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RB 93/00021 New overprint from the Delamerian fold belt and the Cambro-Ordovician APWP for Gondwanaland.
A paleomagnetic study of the mid- to Late Cambrian sedimentary rocks in the northern Delamerian fold belt reveals an overprint acquired after regional folding during the Cambro-Ordovician. The paleopole position, based on data from eight sites, is...-
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Published: 01 Apr 1993
