The use of earthquake rate changes as a stress meter at kilauea volcano

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ABSTRACT Stress changes in the Earth's crust are generally estimated from model calculations that use near-surface deformation as an observational constraint. But the widespread


correlation of changes of earthquake activity with stress1,2,3,4,5 has led to suggestions that stress changes might be calculated from earthquake occurrence rates obtained from seismicity


catalogues. Although this possibility has considerable appeal, because seismicity data are routinely collected and have good spatial and temporal resolution, the method has not yet proven


successful, owing to the nonlinearity of earthquake rate changes with respect to both stress and time. Here, however, we present two methods for inverting earthquake rate data to infer


stress changes, using a formulation for the stress- and time-dependence of earthquake rates6. Application of these methods at Kilauea volcano, in Hawaii, yields good agreement with


independent estimates, indicating that earthquake rates can provide a practical remote-sensing stress meter. Access through your institution Buy or subscribe This is a preview of


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ADDITIONAL ACCESS OPTIONS: * Log in * Learn about institutional subscriptions * Read our FAQs * Contact customer support SIMILAR CONTENT BEING VIEWED BY OTHERS WERE CHANGES IN STRESS STATE


RESPONSIBLE FOR THE 2019 RIDGECREST, CALIFORNIA, EARTHQUAKES? Article Open access 17 June 2020 ESTIMATION OF THE ORIENTATION OF STRESS IN THE EARTH’S CRUST WITHOUT EARTHQUAKE OR BOREHOLE


DATA Article Open access 09 September 2021 STRESS-DRIVEN RECURRENCE AND PRECURSORY MOMENT-RATE SURGE IN CALDERA COLLAPSE EARTHQUAKES Article 05 February 2024 REFERENCES * Simpson, R. W.


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Article  ADS  CAS  Google Scholar  Download references ACKNOWLEDGEMENTS We thank A. Rubin for useful suggestions for this manuscript. AUTHOR INFORMATION AUTHORS AND AFFILIATIONS * US


Geological Survey, Menlo Park, 94025, California, USA James Dieterich & Valérie Cayol * Université B. Pascal, Clermont Ferrand, France Valérie Cayol * Hawaiian Volcano Observatory, US


Geological Survey, 96718, Hawaii, USA Paul Okubo Authors * James Dieterich View author publications You can also search for this author inPubMed Google Scholar * Valérie Cayol View author


publications You can also search for this author inPubMed Google Scholar * Paul Okubo View author publications You can also search for this author inPubMed Google Scholar CORRESPONDING


AUTHOR Correspondence to James Dieterich. RIGHTS AND PERMISSIONS Reprints and permissions ABOUT THIS ARTICLE CITE THIS ARTICLE Dieterich, J., Cayol, V. & Okubo, P. The use of earthquake


rate changes as a stress meter at Kilauea volcano . _Nature_ 408, 457–460 (2000). https://doi.org/10.1038/35044054 Download citation * Received: 22 March 2000 * Accepted: 24 August 2000 *


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