Reflected and refracted seismic profiles in Taiwan and southeastern China
Crustal structures are imaged by active-source experiments.
We used both refracted and reflected phases to model the crustal structures.
The crustal evolution involved the closed rift basin in Fujian and Taiwan orogen.
![](https://sgylab.gl.ntu.edu.tw/wp-content/uploads/2012/09/1-s2.0-S0040195115005156-gr11_lrg.jpg)
Kuo, Y.W., C.Y. Wang, H. Kuo-Chen *, X. Jin, H.T. Cai, J.Y. Lin, F.T. Wu, H.Y. Yen, B.S. Huang, W.T. Liang, D. Okaya, and L. Brown (2015) Crustal structures from the Wuyi-Yunkai orogen to the Taiwan orogen: the onshore-offshore wide-angle seismic experiments of the TAIGER and ATSEE projects, Tectonophysics, doi: 10.1016/j.tecto.2015.09.014.