School of Earth and Environmental Engineering, Hefei University of Technology E-mail: zhangdayu1985@126.com;
School of Earth and Environmental Engineering, Hefei University of Technology;
School of Earth and Environmental Engineering, Hefei University of Technology;
School of Earth and Environmental Engineering, Hefei University of Technology;
School of Earth and Environmental Engineering, Hefei University of Technology;
机译:中国东北乌格图土山斑岩铜钼矿床和花岗岩类的SIMS锆石U-Pb和辉钼矿Re-Os年代学,Hf同位素和全岩地球化学及其地质意义
机译:u-Pb锆石,地球化学和SR-ND-HF同位素限制来自Wunugetushan Porphyry矿床的侵入,中国东北地区:蒙古 - 埃尔加内亚矿化带的三叠系侏罗纪矿化的含义
机译:u-Pb锆石,地球化学和SR-ND-HF同位素限制来自Wunugetushan Porphyry矿床的侵入,中国东北地区:蒙古 - 埃尔加内亚矿化带的三叠系侏罗纪矿化的含义
机译:MO-(Cu)和Cu-Mo轴承花岗岩的地球化学鉴定及其意义:中国轴承侵入的证据
机译:Palea Kavala的矿物学,岩石学,稳定同位素和流体包裹体研究将与侵入有关的和过渡的Fakos斑岩Cu-Mo还原为超热Au-Te矿石系统。
机译:南海神湖地区含甲烷水合物的沉积物中生物标志物的地球化学意义
机译:北昆仑山矿床中晚期三叠纪矿石和贫瘠侵入之间的地球化学对比,NW中国:附件矿物的约束(锆石和磷灰石)