Please use this identifier to cite or link to this item: https://hdl.handle.net/10356/89837
Title: Coulomb stress transfer and accumulation on the Sagaing Fault, Myanmar, over the past 110 years and its implications for seismic hazard
Authors: Wei, Shengji
Li, Y. D.
Wang, R. J.
Zheng, Y.
Xiong, X.
Shan, B.
Zhou, Y. M.
Keywords: Earthquake Triggering
Coulomb Failure Stress
DRNTU::Science::Geology
Issue Date: 2017
Source: Xiong, X., Shan, B., Zhou, Y. M., Wei, S. J., Li, Y. D., Wang, R. J., & Zheng, Y. (2017). Coulomb stress transfer and accumulation on the Sagaing Fault, Myanmar, over the past 110 years and its implications for seismic hazard. Geophysical Research Letters, 44(10), 4781-4789. doi:10.1002/2017GL072770
Series/Report no.: Geophysical Research Letters
Abstract: Myanmar is drawing rapidly increasing attention from the world for its seismic hazard. The Sagaing Fault (SF), an active right‐lateral strike‐slip fault passing through Myanmar, has been being the source of serious seismic damage of the country. Thus, awareness of seismic hazard assessment of this region is of pivotal significance by taking into account the interaction and migration of earthquakes with respect to time and space. We investigated a seismic series comprising10 earthquakes with M > 6.5 that occurred along the SF since 1906. The Coulomb failure stress modeling exhibits significant interactions among the earthquakes. After the 1906 earthquake, eight out of nine earthquakes occurred in the positively stress‐enhanced zone of the preceding earthquakes, verifying that the hypothesis of earthquake triggering is applicable on the SF. Moreover, we identified three visible positively stressed earthquake gaps on the central and southern SF, on which seismic hazard is increased.
URI: https://hdl.handle.net/10356/89837
http://hdl.handle.net/10220/46403
ISSN: 0094-8276
DOI: 10.1002/2017GL072770
Rights: © 2017 American Geophysical Union. This paper was published in Geophysical Research Letters and is made available as an electronic reprint (preprint) with permission of American Geophysical Union. The published version is available at: [http://dx.doi.org/10.1002/2017GL072770]. One print or electronic copy may be made for personal use only. Systematic or multiple reproduction, distribution to multiple locations via electronic or other means, duplication of any material in this paper for a fee or for commercial purposes, or modification of the content of the paper is prohibited and is subject to penalties under law.
Fulltext Permission: open
Fulltext Availability: With Fulltext
Appears in Collections:EOS Journal Articles

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