Millennial slip rate of the Longitudinal Valley fault from river terraces : implications for convergence across the active suture of eastern Taiwan
The Longitudinal Valley fault is a key element in the active tectonics of Taiwan. It is the principal structure accommodating convergence across one of the two active sutures of the Taiwan orogeny. To understand more precisely its role in the suturing process, we analyzed fluvial terraces along the...
Saved in:
Main Authors: | Shyu, J. Bruce H., Sieh, Kerry, Avouac, Jean-Philippe, Chen, Wen-Shan, Chen, Yue-Gau |
---|---|
Format: | Article |
Language: | English |
Published: |
2012
|
Subjects: | |
Online Access: | https://hdl.handle.net/10356/95555 http://hdl.handle.net/10220/8478 |
Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
Institution: | Nanyang Technological University |
Language: | English |
Similar Items
-
Geomorphic analysis of the central range fault, the second major active structure of the longitudinal valley suture, eastern Taiwan
by: Shyu, J. Bruce H., et al.
Published: (2012) -
Tandem suturing and disarticulation of the Taiwan orogen revealed by its neotectonic elements
by: Shyu, J. Bruce H., et al.
Published: (2012) -
Re-evaluation of the surface ruptures of the November 1951 earthquake series in eastern Taiwan, and its neotectonic implications
by: Shyu, J. Bruce H., et al.
Published: (2012) -
Holocene slip rate of the central Garlock fault in Southeastern Searles Valley, California
by: McGill, Sally, et al.
Published: (2012) -
Neotectonic architecture of Taiwan and its implications for future large earthquakes
by: Shyu, J. Bruce H., et al.
Published: (2012)