Matches in SemOpenAlex for { <https://semopenalex.org/work/W4224880009> ?p ?o ?g. }
- W4224880009 endingPage "229364" @default.
- W4224880009 startingPage "229364" @default.
- W4224880009 abstract "The Xiaojiang Fault (XJF) Zone locates in the southeastern of Tibetan Plateau and defines the boundary between the South China and Sichuan-Yunnan blocks. Historical large earthquakes were hosted on the XJF, though its seismic hazard in the near future is under debate. In this study, we utilize portable broad-band seismic network to unravel the microseismic activities along XJF, and to further investigate the fault structures and their properties. Adopting PALM, a newly developed earthquake detection algorithm, we obtained ~13,000 relocated events. The micro-seismicity reveals widespread off-fault structures showing conjugate geometry, while the major faults present low seismicity. The fault branches conjugate to the main-fault present intensive microseismicity, which hosts repeating events and presents high b-value. Regional GPS stations reflect slips are mostly concentrated along the XJF, while the slip rate on off-fault branches correlates with seismic activities on these structures. Combining with other recent seismological and magnetotellurics evidences, we suggest a low strength on these off-fault structures, which may partially release tectonic stress loading and serve as a barrier for future big earthquakes. On the XJF, the microseismic events are clustered on the fault junctions with low b-value. A special set of clusters between 25°N to 25.5°N show an along-strike variation of depth from 10 to 25-km, imaging the boundary between creeping and locked fault portions. We revisit the seismic hazard problem of XJF, and conclude that XJF is at the late stage of inter-seismic period." @default.
- W4224880009 created "2022-04-27" @default.
- W4224880009 creator A5006292733 @default.
- W4224880009 creator A5019685555 @default.
- W4224880009 creator A5034198254 @default.
- W4224880009 creator A5052197567 @default.
- W4224880009 creator A5064826514 @default.
- W4224880009 creator A5067841153 @default.
- W4224880009 creator A5076825933 @default.
- W4224880009 creator A5086032799 @default.
- W4224880009 creator A5088669600 @default.
- W4224880009 creator A5090517968 @default.
- W4224880009 date "2022-06-01" @default.
- W4224880009 modified "2023-10-15" @default.
- W4224880009 title "Microseismicity along Xiaojiang Fault Zone (Southeastern Tibetan Plateau) and the characterization of interseismic fault behavior" @default.
- W4224880009 cites W1512351913 @default.
- W4224880009 cites W1684220077 @default.
- W4224880009 cites W1732576836 @default.
- W4224880009 cites W1761867724 @default.
- W4224880009 cites W1904429860 @default.
- W4224880009 cites W1923991055 @default.
- W4224880009 cites W1969174948 @default.
- W4224880009 cites W1970298430 @default.
- W4224880009 cites W1971834521 @default.
- W4224880009 cites W1984296399 @default.
- W4224880009 cites W1988691001 @default.
- W4224880009 cites W2003555242 @default.
- W4224880009 cites W2003936065 @default.
- W4224880009 cites W2004428748 @default.
- W4224880009 cites W2011590140 @default.
- W4224880009 cites W2013856174 @default.
- W4224880009 cites W2019178381 @default.
- W4224880009 cites W2019784274 @default.
- W4224880009 cites W2024237931 @default.
- W4224880009 cites W2024423630 @default.
- W4224880009 cites W2024866298 @default.
- W4224880009 cites W2026327684 @default.
- W4224880009 cites W2027701123 @default.
- W4224880009 cites W2038034424 @default.
- W4224880009 cites W2043592751 @default.
- W4224880009 cites W2044709616 @default.
- W4224880009 cites W2054324603 @default.
- W4224880009 cites W2056688530 @default.
- W4224880009 cites W2056894820 @default.
- W4224880009 cites W2063293928 @default.
- W4224880009 cites W2065017756 @default.
- W4224880009 cites W2068222277 @default.
- W4224880009 cites W2075028436 @default.
- W4224880009 cites W2076547603 @default.
- W4224880009 cites W2081428288 @default.
- W4224880009 cites W2085878288 @default.
- W4224880009 cites W2087563892 @default.
- W4224880009 cites W2099857446 @default.
- W4224880009 cites W2104292910 @default.
- W4224880009 cites W2105465498 @default.
- W4224880009 cites W2105658614 @default.
- W4224880009 cites W2108656739 @default.
- W4224880009 cites W2136944354 @default.
- W4224880009 cites W2141107952 @default.
- W4224880009 cites W2147129972 @default.
- W4224880009 cites W2163379050 @default.
- W4224880009 cites W2164610741 @default.
- W4224880009 cites W2165646430 @default.
- W4224880009 cites W2167327624 @default.
- W4224880009 cites W2168276911 @default.
- W4224880009 cites W2319880916 @default.
- W4224880009 cites W2472399859 @default.
- W4224880009 cites W2520209389 @default.
- W4224880009 cites W2528961483 @default.
- W4224880009 cites W2536348194 @default.
- W4224880009 cites W2595787243 @default.
- W4224880009 cites W2747813374 @default.
- W4224880009 cites W2766247933 @default.
- W4224880009 cites W2767368244 @default.
- W4224880009 cites W2792357269 @default.
- W4224880009 cites W2792887548 @default.
- W4224880009 cites W2794885244 @default.
- W4224880009 cites W2904784200 @default.
- W4224880009 cites W2914754204 @default.
- W4224880009 cites W2946919159 @default.
- W4224880009 cites W2947406642 @default.
- W4224880009 cites W2972562525 @default.
- W4224880009 cites W2979681142 @default.
- W4224880009 cites W2981937856 @default.
- W4224880009 cites W2982370370 @default.
- W4224880009 cites W2986126436 @default.
- W4224880009 cites W2999289209 @default.
- W4224880009 cites W3010759802 @default.
- W4224880009 cites W3041056926 @default.
- W4224880009 cites W3073445426 @default.
- W4224880009 cites W3162088004 @default.
- W4224880009 cites W3176638204 @default.
- W4224880009 cites W3184121347 @default.
- W4224880009 cites W3196810282 @default.
- W4224880009 cites W3198947267 @default.
- W4224880009 cites W3205540234 @default.
- W4224880009 cites W3208155334 @default.
- W4224880009 cites W4206243173 @default.