Two-phase subduction and subsequent collision defines the Paleotethyan tectonics of the southeastern Tibetan Plateau: Evidence from zircon U-Pb dating, geochemistry, and structural geology of the Sanjiang orogenic belt, southwest China
T.N.Yang Y.Ding H.R.Zhang J.W.Fan M.J.Liang X.H.Wang
Institute of Geology,Chinese Academy of Geological Sciences,Beijing 100037,China Institute of Geomechanics,Chinese Academy of Geological Sciences,Beijing 100081,China
国内会议
北京
英文
1905-1905
2014-10-19(万方平台首次上网日期,不代表论文的发表时间)