《Table 2 Electron microprobe analyses of plagioclases in the plagiogranite from the Diyanmiao ophiol

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《"Discovery of the Plagiogranites in the Diyanmiao Ophiolite, Southeastern Central Asian Orogenic Belt, Inner Mongolia, China and Its Tectonic Significance"》

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Major elements were analyzed by X-ray fluorescence（XRF）（Rigaku 3270E） at the Tianjin Institute of Geology and Mineral Resources，China Geological Survey.Analytical precision was generally better than 2%for most oxides，monitored by analyses of Chinese national standard samples GSR–1，GSR–2 and GSR–3.Trace element data also were obtained at the Tianjin Institute of Geology and Mineral Resources，China Geological Survey by inductively coupled plasma mass spectrometer（ICP-MS）using the analytical procedure of Liu et al.（2008）.The analytical precisions for most trace elements are greater than 5%，monitored by analyses of Chinese national standard samples GSR–1 and GSR–3.The analytical precision was better than 5%for trace elements.The major and trace elemental data from plagiogranite samples are listed in Table 3.