Fluid inclusion evidence characterizing the P-T-f evolution of the HP-UHP rocks and veins from the Dabie-Sulu orogenic belt

摘要：

The Dabie-Sulu Triassic orogenic belt in central-east China was formed by northward subduction of the Yangtze plate beneath the North China plate.

作者: Shen K. Zhang Z. Sun Y. Shu L. Li, S.H.

作者单位: Shandong institute of Geological Sciences, Jinan, China 250013 Institute of geology, Chinese Academy of Geological Sciences, Beijing, China 100037

会议类型: 国际会议

会议名称: Asian Current Research on Fluid Inclusions(第七届亚洲流体包裹体国际会议)(ACROFI VII-2018)

会议地点: 北京

会议语种:英文

页码: 115-116

在线出版日期: 2018-09-11（万方平台首次上网日期，不代表论文的发表时间）