Lenhardt, NilsBöhnel, HaraldHinderer, MatthiasHornung, Jens2014-11-042014-11-042013-05Lenhardt, N, Böhnel, H, Hinderer, M & Hornung, J 2014, 'Paleocurrent direction measurements in a volcanic setting by means of anisotropy of magnetic susceptibility : a case study from the lower Miocene Tepoztlán Formation (Transmexican Volcanic Belt, Central Mexico)', Sedimentary Geology, vol. 290, no. 5, pp. 1-14.0037-0738 (print)1879-0968 (online)10.1016/j.sedgeo.2013.02.013http://hdl.handle.net/2263/42481Sources of ancient volcanic rocks are often unknown if they are either eroded and/or covered by younger deposits. This problem, as well as the provenance of reworked volcaniclastic, fluvial and mass-flow deposits, can be partially solved by the application of anisotropy of the magnetic susceptibility (AMS). For massive and poorly sorted volcaniclastic rocks in particular this may be the only way of finding reliable transport directions and therefore allowing for paleogeographic reconstructions. Here, we present a data set of 428 AMS measurements and 249 measurements of sedimentary paleocurrent indicators from the Miocene Tepoztlán Formation at the southern edge of the Transmexican Volcanic Belt (Central Mexico). The highest degree of reliability of AMS measurements is gained for data from lava samples and the lowest from mass flows. Sedimentary structures in sandstones and conglomerates such as trough cross-stratification, asymmetric ripple marks, and the shape of scours and channels could be used to calibrate the results from AMS data and to prove their reliability. AMS data on fluvial deposits point to a drainage systemwith aW–E flow direction, indicating an outflow of the river system into the ancient Gulf of Mexico.en© 2013 Elsevier B.V. All rights reserved. Notice : this is the author’s version of a work that was accepted for publication in Sedimentary Geology. Changes resulting from the publishing process, such as peer review, editing, corrections, structural formatting, and other quality control mechanisms may not be reflected in this document. Changes may have been made to this work since it was submitted for publication. A definitive version was subsequently published in Sedimentary Geology, vol. 290, no. 5, pp. 1-14 2013. doi : 10.1016/j.sedgeo.2013.02.013.Paleocurrent directionVolcaniclasticMioceneMexicoTransmexican Volcanic Belt (Central Mexico)Anisotropy of the magnetic susceptibility (AMS)Postprint Article