Cambrian-Ordovician paleogeography of Baltica

T. H. Torsvik, P. D. Ryan, A. Trench, D. A.T. Harper

Research output: Contribution to journalArticle

48 Citations (Scopus)

Abstract

Recent paleomagnetic data and existing paleontological evidence show that Baltica occupied temperate southern latitudes during Cambrian and Early Ordovician time, but was inverted with reference to its present orientation. Hence, the currently opposed margins of the Baltic and Laurentian shield were not conterminous in the early Paleozoic. Laurentian and Baltic late Precambrian rifting episodes may therefore have occurred along unrelated continental margins. Closure of the Tornquist Sea was accompanied by the counterclockwise rotation of Baltica relative to Avalonia in Early to Middle Ordovician time. This rotation, initiated in Late Cambrian-Early Ordovician time, was coeval with the Finnmarkian orogeny in the northern Scandinavian Caledonides. -Authors

Original languageEnglish
Pages (from-to)7-10
Number of pages4
JournalGeology
Volume19
Issue number1
DOIs
Publication statusPublished - 1991
Externally publishedYes

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Baltica
paleogeography
Ordovician
Avalonia
orogeny
rifting
continental margin
shield
Precambrian
Paleozoic

Cite this

Torsvik, T. H. ; Ryan, P. D. ; Trench, A. ; Harper, D. A.T. / Cambrian-Ordovician paleogeography of Baltica. In: Geology. 1991 ; Vol. 19, No. 1. pp. 7-10.
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Cambrian-Ordovician paleogeography of Baltica. / Torsvik, T. H.; Ryan, P. D.; Trench, A.; Harper, D. A.T.

In: Geology, Vol. 19, No. 1, 1991, p. 7-10.

Research output: Contribution to journalArticle

TY - JOUR

T1 - Cambrian-Ordovician paleogeography of Baltica

AU - Torsvik, T. H.

AU - Ryan, P. D.

AU - Trench, A.

AU - Harper, D. A.T.

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