Research Paper GEOSPHERE Late Pleistocene rates of rock uplift and faulting at the boundary between the southern Coast Ranges and the western Transverse GEOSPHERE, v. 17 no. 3 Ranges in California from reconstruction and luminescence dating https://doi.org/10.1130/GES02274.1 14 figures; 2 tables of the Orcutt Formation CORRESPONDENCE:
[email protected] Ian S. McGregor and Nathan W. Onderdonk Department of Geological Sciences, California State University–Long Beach, 1250 Bellflower Boulevard, Long Beach, California 90804, USA CITATION: McGregor, I.S., and Onderdonk, N.W., 2021, Late Pleistocene rates of rock uplift and faulting at the boundary between the southern Coast Ranges ABSTRACT consistent with models that attribute shortening across the Santa Maria Basin and the western Transverse Ranges in California from to accommodation of clockwise rotation of the western Transverse Ranges and reconstruction and luminescence dating of the Orcutt Formation: Geosphere, v. 17, no. 3, p. 932–956, https:// The western Transverse Ranges and southern Coast Ranges of California suggest that rotation has continued into late Quaternary time. doi .org /10.1130 /GES02274.1. are lithologically similar but have very different styles and rates of Quaternary deformation. The western Transverse Ranges are deformed by west-trending Science Editor: Andrea Hampel folds and reverse faults with fast rates of Quaternary fault slip (1–11 mm/yr) ■ INTRODUCTION Associate Editor: Jeff Lee and uplift (1–7 mm/yr). The southern Coast Ranges, however, are primarily deformed by northwest-trending folds and right-lateral strike-slip faults with The Coast Ranges of California are deformed by northwest-striking faults Received 15 April 2020 Revision received 16 November 2020 much slower slip rates (3 mm/yr or less) and uplift rates (<1 mm/yr).