Postseismic deformation following the 1999 Chi-Chi earthquake, Taiwan : implication for lower-crust rheology
On 1999 September 21, the Mw 7.6 Chi-Chi earthquake ruptured a segment of the Chelungpu Fault, a frontal thrust fault of the Western Foothills of Taiwan. The stress perturbation induced by the rupture triggered a transient deformation across the island, which was well recorded by a wide network of c...
Main Authors: | Rousset, Baptiste, Barbot, Sylvain, Avouac, Jean-Philippe, Hsu, Ya-Ju |
---|---|
Format: | Journal Article |
Language: | English |
Published: |
2013
|
Subjects: | |
Online Access: | https://hdl.handle.net/10356/96876 http://hdl.handle.net/10220/18092 |
Similar Items
-
Lower-crustal rheology and thermal gradient in the Taiwan orogenic belt illuminated by the 1999 Chi-Chi earthquake
by: Tang, Chi-Hsien, et al.
Published: (2019) -
A precursory ULF signature for the Chi-Chi earthquake in Taiwan
by: Y. Akinaga, et al.
Published: (2001-01-01) -
Seismic behavior in central Taiwan : response to stress evolution following the 1999 Mw 7.6 Chi-Chi earthquake
by: Wu, Yih-Min, et al.
Published: (2014) -
ULF/ELF emissions observed in Japan, possibly associated with the Chi-Chi earthquake in Taiwan
by: K. Ohta, et al.
Published: (2001-01-01) -
The Possible Observation of Slow Slip Events Prior to the Occurrence of the 1999 Chi-Chi Earthquake
by: Cheng-Horng Lin
Published: (2012-01-01)