作者: Ian Metcalfe
DOI: 10.1144/SP315.2
关键词: Permian 、 Terrane 、 Paleozoic 、 Paleontology 、 Devonian 、 Suture (geology) 、 Gondwana 、 Geology 、 Plate tectonics 、 Island arc
摘要: SE Asia comprises a collage of continental terranes derived directly or indirectly from the India–Australian margin of eastern Gondwana. The Late Palaeozoic and Mesozoic evolution of the region involved the rifting and separation of three elongate continental slivers from eastern Gondwana and the successive opening and closure of three ocean basins, the Palaeo-Tethys, Meso-Tethys and Ceno-Tethys. The Sukhothai Island Arc System, including the Linchang, Sukhothai and Chanthaburi terranes, is identified between the Sibumasu and …