Research Article| September 12, 2018 Triggered Seismicity after North Korea’s 3 September 2017 Nuclear Test Jiayuan Yao; Jiayuan Yao aLaboratory of Seismology and Physics of Earth’s Interior, School of Earth and Space Sciences, University of Science and Technology of China, Hefei, Anhui 230026, China, kakayao@mail.ustc.edu.cndongzhi@mail.ustc.edu.cnluzhou@mail.ustc.edu.cn Search for other works by this author on: GSW Google Scholar Dongdong Tian; Dongdong Tian aLaboratory of Seismology and Physics of Earth’s Interior, School of Earth and Space Sciences, University of Science and Technology of China, Hefei, Anhui 230026, China, kakayao@mail.ustc.edu.cndongzhi@mail.ustc.edu.cnluzhou@mail.ustc.edu.cn Search for other works by this author on: GSW Google Scholar Zhou Lu; Zhou Lu aLaboratory of Seismology and Physics of Earth’s Interior, School of Earth and Space Sciences, University of Science and Technology of China, Hefei, Anhui 230026, China, kakayao@mail.ustc.edu.cndongzhi@mail.ustc.edu.cnluzhou@mail.ustc.edu.cn Search for other works by this author on: GSW Google Scholar Li Sun; Li Sun bChina Earthquake Networks Center, Beijing 100045, China, sunli@seis.ac.cn Search for other works by this author on: GSW Google Scholar Lianxing Wen Lianxing Wen cDepartment of Geosciences, State University of New York at Stony Brook, Stony Brook, New York 11794 U.S.A., lianxing.wen@stonybrook.edudAlso at Laboratory of Seismology and Physics of Earth’s Interior, School of Earth and Space Sciences, University of Science and Technology of China, Hefei, Anhui 230026, China. Search for other works by this author on: GSW Google Scholar Author and Article Information Jiayuan Yao aLaboratory of Seismology and Physics of Earth’s Interior, School of Earth and Space Sciences, University of Science and Technology of China, Hefei, Anhui 230026, China, kakayao@mail.ustc.edu.cndongzhi@mail.ustc.edu.cnluzhou@mail.ustc.edu.cn Dongdong Tian aLaboratory of Seismology and Physics of Earth’s Interior, School of Earth and Space Sciences, University of Science and Technology of China, Hefei, Anhui 230026, China, kakayao@mail.ustc.edu.cndongzhi@mail.ustc.edu.cnluzhou@mail.ustc.edu.cn Zhou Lu aLaboratory of Seismology and Physics of Earth’s Interior, School of Earth and Space Sciences, University of Science and Technology of China, Hefei, Anhui 230026, China, kakayao@mail.ustc.edu.cndongzhi@mail.ustc.edu.cnluzhou@mail.ustc.edu.cn Li Sun bChina Earthquake Networks Center, Beijing 100045, China, sunli@seis.ac.cn Lianxing Wen cDepartment of Geosciences, State University of New York at Stony Brook, Stony Brook, New York 11794 U.S.A., lianxing.wen@stonybrook.edudAlso at Laboratory of Seismology and Physics of Earth’s Interior, School of Earth and Space Sciences, University of Science and Technology of China, Hefei, Anhui 230026, China. Publisher: Seismological Society of America First Online: 12 Sep 2018 Online Issn: 1938-2057 Print Issn: 0895-0695 © Seismological Society of America Seismological Research Letters (2018) 89 (6): 2085–2093. https://doi.org/10.1785/0220180135 Article history First Online: 12 Sep 2018 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Jiayuan Yao, Dongdong Tian, Zhou Lu, Li Sun, Lianxing Wen; Triggered Seismicity after North Korea’s 3 September 2017 Nuclear Test. Seismological Research Letters 2018;; 89 (6): 2085–2093. doi: https://doi.org/10.1785/0220180135 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietySeismological Research Letters Search Advanced Search ABSTRACT The 3 September 2017 nuclear test conducted by the Democratic People’s Republic of Korea was followed by a series of small seismic events. In this study, we conduct a survey of small seismic events from 1 May 2017 to 25 April 2018 near North Korea’s nuclear test site. We report 88 seismic events, including the 2017 nuclear test, the collapse event 8.5 min later, and 86 earthquakes afterward. Among the 86 earthquakes, 11 are well constrained to be distributed along a near north–south direction within a region of 2 km, ∼8.4 km north of the test site. The null detection before the 2017 test and the intense seismicity after the test, along with the predicted normal tensile stress the 2017 test applied on the fault, provide strong evidence that the 2017 test triggered these earthquakes. Some characteristics (the distance to the nuclear test center, depth, and magnitude) of these triggered aftershocks fit the general characteristics of the aftershocks in the Nevada National Security Site and the Semipalatinsk test site after nuclear tests, but the aftershocks of North Korea’s 2017 test exhibit a different evolution lasting at least eight months with two bursts occurring on early December 2017 and early February 2018 and an otherwise general low occurrence rate, possibly caused by a different geological setting of the test site. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
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