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机译:华北克拉通东部河北东部古近纪至E古代的地壳演化:石RIM属碎屑锆石的SHRIMP U-Pb定年和原位Hf同位素研究的新证据
Institute of Geology, Chinese Academy of Geological Sciences, 26 Baiwanzhuang Road, Beijing 100037, China,Department of Geosciences, National Taiwan University, Taipei, Taiwan;
Institute of Geology, Chinese Academy of Geological Sciences, 26 Baiwanzhuang Road, Beijing 100037, China;
Institute of Geology, Chinese Academy of Geological Sciences, 26 Baiwanzhuang Road, Beijing 100037, China;
School of Earth & Environmental Sciences, University of Wollongong, Wollongong, NSW 2522, Australia;
Institute of Geology, Chinese Academy of Geological Sciences, 26 Baiwanzhuang Road, Beijing 100037, China;
Institute of Geology, Chinese Academy of Geological Sciences, 26 Baiwanzhuang Road, Beijing 100037, China;
Institute of Geology, Chinese Academy of Geological Sciences, 26 Baiwanzhuang Road, Beijing 100037, China;
Institute of Geology, Chinese Academy of Geological Sciences, 26 Baiwanzhuang Road, Beijing 100037, China;
Department of Geosciences, National Taiwan University, Taipei, Taiwan;
Detrital zircon; Eoarchean; SHRIMP dating; Hf-isotopes; Eastern Hebei; North China Craton;
机译:华北克拉通草丛石英岩中古代碎屑锆石的SHRIMP U-Pb和CAMECA 1280氧同位素结果:3.8 Ga AGO地壳重现的证据
机译:U-Pb年龄和元古生界静二榆组碎屑锆石的Hf同位素揭示了华北克拉通东部前寒武纪地壳演化
机译:eoarchean在印度Dharwar Craton中的中间核石成分进化:来自Detrital Zircon U-Pb和HF同位素的证据
机译:华北克拉通宣龙型沉积铁矿的地质年代学研究:川岭沟组碎屑锆石U-Pb年龄的证据
机译:南美洲的岩浆历史和地壳成因:现代河流中U-Pb年龄和碎屑锆石的Hf同位素的限制。
机译:华北克拉顿东北地壳的大陆地壳增长率:来自Laoha河的U-Pb约会和Lu-HF同位素的限制