Sharp Changes of Crustal Seismic Anisotropy Across the Central Tanlu Fault Zone in East China
| dc.citation.articleNumber | e2022GL099184 | en_US |
| dc.citation.issueNumber | 1 | en_US |
| dc.citation.journalTitle | Geophysical Research Letters | en_US |
| dc.citation.volumeNumber | 50 | en_US |
| dc.contributor.author | Miao, Wenpei | en_US |
| dc.contributor.author | Niu, Fenglin | en_US |
| dc.contributor.author | Chen, Haichao | en_US |
| dc.date.accessioned | 2023-01-27T14:47:12Z | en_US |
| dc.date.available | 2023-01-27T14:47:12Z | en_US |
| dc.date.issued | 2023 | en_US |
| dc.description.abstract | Both seismic and geodetic data suggested that the ∼120-km long Weifang segment of the Tanlu fault zone, a large-scale active strike-slip system at east China, is a seismic gap with no obvious along-strike shear motion at surface. Measuring crustal deformation around the segment is crucial to constrain stress/strain buildup and potential seismic risk at the fault. We measured crustal and upper mantle seismic anisotropy using P-to-S converted waves at the Moho (Pms) and core-mantle boundary (SKS) recorded by broadband arrays across the Weifang fault segment. The measured crustal anisotropy inside the fault zone shows a fast direction of ∼NNE, parallel to the fault orientation. Right east to the fault zone, the fast axis rotates by almost 90° to ESE. The crustal anisotropy within the fault zone could be caused by aligned microcracks and foliated minerals due to long-lasting shear motion inside the fault zone. | en_US |
| dc.identifier.citation | Miao, Wenpei, Niu, Fenglin and Chen, Haichao. "Sharp Changes of Crustal Seismic Anisotropy Across the Central Tanlu Fault Zone in East China." <i>Geophysical Research Letters,</i> 50, no. 1 (2023) Wiley: https://doi.org/10.1029/2022GL099184. | en_US |
| dc.identifier.digital | 2022-Miao | en_US |
| dc.identifier.doi | https://doi.org/10.1029/2022GL099184 | en_US |
| dc.identifier.uri | https://hdl.handle.net/1911/114253 | en_US |
| dc.language.iso | eng | en_US |
| dc.publisher | Wiley | en_US |
| dc.rights | This is an open access article under the terms of the Creative Commons Attribution-NonCommercial-NoDerivs License, which permits use and distribution in any medium, provided the original work is properly cited, the use is non-commercial and no modifications or adaptations are made. | en_US |
| dc.rights.uri | https://creativecommons.org/licenses/by-nc-nd/4.0/ | en_US |
| dc.title | Sharp Changes of Crustal Seismic Anisotropy Across the Central Tanlu Fault Zone in East China | en_US |
| dc.type | Journal article | en_US |
| dc.type.dcmi | Text | en_US |
| dc.type.publication | publisher version | en_US |
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