Welcome to the new version of CaltechAUTHORS. Login is currently restricted to library staff. If you notice any issues, please email coda@library.caltech.edu
Published August 3, 2005 | Published + Submitted + Supplemental Material
Journal Article Open

Neotectonic architecture of Taiwan and its implications for future large earthquakes


The disastrous effects of the 1999 Chi-Chi earthquake in Taiwan demonstrated an urgent need for better knowledge of the island's potential earthquake sources. Toward this end, we have prepared a neotectonic map of Taiwan. The map and related cross sections are based upon structural and geomorphic expression of active faults and folds both in the field and on shaded relief maps prepared from a 40-m resolution digital elevation model, augmented by geodetic and seismologic data. The active tandem suturing and tandem disengagement of a volcanic arc and a continental sliver to and from the Eurasian continental margin have created two neotectonic belts in Taiwan. In the southern part of the orogen both belts are in the final stage of consuming oceanic crust. Collision and suturing occur in the middle part of both belts, and postcollisional collapse and extension dominate the island's northern and northeastern flanks. Both belts consist of several distinct neotectonic domains. Seven domains (Kaoping, Chiayi, Taichung, Miaoli, Hsinchu, Ilan, and Taipei) constitute the western belt, and four domains (Lutao-Lanyu, Taitung, Hualien, and Ryukyu) make up the eastern belt. Each domain is defined by a distinct suite of active structures. For example, the Chelungpu fault (source of the 1999 earthquake) and its western neighbor, the Changhua fault, are the principal components of the Taichung Domain, whereas both its neighboring domains, the Chiayi and Miaoli Domains, are dominated by major blind faults. In most of the domains the size of the principal active fault is large enough to produce future earthquakes with magnitudes in the mid-7 values.

Additional Information

© 2005 American Geophysical Union. Received 21 June 2004; revised 13 January 2005; accepted 22 March 2005; published 3 August 2005. We are grateful for valuable discussions with J.-P. Avouac, O. Beyssac, Y.-C. Chan, W.-C. Chi, H.-T. Chu, M.-L. Hsieh, J.-C. Hu, J.-C. Lee, C.-H. Lo, C.-Y. Lu, Y. Ota, C. Rubin, M. Simons, Q. Sung, L.S. Teng, B. Wernicke, and S.-B. Yu. Also, we have benefited from stimulating discussions with students of two field classes in Taiwan and a neotectonic seminar at National Taiwan University. The comments and suggestions of reviewers I. Manighetti and R. S. Yeats greatly helped us improve this manuscript. Our mapping would have been impossible had C.-T. Lee not made us aware that high-quality digital topography of the island existed. J. Giberson, manager of the Caltech's GIS laboratory, helped with the technical aspects of mapping. Our project in Taiwan was initially supported by private funds of Caltech's Division of Geological and Planetary Sciences and later by NSF grant EAR-0208505. This research was also supported in part by the Gordon and Betty Moore Foundation. This is Caltech Tectonics Observatory contribution 3.

Attached Files

Published - 2004JB003251.pdf

Submitted - shyu_JGR2005.pdf

Supplemental Material - shyu_JGR2005_supp_1_.pdf


Files (21.5 MB)
Name Size Download all
13.6 MB Preview Download
7.5 MB Preview Download
358.4 kB Preview Download

Additional details

August 19, 2023
August 19, 2023