Surface Rupture and Behavior of Thrust Faults Probed in Taiwan
Document Type
Article
Department or Administrative Unit
Geological Sciences
Publication Date
10-19-2006
Abstract
Taiwan's destructive Chi-chi earthquake of September 21, 1999, was a dramatic expression of active tectonic processes at a complex collisional plate boundary. It resulted in more than 2,400 causalities and tens of billions of dollars in property loss. During the earthquake, an 80-km stretch of the country's mountainous backbone moved upward and westward along the range-bounding Chelungpu thrust fault (Figure la). A team of earthquake geologists from the United States, in collaboration with geoscientists from Academia Sinica, National Taiwan University and the Central Geological Survey of Taiwan, worked together to address questions concerning the recurrence of large-magnitude earthquakes along reverse faults in Taiwan.
Recommended Citation
Rubin, C. M., Sieh, K., Chen, Y. G., Lee, J. C., Chu, H. T., Yeats, R., Mueller, K., & Chan, Y. C. (2001). Surface rupture and behavior of thrust faults probed in Taiwan. Eos, Transactions American Geophysical Union, 82(47), 565-567 https://doi.org/10.1029/01eo00331
Journal
Eos
Comments
This article was originally published in Eos. The full-text article from the publisher can be found here.
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