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09-Feb-2020 05:13

See our Privacy Policy and Third Party Partners to learn more about the use of data and your rights. Growth of magnetite has been variably linked to fluid-bearing events or clay diagenesis, and the development of a chemical remagnetization as a result of such events.By combining newly determined ages of illitization in folds with new paleomagnetic results in Mexico’s central Sierra Madre Oriental, this study demonstrates the ability to associate a radiometric age with synfolding remagnetizations.Extensive work has shown that many carbonates around the world have been remagnetized (Jackson and Swanson-Hysell, 2012; Mc Cabe and Elmore, 1989; Van der Voo and Torsvik, 2012), highlighting the potentially wide-scale application of this approach.Deformation of the area occurred during the Late Cretaceous to Paleogene, with the basins dominated by folding and intense water-rock interaction (see Fitz-Díaz et al., 2011b, for details); while the platforms were thrust dominated and showed much less fluid-rock interaction (Aranda-Gómez et al., 2000; Fitz-Díaz et al., 2012).Deformation in the central Sierra Madre Oriental was dated (Fitz-Díaz et al., 2014) using the Ar/Ar illite dating technique; that study targeted fold and thrust dating in the region.

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This hypothesis was further supported by Katz et al. Scanning electron microscopy, X-ray diffraction, stable isotope, and geochronological analyses of samples from several folds showed that illite grew along shear-related horizons during folding.Magnetic directions from 28 sites in the mid-Cretaceous section of the Tamaulipas Formation in the central Sierra Madre (CSM) are summarized in Table 1.



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