https://scholars.lib.ntu.edu.tw/handle/123456789/614604
DC 欄位 | 值 | 語言 |
---|---|---|
dc.contributor.author | Wu Y.M.; Chen Y.G.; Shin T.C.; Kuochen H.; Hou C.S.; Hu J.C.; Chang C.H.; Wu C.F.; Teng T.L. | en_US |
dc.contributor.author | HAO KUO-CHEN | zz |
dc.creator | Wu Y.M.; Chen Y.G.; Shin T.C.; Kuochen H.; Hou C.S.; Hu J.C.; Chang C.H.; Wu C.F.; Teng T.L. | - |
dc.date.accessioned | 2022-06-30T02:05:45Z | - |
dc.date.available | 2022-06-30T02:05:45Z | - |
dc.date.issued | 2006 | - |
dc.identifier | GPRLA | - |
dc.identifier.issn | 00948276 | - |
dc.identifier.uri | https://www.scopus.com/inward/record.uri?eid=2-s2.0-33644745539&doi=10.1029%2f2005GL024711&partnerID=40&md5=f4449b7f85a41a2b11026a2c71f489fd | - |
dc.identifier.uri | https://scholars.lib.ntu.edu.tw/handle/123456789/614604 | - |
dc.description.abstract | The 2003 Chengkung earthquake (Mw 6.8) provided diagnostic evidence for a source model showing the deformation process of the seismogenic Chihshang fault in eastern Taiwan. The aftershocks show a fault-bend at a depth of 18 km. Coseismic ground displacements recorded by strong-motion records allow us to deduce instant rupturing of this event. Our resulting model shows a fault length of ∼33 km and dip-slip dominant rupture on fault-plane deeper than 18 km. Estimated coseismic displacements constrain two fault planes: one at 5-18 km depth dipping 60°E and 18-36 km depth dipping 45°E. The uppermost fault-plane of the Chihshang Fault (0-5 km) did not break immediately after the main shock; however, it may have a major role in after-slip and even interseismic ground deformation. The Taiyuan basin developed in the hanging wall is a geomorphic feature consistent with and adequately explained by coseismic ground displacements. Copyright 2006 by the American Geophysical Union. | - |
dc.language | en-US | - |
dc.publisher | American Geophysical Union | - |
dc.relation.ispartof | Geophysical Research Letters | - |
dc.subject | Deformation; Earthquake effects; Mathematical models; Seismology; Shock waves; Tectonics; Coseismic displacements; Fault rupture inversion; Interseismic ground deformations; Neotectonics; Earthquakes; crustal deformation; deformation mechanism; earthquake; Asia; Eurasia; Far East; Taiwan | - |
dc.title | Coseismic versus interseismic ground deformations, fault rupture inversion and segmentation revealed by 2003 Mw 6.8 Chengkung earthquake in eastern Taiwan | en_US |
dc.type | journal article | en |
dc.identifier.doi | 10.1029/2005GL024711 | - |
dc.identifier.scopus | 2-s2.0-33644745539 | - |
dc.relation.journalvolume | 33 | - |
dc.relation.journalissue | 2 | - |
item.openairetype | journal article | - |
item.openairecristype | http://purl.org/coar/resource_type/c_6501 | - |
item.fulltext | no fulltext | - |
item.grantfulltext | none | - |
item.cerifentitytype | Publications | - |
crisitem.author.dept | Geosciences | - |
crisitem.author.orcid | 0000-0003-2282-9218 | - |
crisitem.author.parentorg | College of Science | - |
顯示於: | 地質科學系 |
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