| 内蒙古毛登地区阿鲁包格山花岗斑岩地质特征及U-Pb年代学意义 |
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| 引用本文： | 刘传宝,王强,王建忠,郎欣欣,张猛,侯冠宇.内蒙古毛登地区阿鲁包格山花岗斑岩地质特征及U-Pb年代学意义[J].矿产勘查,2018,9(7):1316-1321. |
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| 作者姓名： | 刘传宝 王强 王建忠 郎欣欣 张猛 侯冠宇 |
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| 作者单位： | 内蒙古自治区第十地质矿产勘查开发院,赤峰 024000,内蒙古自治区第十地质矿产勘查开发院,赤峰 024000,内蒙古自治区第十地质矿产勘查开发院,赤峰 024000,内蒙古自治区第十地质矿产勘查开发院,赤峰 024000,内蒙古自治区第十地质矿产勘查开发院,赤峰 024000,内蒙古自治区第十地质矿产勘查开发院,赤峰 024000 |
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| 基金项目： | 全国重要矿集区找矿预测的子项目内蒙古毛登矿集区找矿预测(编号:0747-1761SITCN072/3)资助。 |
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| 摘 要： | 阿鲁包格山花岗斑岩体地处天山-兴蒙造山系南缘,位于大兴安岭弧盆系锡林浩特岩浆弧之中,与中二叠统大石寨组上段地层和下白垩统白音高老组地层相邻。通过岩相学分析以及结合前人研究表明花岗斑岩与酸性熔岩及酸性火山碎屑岩的矿物组成与化学成分相似,指示两者为同源岩浆活动的产物。通过LA-ICP-MS U-Pb年龄测定的花岗斑岩的加权平均年龄值为(133.68±0.76) Ma(MSWD=1.04),略晚于下白垩统白音高老组酸性熔岩及酸性火山碎屑岩,表明了阿鲁包格山岩体与酸性熔岩及酸性火山碎屑岩为同期异相岩浆活动的产物。
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| 关 键 词： | 阿鲁宝格山 花岗斑岩 地质特征 年代学特征 |
| 收稿时间： | 2017/3/20 0:00:00 |
Significance of geological features and U-Pb chronology features, Alubaogeshan granite-porphyry, MaoDeng area of Inner Mongolia |
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| LIU Chuan-bao,WANG Qiang,WANG Jian-zhong,LANG Xin-xin,ZHANG Meng and HOU Guan-yu.Significance of geological features and U-Pb chronology features, Alubaogeshan granite-porphyry, MaoDeng area of Inner Mongolia[J].Mineral Exploration,2018,9(7):1316-1321. |
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| Authors: | LIU Chuan-bao WANG Qiang WANG Jian-zhong LANG Xin-xin ZHANG Meng and HOU Guan-yu |
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| Affiliation: | Inner Mongolia Tenth geological mineral Exploration Institute,Inner Mongolia,Chifeng 024000,Inner Mongolia Tenth geological mineral Exploration Institute,Inner Mongolia,Chifeng 024000,Inner Mongolia Tenth geological mineral Exploration Institute,Inner Mongolia,Chifeng 024000,Inner Mongolia Tenth geological mineral Exploration Institute,Inner Mongolia,Chifeng 024000,Inner Mongolia Tenth geological mineral Exploration Institute,Inner Mongolia,Chifeng 024000 and Inner Mongolia Tenth geological mineral Exploration Institute,Inner Mongolia,Chifeng 024000 |
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| Abstract: | Alubaogeshan granite-porphyry is located in the southern margin of Tianshan Xingmeng orogenic system, and in the Xilinhaote magmatic arc of the arc basin system of DaHinggan Mountains. The petrographic analysis and previous research results show that the mineral composition and chemical composition of granite-porphyry acidic lava and acidic volcaniclastic rocks are similar, indicating they are products of homologous magmatic activities. The weighted average age of granite porphyry determined by LA-ICP-MS U-Pb dating is 133.68Ma(+0.76Ma)(MSWD=1.04), slightly later than acidic lava and acid volcaniclastic rocks in the lower Cretaceous Baiyin Gao Lao formation, It is indicated that the Alubaogeshan intrusion, acidic lava and acidic volcaniclastic rocks are products formed by magmatism of synchronous and different lithofacies. |
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| Keywords: | Alubageshan granite porphyry geological features chronological characteristics |
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