scholarly journals Active Fault along the Chelungpu Fault, Central Taiwan, Especially its Close Coincidence with the Location of the 1999 Chichi Earthquake Fault.

2003 ◽  
Vol 112 (1) ◽  
pp. 18-34 ◽  
Author(s):  
Yoko OTA ◽  
Mitsuhisa WATANABE ◽  
Yasuhiro SUZUKI ◽  
Hiroshi SAWA
Geosciences ◽  
2021 ◽  
Vol 11 (3) ◽  
pp. 139
Author(s):  
Giancarlo Molli ◽  
Isabelle Manighetti ◽  
Rick Bennett ◽  
Jacques Malavieille ◽  
Enrico Serpelloni ◽  
...  

Based on the review of the available stratigraphic, tectonic, morphological, geodetic, and seismological data, along with new structural observations, we present a reappraisal of the potential seismogenic faults and fault systems in the inner northwest Apennines, Italy, which was the site, one century ago, of the devastating Mw ~6.5, 1920 Fivizzano earthquake. Our updated fault catalog provides the fault locations, as well as the description of their architecture, large-scale segmentation, cumulative displacements, evidence for recent to present activity, and long-term slip rates. Our work documents that a dense network of active faults, and thus potential earthquake fault sources, exists in the region. We discuss the seismogenic potential of these faults, and propose a general tectonic scenario that might account for their development.


Minerals ◽  
2018 ◽  
Vol 8 (9) ◽  
pp. 385 ◽  
Author(s):  
Li-Wei Kuo ◽  
Jyh-Rou Huang ◽  
Jiann-Neng Fang ◽  
Jialiang Si ◽  
Haibing Li ◽  
...  

Graphitization of carbonaceous materials (CM) has been experimentally demonstrated as potential evidence of seismic slip within a fault gouge. The southern segment of the Longmenshan fault, a CM-rich-gouge fault, accommodated coseismic slip during the 2008 Mw 7.9 Wenchuan earthquake and potentially preserves a record of processes that occurred on the fault during the slip event. Here, we present a multi-technique characterization of CM within the active fault zone of the Longmenshan fault from the Wenchuan earthquake Fault Scientific Drilling-1. By contrast with field observations, graphite is pervasively and only distributed in the gouge zone, while heterogeneously crystallized CM are present in the surrounding breccia. The composite dataset that is presented, which includes the localized graphite layer along the 2008 Wenchuan earthquake principal slip zone, demonstrates that graphite is widely distributed within the active fault zone. The widespread occurrence of graphite, a seismic slip indicator, reveals that surface rupturing events commonly occur along the Longmenshan fault and are characteristic of this tectonically active region.


2007 ◽  
Vol 18 (2) ◽  
pp. 223 ◽  
Author(s):  
Andrew Tien-Shun Lin ◽  
Shun-Min Wang ◽  
Jih-Hao Hung ◽  
Ming-Shyan Wu ◽  
Chih-Shae Liu

2004 ◽  
Vol 159 (1) ◽  
pp. 9-16 ◽  
Author(s):  
C. P. Chang ◽  
C. T. Wang ◽  
T. Y. Chang ◽  
K. S. Chen ◽  
L. S. Liang ◽  
...  

2007 ◽  
Vol 18 (1) ◽  
pp. 055 ◽  
Author(s):  
Yoko Ota ◽  
Masanobu Shishikura ◽  
Kiyoshi Ichikawa ◽  
Mitsuhisa Watanabe ◽  
Makoto Yanagida ◽  
...  

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