Page 3 - i1052-5173-29-9+FY19

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.
and information for more than 22,000 GSA member readers
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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
®
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.
publication do not reflect official positions of the Society.
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