, Dirk Frei, Tonny Thomsen

Research output: Chapter in Book/Report/Conference proceedingChapter in bookResearchpeer-review

67 Citations (Scopus)


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 Autochthon to the typical, mainly Mesoproterozoic-age profile (c. 950-1700 Ma) of the Sveconorwegian Orogen of southwestern Scandinavia in the hinterland. Late Ediacaran to Early Cambrian shallow-marine Vemdal quartzites of the Jämtlandian Nappes (Lower Allochthon) provide strong bimodal signatures with TIB (1700-1800 Ma) and Sveconorwegian, sensu stricto (900-1150 Ma) ages dominant. Mid-Ordovician turbidites (Norråker Formation) of the Lower Allochthon in Sweden, sourced from the west, have unimodal signatures dominated by Sveconorwegian ages with peaks at 1000-1100 Ma, but with subordinate components of older Mesoproterozoic zircons (1200-1650 Ma). Latest Ordovician shallow-marine quartzites also yield bimodal signatures, but are more dispersed than in the Vemdal quartzites. In the greenschist facies lower parts of the Middle Allochthon, the Fuda (Offerdal Nappe) and Särv Nappe signatures are either unimodal or bimodal (950-1100 and/or 1700-1850 Ma), with variable dominance of the younger or older group, and subordinate other Mesoproterozoic components. In the overlying, amphibolite to eclogite facies lower part of the Seve Nappe Complex, where the metasediments are dominated by feldspathic quartzites, calcsilicate-rich psammites and marbles, most units have bimodal signatures similar to the Särv Nappes, but more dispersed; one has a unimodal signature very similar to the Ordovician turbidites of the Jämtlandian Nappes. In the overlying Upper Allochthon, Lower Kä li (Baltica-proximal, Virisen Terrane), Late Ordovician quartzites provide unimodal signatures dominated by Sveconorwegian ages (sensu stricto). Further north in the Scandes, previously published zircon signatures in quartzites of the Lower Allochthon are similar to the Vemdal quartzites in Jämtland. Data from the Kalak Nappes at 708N are in no way exotic to the Sveconorwegian Baltoscandian margin. They do show a Timanian influence (ages of c. 560-610 Ma), as would be expected from the palinspastic reconstructions of the nappes. Thus the detrital zircon signatures reported here and published elsewhere provide supporting evidence for a continuation northwards of the Sveconorwegian Orogen in the Neoproterozoic, from type areas in the south, along the Baltoscandian margin of Baltica into the high Arctic.

Original languageEnglish
Title of host publicationNew perspectives on the Caledonides of Scandinavia and related areas
EditorsF. Corfu, D. Gasser, D.M. Chew
Place of PublicationLondon
PublisherGeological Society of London
Number of pages25
ISBN (Electronic)978-1-86239-377-6
Publication statusPublished - 2014

Publication series

SeriesGeological Society London, Special Publications

Programme Area

  • Programme Area 4: Mineral Resources


Dive into the research topics of 'The Baltoscandian margin detrital zircon signatures of the central Scandes'. Together they form a unique fingerprint.

Cite this