Fig. 7 Seismic reflection data across the NMSZ.

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Presentation transcript:

Fig. 7 Seismic reflection data across the NMSZ. Seismic reflection data across the NMSZ. (A) Location map of the marine seismic reflection line M6 acquired along the Mississippi River, MO-155 well (orange star), and NMSZ seismicity (green circles). CGF, Cottonwood Grove fault. (B) Unmarked (top) and interpreted (bottom) seismic line M6. The Axial fault and the CGF deform the base of the Quaternary alluvium [marked by the Eocene/Quaternary unconformity (Q/Eo)], Cenozoic, and Mesozoic semi-consolidated sediments to the top of the Ordovician rocks. Vertical displacements increase with age of geologic unit on each fault from ~25 m at the base of the Quaternary to ~40 m at the top of the Cretaceous sediments to ~60 m at the top of the Ordovician rocks, indicating a long-lived history of deformation along both faults throughout the Cenozoic and possibly the Mesozoic (WG, Paleocene-Eocene Wilcox Group; Kr, Upper Cretaceous sediments; Pz, Ordovician sedimentary rocks). (C) Hypocenter locations (green circles) within 10 km of the seismic line projected onto the profile show the Axial fault as a vertical fault that extends to depths of 12 km beneath the seismic line. Focal mechanisms show predominant left-lateral strike-slip movement along the Axial fault. Whether the Axial fault and the Cottonwood Grove faults are two distinct structures at depth or part of a flower strike-slip system is still debated. Maria Beatrice Magnani et al. Sci Adv 2017;3:e1701593 Copyright © 2017 The Authors, some rights reserved; exclusive licensee American Association for the Advancement of Science. No claim to original U.S. Government Works. Distributed under a Creative Commons Attribution NonCommercial License 4.0 (CC BY-NC).