Carboniferous to Triassic polyphase tectonic transition in the western North China craton: A retroarc basin response to termination of the middle segment of the Paleo-Asian Ocean.

Autor: Jiaopeng Sun1 sunjiaopeng@nwu.edu.cn, Yunpeng Dong1 dongyp@nwu.edu.cn, Junfeng Zhao1, Qiang Chen2
Zdroj: Geological Society of America Bulletin. Sep/Oct2024, Vol. 136 Issue 9, p4149-4174. 26p.
Databáze: Academic Search Ultimate