冀北大滩盆地铀(钼)成矿流纹岩-花岗斑岩SHRIMP锆石U-Pb定年、地球化学及Sr-Nd同位素特征

张雅菲, 巫建华, 姜山, 刘玄, 吴仁贵, 刘帅, 郭国林. 冀北大滩盆地铀(钼)成矿流纹岩-花岗斑岩SHRIMP锆石U-Pb定年、地球化学及Sr-Nd同位素特征[J]. 岩石学报, 2016, 32(1): 193-211.
引用本文: 张雅菲, 巫建华, 姜山, 刘玄, 吴仁贵, 刘帅, 郭国林. 冀北大滩盆地铀(钼)成矿流纹岩-花岗斑岩SHRIMP锆石U-Pb定年、地球化学及Sr-Nd同位素特征[J]. 岩石学报, 2016, 32(1): 193-211.
ZHANG YaFei, WU JianHua, JIANG Shan, LIU Xuan, WU RenGui, LIU Shuai, GUO GuoLin. SHRIMP U-Pb geochronology, geochemistry and Sr-Nd isotopes of the uranium-(molybdenum) related rhyolite and granitic porphyry, Datan, northern Heibei[J]. Acta Petrologica Sinica, 2016, 32(1): 193-211.
Citation: ZHANG YaFei, WU JianHua, JIANG Shan, LIU Xuan, WU RenGui, LIU Shuai, GUO GuoLin. SHRIMP U-Pb geochronology, geochemistry and Sr-Nd isotopes of the uranium-(molybdenum) related rhyolite and granitic porphyry, Datan, northern Heibei[J]. Acta Petrologica Sinica, 2016, 32(1): 193-211.

冀北大滩盆地铀(钼)成矿流纹岩-花岗斑岩SHRIMP锆石U-Pb定年、地球化学及Sr-Nd同位素特征

  • 基金项目:

    本文受国家自然科学基金项目(41372071)和中国核工业集团公司项目(中核地计[2008]74号)联合资助.

详细信息

SHRIMP U-Pb geochronology, geochemistry and Sr-Nd isotopes of the uranium-(molybdenum) related rhyolite and granitic porphyry, Datan, northern Heibei

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  • 大滩火山岩盆地位于华北克拉通北缘,燕辽多金属(Mo-U-Ag-Pb-Zn)成矿带西段,沽源-红山子铀成矿亚带西南段。高精度SHRIMP锆石U-Pb定年表明,盆地内张家口组流纹岩和侵入其中的花岗斑岩分别形成于140.2±1.9Ma(2σ,MSWD=1.7)和131.7±1.1Ma(2σ,MSWD=0.8)。全岩主、微量元素特征显示,流纹岩和花岗斑岩均富集Si、Fe、Ga、Rb、Pb、Th、U、Zr、Hf、Nb、Ta和LREE,亏损Al、Mg、Ti、Ba、Sr、Eu、Cr、Ni和HREE,为典型的A型花岗岩特征。全岩Nd同位素研究表明,二者具有相似的εNd(t)(分别为-15.9和-16.5)和tDM2值(分别为2267Ma和2220Ma),暗示二者具有相同的岩浆来源。元素相关性分析表明,母岩浆从流纹岩演化至花岗斑岩经历了一定程度的钾长石和黑云母的结晶分异,导致了后者Si、U、HREE的进一步富集,以及Fe、Mg、Ti、Al、Sr、Ba、Eu、Zr、LREE等元素的相对亏损。结合前人工作,我们认为流纹岩和花岗斑岩形成于华北克拉通岩石圈减薄及破坏的板内伸展背景,来源于古元古代(ca. 2.2~2.3Ga)火成地壳物质(英云闪长质、花岗闪长质岩石)的部分熔融。结合全岩Rb-Sr等时线年龄及前人获得的矿石U-Pb年龄推断,该区主要铀(钼)矿化时代介于105~110Ma,明显晚于流纹岩和花岗斑岩的成岩时代。通过与区域上的产铀盆地(沽源)对比,以及对流纹岩和花岗斑岩的U含量等特征分析认为,两者(尤其是花岗斑岩)是很好的铀矿成矿物质来源,暗示了大滩盆地具有良好的成矿前景。
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出版历程
收稿日期:  2015-03-01
修回日期:  2015-07-28
刊出日期:  2016-01-31

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