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For 77 sites, thermal demagnetization allowed determination of a characteristic magnetization (ChRM) with site-mean 95% confidence limit, α95, ≤15°. The ChRM is carried predominantly or entirely by hematite. Fold and reversal tests from two of the sampled localities indicate that the characteristic magnetization is synfolding, likely acquired during the earliest stages of deformation. Additionally, a modified conglomerate test at one locality and the nearly uniform direction of ChRM across the Devonian to Permian age units clearly reveals the secondary nature of the characteristic magnetization. Finally, the ChRM directions are discordant from any expected Paleozoic directions. Paleomagnetic poles calculated from the ChRM directions fall near the Cenozoic portion of the apparent polar wander path for South America. We interpret these observations to indicate widespread chemical remagnetization of these Paleozoic strata during, but prior to completion of, Cenozoic Andean folding."},{"label":"DOI","value":"10.1029/98JB02848"},{"label":"Volume","value":"103"},{"label":"Publication Date","value":"D:12 M:10 Y:1998"},{"label":"Publication Information","value":"Copyright 1998 American Geophysical Union. The original published version of this article may be found at http://dx.doi.org/10.1029/98JB02848."}],"description":"Tertiary remagnetization of Paleozoic rocks from the Eastern Cordillera and sub-Andean Belt of Bolivia","sequences":[{"@type":"sc:Sequence","canvases":[{"@id":"https://iiif.quartexcollections.com/portland/iiif/4a945391-dd9c-4968-a812-b5156986a7fe/canvas/_1","@type":"sc:Canvas","label":"Tertiary remagnetization of Paleozoic rocks from the Eastern 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