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  4. Is the Lishan fault of Taiwan active?
 
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Is the Lishan fault of Taiwan active?

Journal
Tectonophysics
Journal Volume
661
Pages
210-214
Date Issued
2015
Author(s)
Francis Wu
Wu-Lung Chang
Chih-Yu Chang
Ching-Yu Cheng
Naoshi Hirata
HAO KUO-CHEN  
DOI
10.1016/j.tecto.2015.09.002
URI
https://www.scopus.com/inward/record.uri?eid=2-s2.0-84946499227&doi=10.1016%2fj.tecto.2015.09.002&partnerID=40&md5=c6c36f6b1de18a20755ee63498f3940f
https://scholars.lib.ntu.edu.tw/handle/123456789/614583
Abstract
The Lishan fault has been characterized alternately as a major discontinuity in stratigraphy, structures and metamorphism, a ductile shear zone, a tectonic suture or non-existent. In addition to being a geological boundary, it also marks transitions in subsurface structures. Thus, the seismicity to the west of the fault permeates through the upper and mid-crust while beneath the Central Range it is noticeably less and largely concentrated in the upper 12. km. A prominent west-dipping conductive zone extends upward to meet the Lishan fault. Also, the eastward increase of crust thickness from ~. 30. km in the Taiwan Strait quickens under the Lishan fault to form a root of over 50. km under the Central Range. In the past, the small magnitude seismicity along the Lishan fault has been noticed but is too diffuse for definitive association with the fault. Recent processing of aftershock records of the 1999 Mw 7.6 Chi-Chi earthquake using Central Weather Bureau data and, especially, data from three post-Chi-Chi deployments of seismic stations across central Taiwan yielded hypocenters that appear to link directly to the Lishan structure. The presence of a near 4-km-long vertical seismic zone directly under the surface trace of the Lishan fault indicates that it is an active structure from the surface down to about 35. km, and the variety of focal mechanisms indicates that the fault motion can be complex and depth-dependent. © 2015 Elsevier B.V.
Subjects
Balloons; Earthquakes; Seismology; Stratigraphy; Active fault; Central weather bureaux; ChiChi earthquake; Ductile shear zone; Focal mechanism; Geological boundaries; Seismic arrays; Subsurface structures; Faulting; active fault; aftershock; Chi-Chi earthquake 1999; crustal thickness; ductile deformation; earthquake hypocenter; fault slip; fault zone; focal mechanism; seismicity; shear zone; tectonic setting; Taiwan
Publisher
Elsevier B.V.
Type
journal article

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