| 西拉沐伦成矿带中生代花岗岩浆活动与钼成矿作用 |
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| 引用本文： | 曾庆栋,刘建明,褚少雄,付国立,于文斌,李泽明,高玉友,李元九,孙燕,周伶俐,段晓侠,张松,王永彬.西拉沐伦成矿带中生代花岗岩浆活动与钼成矿作用[J].吉林大学学报(地球科学版),2011,41(6):1705-1714,1725. |
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| 作者姓名： | 曾庆栋 刘建明 褚少雄 付国立 于文斌 李泽明 高玉友 李元九 孙燕 周伶俐 段晓侠 张松 王永彬 |
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| 作者单位： | 中国科学院矿产资源研究重点实验室/地质与地球物理研究所,北京,100029;内蒙古自治区赤峰市国土资源局,内蒙古,赤峰024006;核工业243大队,内蒙古,赤峰024006 |
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| 基金项目： | 国家自然科学基金项目(40972065); 全国危机矿山找矿专项综合研究项目(20089931); 国家重点自然科学基金项目(41030421) |
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| 摘 要： | 位于华北克拉通北缘的西拉沐伦成矿带内花岗岩浆活动及钼矿化发育,带内主要成矿侵入体岩石类型包括二长花岗岩、斑状花岗岩、花岗斑岩及流纹斑岩,这些岩石属于高钾钙碱性和钾玄岩系列,岩浆源区为古老下地壳和新生地壳。这些侵入体形成于早—中三叠世、晚侏罗世及早白垩世。带内钼矿床包括斑岩型、石英脉型、云英岩型和火山-次火山热液型4种类型,以斑岩型矿床最为发育。带内钼矿床形成时代与相关侵入岩时代一致,也形成于早—中三叠世、晚侏罗世及早白垩世,以早白垩世钼矿床最为发育。3期成岩成矿作用分别形成于华北板块与西伯利亚板块同碰撞至后碰撞构造环境、古太平洋板块向欧亚大陆俯冲的构造环境和中国东部岩石圈减薄构造环境。
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| 关 键 词： | 花岗岩 钼矿床 中生代 西拉沐伦成矿带 |
Mesozoic Granitic Magmatism and Molybdenum Ore-Forming Processes in the Xilamulun Metallogenic Belt |
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| ZENG Qing-dong,LIU Jian-ming,CHU Shao-xiong,FU Guo-li,YU Wen-bin,LI Ze-ming,Gao Yu-you,LI Yuan-jiu,SUN Yan,ZHOU Ling-li,DUAN Xiao-xia,ZHANG Song,WANG Yong-bin.Mesozoic Granitic Magmatism and Molybdenum Ore-Forming Processes in the Xilamulun Metallogenic Belt[J].Journal of Jilin Unviersity:Earth Science Edition,2011,41(6):1705-1714,1725. |
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| Authors: | ZENG Qing-dong LIU Jian-ming CHU Shao-xiong FU Guo-li YU Wen-bin LI Ze-ming Gao Yu-you LI Yuan-jiu SUN Yan ZHOU Ling-li DUAN Xiao-xia ZHANG Song WANG Yong-bin |
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| Institution: | ZENG Qing-dong1,LIU Jian-ming1,CHU Shao-xiong1,FU Guo-li2,YU Wen-bin3,LI Ze-ming3,Gao Yu-you3,LI Yuan-jiu3,SUN Yan1,ZHOU Ling-li1,DUAN Xiao-xia1,ZHANG Song1,WANG Yong-bin1 1.Key Laboratory of Mineral Resources/Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China 2.Chifeng Bureau of Land and Resources,Chifeng 024006,Inner Mongolia,China 3.No.243 Geological Party of Nuclear Industry,China |
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| Abstract: | Granitoids and molybdenum ore deposits or ore spots are well developed in the Xilamulun metallogenic belt located on the northern margin of the North China craton.The ore-bearing intrusive rocks include monozogranite,porphyritic granite,granite porphyry and rhyolite porphyry,which belong to the high-K calc-alkaline and shoshonite series.The rock-forming materials were derived from the lower crust and juvenile crust.These granitic intrusive rocks were formed in Early-Middle Triassic,Late Jurassic and Early C... |
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| Keywords: | granite molybdenum deposits Mesozoic Xilamulun metallogenic belt |
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