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机译:“地球化学,锆石U-Pb和Hf同位素的勘察,NW Sanandaj-Sirjan区,伊朗:在新Tethyan岩石划分期间对中生代 - 新生代岩浆岩浆岩石的影响”[Gondwana Res。,62,2018,227-245]
State Key Laboratory of Lithospheric Evolution Institute of Geology and Geophysics Chinese Academy of Sciences;
State Key Laboratory of Lithospheric Evolution Institute of Geology and Geophysics Chinese Academy of Sciences;
State Key Laboratory of Lithospheric Evolution Institute of Geology and Geophysics Chinese Academy of Sciences;
Research Institute for Earth Sciences Geological Survey of Iran;
Institute for Advanced Studies in Basic Sciences;
Research Institute for Earth Sciences Geological Survey of Iran;
State Key Laboratory of Lithospheric Evolution Institute of Geology and Geophysics Chinese Academy of Sciences;
State Key Laboratory of Lithospheric Evolution Institute of Geology and Geophysics Chinese Academy of Sciences;
State Key Laboratory of Lithospheric Evolution Institute of Geology and Geophysics Chinese Academy of Sciences;
State Key Laboratory of Lithospheric Evolution Institute of Geology and Geophysics Chinese Academy of Sciences;
State Key Laboratory of Lithospheric Evolution Institute of Geology and Geophysics Chinese Academy of Sciences;
机译:“地球化学,锆石U-Pb和Hf同位素的勘察,NW Sanandaj-Sirjan区,伊朗:在新Tethyan岩石划分期间对中生代 - 新生代岩浆岩浆岩石的影响”[Gondwana Res。,62,2018,227-245]
机译:伊朗西部新特提斯缝合线的Sanandaj-Sirjan区:锆石U-Pb证据表明冈瓦纳北部古生代晚期裂陷和侏罗纪造山运动
机译:Sanandaj-Sirjan区在伊朗西部Neo-Tethyan Suture区:锆石U-PB证据证明已故古生代北部北部吉隆坡和中侏罗腊奥发生的证据
机译:伊朗西部新特提斯缝合线的Sanandaj-Sirjan区:锆石U-Pb证据表明冈瓦纳北部古生代晚期裂陷和侏罗纪造山运动