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SEPTEMBER 2019  |  VOLUME 29, NUMBER 9
                                                SCIENCE

                                                  4   Deep slab collision during Miocene subduction
                                                      causes uplift along crustal-scale reverse faults in
                                                      Fiordland, New Zealand
       GSA TODAY (ISSN 1052-5173 USPS 0456-530) prints news       Keith Klepeis et al.
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       April is a combined issue). GSA TODAY is published by The   Cover: Graduate student Peter Lindquist (University of Vermont)
       Geological Society of America  Inc. (GSA) with offices at   examines exposures of Cretaceous gneiss in eastern Fiordland where
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       3300 Penrose Place, Boulder, Colorado, USA, and a mail-  crustal-scale reverse faults placed a large slice of lower crust up and
       ing address of P.O. Box 9140, Boulder, CO 80301-9140, USA.
       GSA provides this and other forums for the presentation   to the east (right) over middle and upper crustal rocks. The faulting
       of diverse opinions and positions by scientists worldwide,   occurred at 8–7 Ma when a subducting slab of ocean crust collided
       regardless of race, citizenship, gender, sexual orientation,   with preexisting material at ~100 km depth beneath Fiordland.
       religion, or political viewpoint. Opinions presented in this   Photo by Keith Klepeis. See related article, p. 4–10.
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