C
Chii-Wen Lin
Researcher at Central Geological Survey, MOEA
Publications - 6
Citations - 99
Chii-Wen Lin is an academic researcher from Central Geological Survey, MOEA. The author has contributed to research in topics: Fault (geology) & Fault scarp. The author has an hindex of 4, co-authored 6 publications receiving 88 citations.
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Journal ArticleDOI
Late Holocene Paleoseismicity of the Southern Part of the Chelungpu Fault in Central Taiwan: Evidence from the Chushan Excavation Site
Wen-Shan Chen,Chih-Cheng Yang,I-Chin Yen,Long-Sheng Lee,Kun-Jie Lee,Hsiao-Chin Yang,Hui-Cheng Chang,Yoko Ota,Chii-Wen Lin,Wei-Hsiung Lin,Tung-Sheng Shih,Shih-Ting Lu +11 more
TL;DR: Based on core-boring estimates, the vertical displace- ment on both sides is 7 m along a 24 east-dipping thrust fault, which ruptured during the Chichi earthquake.
Journal ArticleDOI
Late Holocene paleoearthquake activity in the middle part of the Longitudinal Valley fault, eastern Taiwan
Wen-Shan Chen,I-Chin Yen,Keegan P. Fengler,Charles M. Rubin,Chi-Cheng Yang,Hsiao-Chin Yang,Hui-Cheng Chang,Chii-Wen Lin,Wei-Hsiung Lin,Yen-Chiu Liu,Yen-Hui Lin +10 more
TL;DR: In this paper, the authors showed that the Juisui fault of the Longitudinal valley fault is the most important arc-continent collisional boundary fault between the Philippine Sea plate and the Eurasian continent.
Journal ArticleDOI
Paleoseismology of the Rueisuei Segment of the Longitudinal Valley Fault, Eastern Taiwan
TL;DR: Based on stratigraphic ordering and a statistical comparison of radiocarbon dates using the OxCal program, Wang et al. as mentioned in this paper estimate that two pre-1951 earthquake surface ruptures at the Dafu site occurred in the periods A.D. 1736-1898 and A. D. 1564-1680.
Journal ArticleDOI
Active deformation front delineated by drainage pattern analysis and vertical movement rates, southwestern Coastal Plain of Taiwan
TL;DR: In this article, a blind thrust may exist between the plain (PL), the tilted tableland (TT), and the low hills (LH), based on geomorphology, drainage pattern and stratigraphic records.
Late Holocene Paleoseismicity of the Southern Part of the Chelungpu Fault in Central Taiwan: Evidence from the
Wen-Shan Chen,Chi-Cheng Yang,Yi-Ching Yen,Kun-Jie Lee,Hsiao-Chin Yang,Hui-Cheng Chang,Chii-Wen Lin,Wei-Hsiung Lin,Tung-Sheng Shih,Shih-Ting Lu,Jing Liu-Zeng,Yann Klinger,Xiwei Xu,Cécile Lasserre,Wenbing Chen,Paul Tapponnier,Biao Zhang,Christoforos Benetatos,Douglas S. Dreger,Anastasia Kiratzi,Annette M. Veilleux,Diane I. Doser,Andrew B. Lockman,Richard M. Allen,Ekrem Zor,Eric Sandvol,Arif H. Gasanov,Gurban Yetirmishli,Laurentiu Danciu,G-Akis Tselentis,Elisabetta Giampiccolo,Salvatore D'Amico,Domenico Patanè,Stefano Gresta +33 more
TL;DR: Based on core-boring estimates, the vertical displace- ment on both sides is 7 m along a 24 east-dipping thrust fault, which ruptured during the Chichi earthquake as discussed by the authors.