New advances in the study of Tethyan Geodynamic System  

作　　者：Lin DING 

机构地区：[1]State Key Laboratory of Tibetan Plateau Earth System Science(LATPES),Institute of Tibetan Plateau Research,Chinese Academy of Sciences,Beijing 100101,China

出　　处：《Science China Earth Sciences》2024年第3期874-878,共5页中国科学（地球科学英文版）

摘　　要：Tethyan Ocean was initially proposed by Austrian geologist Eduard Suess in 1893. The study of the Tethyan evolution by European geologists has led to the development of modern geology, but not to the establishment of plate tectonics theory(Trümpy, 2001). With the progress in various studies, the concept of Tethys has evolved from a Mesozoic ocean into three long-term evolving oceans:Proto-Tethys, Paleo-Tethys, and Neo-Tethys (Figure 1), and their life cycles cover the entire Phanerozoic era (Wu et al., 2020).

关 键 词：GEOLOGY MESOZOIC OCEAN 

分 类 号：P542[天文地球—构造地质学]