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机译:西伯利亚克拉通新元古代活动大陆边缘的岩浆作用演化和碳酸盐-花岗岩联系:热年代学重建1
Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch of the Russian Academy of Sciences, Novosibirsk;
Krasnoyarsk Research Institute of Geology, Geophysics and Mineral Resources, Krasnoyarsk;
Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch of the Russian Academy of Sciences, Novosibirsk,Novosibirsk State University;
Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch of the Russian Academy of Sciences, Novosibirsk,Novosibirsk State University;
Novosibirsk State University,Institute of Computational Mathematics and Mathematical Geophysics Siberian Branch of the Russian Academy of Sciences, Novosibirsk;
Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch of the Russian Academy of Sciences, Novosibirsk,School of Earth, Environmental and Biological Sciences, Queensland University of Technology, Brisbane, Australia;
Sobolev Institute of Geology and Mineralogy Siberian Branch of the Russian Academy of Sciences, Novosibirsk;
Novosibirsk State University;
Karpinsky Russian Geological Research Institute, Saint Petersburg;
机译:堤防岩岩在埃德基兰的西伯利亚Craton变革活跃的大陆边缘的演变中
机译:西伯利亚克拉通西南部新元古代活动边界最终(576-546 Ma)发育阶段的Adakite-Gabbro-Anorthosite岩浆作用
机译:NeoProteroZoio Intraplate Magmatism沿西伯利亚Craton的西部边缘:对罗迪尼亚的分手的影响超大了
机译:华北克拉通西南缘中新元古代京铁山BIF矿床成因:岩石学和地球化学约束
机译:加利福尼亚州诺帕山脉南部的新元古代强尼组和斯特林石英岩的地球化学:解释气候,构造和沉积过程在重建裂谷大陆边缘的早期演化中的作用。
机译:华北克拉通南缘中元古代Bingmagou组沉积环境与沉积演化
机译:堤防岩浆广场在埃德基甘山西伯利亚克拉顿转变活跃的大陆边缘的演变