HO-HAN HSUCHAR-SHINE LIUChang, Ya TingYa TingChangChang, Jih HsinJih HsinChangKo, Chia ChunChia ChunKoChiu, Shye DonqShye DonqChiuChen, Song ChuenSong ChuenChen2019-06-192019-06-192017/11/113679120https://scholars.lib.ntu.edu.tw/handle/123456789/411194? 2017 The architecture and distribution of mud diapirs are shaped by tectonic activity, sediment filling and unbalanced loading characteristics. Mud diapir development also controls spatial variations of intraslope basins in slope areas and can spur upwaAccretionary prism | Convergent tectonics | Gas hydrates | Intraslope basin | Mud diapir | Reflection seismic profiles | SW TaiwanAccretionary prism; Convergent tectonics; Gas hydrates; Intraslope basin; Mud diapir; Reflection seismic profiles; SW Taiwan[SDGs]SDG13[SDGs]SDG14accretionary prism; basin evolution; diapir; gas hydrate; mud; seismic reflection; tectonics; Taiwanjournal article10.1016/j.jseaes.2017.05.0072-s2.0-85020078338WOS:000414883300015https://api.elsevier.com/content/abstract/scopus_id/85020078338