A west-dipping seismogenic boundary beneath the Chia-Yi area of western Taiwan
Taiwan is one of the most typical arc-continental collision systems in the world. The Taiwan orogeny is often explained by the thin-skin model, where a shallow decollement, with depths of less than 10 km, is considered as the crustal deformation boundary for generating significant mountains on the i...
| Main Authors: | , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Chinese Geoscience Union
2018-01-01
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| Series: | Terrestrial, Atmospheric and Oceanic Sciences |
| Online Access: |
http://tao.cgu.org.tw/media/k2/attachments/v295p499.pdf
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