| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 8912923 | Earth-Science Reviews | 2018 | 39 Pages |
Abstract
A structure reconstruction reveals that the North Luzon Trough forearc strata have experienced multiple stages of thrust deformation from subduction through collision to obduction. These deformations account for the mechanism and processes to develop the modern-forming highly sheared SSZ-bearing forearc Lichi Mélange tectonically in the western Coastal Range during the last 1â¯Ma.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
Chi-Yue Huang, Wen-Huang Chen, Ming-Huei Wang, Chiou-Ting Lin, Shengxiong Yang, Xuejie Li, Mengming Yu, XiXi Zhao, Kenn-Ming Yang, Char-Shine Liu, Yu-Huan Hsieh, Ron Harris,