Tectonophysics, v. 361, n. 1, p. 61-82, 2003. http://dx.doi.org/10.1016/S0040-1951(02)00561-9International audienc
EGU General Assembly 2020, Online, 4–8 May 2020Studies of mountain belts worldwide have shown that t...
Geological Society of America. Special Paper, v. 358, p. 189-213, 2002. http://dx.doi.org/10.1130/0-...
The ocean margin island of Taiwan is a geodynamic body of young and complex build. It is the site of...
Tectonophysics, v. 361, n. 1, p. 61-82, 2003. http://dx.doi.org/10.1016/S0040-1951(02)00561-9Interna...
The Taiwan orogen is forming due to the oblique collision between the Eurasian continental margin a...
The Kenting Mélange on the Hengchun Peninsula, Taiwan, formed through tectonic shearing of subductio...
The Eurasian Margin is obliquely colliding with the Luzon Arc to form the Taiwan orogen. This config...
International audienceThe Taiwanese range has resulted from the collision between the Luzon volcanic...
The collision process around Taiwan can be distinguished as subduction stage and mature arc-continen...
Studies of mountain belts worldwide have shown that the structural, mechanical, and kinematic evolut...
Studies of mountain belts worldwide show that along-strike changes are common in their foreland fold...
Studies of mountain belts worldwide show that along‐strike changes are common in their foreland fold...
Studies of mountain belts worldwide show that along‐strike changes are common in their foreland fold...
Studies of mountain belts worldwide show that along‐strike changes are common in their foreland fold...
Abstract not availableXinchang Zhang, Peter A. Cawood, Chi-Yue Huang, Yuejun Wang, Yi Yan, M. Santos...
EGU General Assembly 2020, Online, 4–8 May 2020Studies of mountain belts worldwide have shown that t...
Geological Society of America. Special Paper, v. 358, p. 189-213, 2002. http://dx.doi.org/10.1130/0-...
The ocean margin island of Taiwan is a geodynamic body of young and complex build. It is the site of...
Tectonophysics, v. 361, n. 1, p. 61-82, 2003. http://dx.doi.org/10.1016/S0040-1951(02)00561-9Interna...
The Taiwan orogen is forming due to the oblique collision between the Eurasian continental margin a...
The Kenting Mélange on the Hengchun Peninsula, Taiwan, formed through tectonic shearing of subductio...
The Eurasian Margin is obliquely colliding with the Luzon Arc to form the Taiwan orogen. This config...
International audienceThe Taiwanese range has resulted from the collision between the Luzon volcanic...
The collision process around Taiwan can be distinguished as subduction stage and mature arc-continen...
Studies of mountain belts worldwide have shown that the structural, mechanical, and kinematic evolut...
Studies of mountain belts worldwide show that along-strike changes are common in their foreland fold...
Studies of mountain belts worldwide show that along‐strike changes are common in their foreland fold...
Studies of mountain belts worldwide show that along‐strike changes are common in their foreland fold...
Studies of mountain belts worldwide show that along‐strike changes are common in their foreland fold...
Abstract not availableXinchang Zhang, Peter A. Cawood, Chi-Yue Huang, Yuejun Wang, Yi Yan, M. Santos...
EGU General Assembly 2020, Online, 4–8 May 2020Studies of mountain belts worldwide have shown that t...
Geological Society of America. Special Paper, v. 358, p. 189-213, 2002. http://dx.doi.org/10.1130/0-...
The ocean margin island of Taiwan is a geodynamic body of young and complex build. It is the site of...