机译:U-Pb的斑脱辉岩年龄和Hf,Nd同位素化学限制了Fennoscandian Shield从1.6 Ga到0.9 Ga的反复铁镁质岩浆作用
Department of Geosciences University of Arizona;
Department of Geosciences University of Arizona;
Department of Geology GeoBiosphere Science Centre Lund University;
Department of Earth and Atmospheric Sciences University of Alberta;
Department of Geosciences University of Arizona;
Department of Geology Washington State University;
Laboratory for Isotope Geology Swedish Museum of Natural HistoryDepartment of Earth Sciences Uppsala University;
机译:U-Pb铅锌矿年龄和Hf,Nd同位素化学限制了Fennoscandian Shield从1.6 Ga到0.9 Ga的反复铁镁质岩浆作用
机译:在芬诺斯堪的亚地区追踪1271–1246 Ma中央斯堪的纳维亚白云岩组镁铁质岩浆作用:Moslatt和Borgefjell白云岩的U–Pb Baddeleyite和Hf同位素数据
机译:印度南部西部Dharwar Craton的Pb-Pb Baddeleyite年龄的镁铁岩脉:进入2.21-2.18 Ga全球镁铁质岩浆作用的窗口
机译:中国西北中亚造山带黄山洞含硫化物的镁铁质-超镁铁质侵入体的Hf-Sr-Nd-Pb同位素和岩石化学
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:Baddeleyite从大型复合体存款:基于U-PB(ID-TIMS)和LA-ICP-MS数据的北极地区(NE Fennoscandand Shield)中的Archean-古生代羽流过程的重要性