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Journal of the Geological Society; September 2006; v. 163; no. 5; p. 753-759; DOI: 10.1144/0016-76492005-126
© 2006 Geological Society of London
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Original Article

Was Baltica right-way-up or upside-down in the Neoproterozoic?

Peter A. Cawood and Sergei A. Pisarevsky

Tectonics Special Research Centre, School of Earth and Geographical Sciences, The University of Western Australia, 35 Stirling Highway, Crawley, WA 6009, Australia (e-mail: pcawood@tsrc.uwa.edu.au)

Baltica is a progeny of Rodinia, born from the breakup of the supercontinent in the Neoproterozoic. Within Rodinia, Baltica is generally placed adjacent to NE Laurentia but in a variety of configurations, which vary by up to 3000 km along the strike of the Laurentian margin and include both right-way-up and upside-down orientations (current coordinates). Geological and palaeomagnetic data show that the only viable reconstruction juxtaposes the western Scandinavian margin of Baltica, in its right-way-up orientation, against the Rockall–Scotland–SE Greenland segment of Laurentia.




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