Correlation of porosity variations and rheological transitions on the southern Cascadia megathrust
Author:
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences
Link
http://www.nature.com/articles/s41561-021-00740-1.pdf
Reference74 articles.
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2. Hyndman, R. D. & Wang, K. The rupture zone of Cascadia great earthquakes from current deformation and the thermal regime. J. Geophys. Res. 100, 22133–22154 (1995).
3. Hyndman, R. D. Downdip landward limit of Cascadia great earthquake rupture. J. Geophys. Res. 118, 5530–5549 (2013).
4. McCaffrey, R., King, R. W., Payne, S. J. & Lancaster, M. Active tectonics of northwestern US inferred from GPS‐derived surface velocities. J. Geophys. Res. 118, 709–723 (2013).
5. Schmalzle, G. M., McCaffrey, R. & Creager, K. C. Central Cascadia subduction zone creep. Geochem. Geophys. Geosyst. 15, 1515–1532 (2014).
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