| 内蒙古敖包吐铅锌矿床花岗岩类年代学及其地球化学特征 |
| Received:May 15, 2013 Revised:April 05, 2014 点此下载全文 |
| 引用本文：DONG XuZhou,ZHOU ZhenHua,WANG RunHe,LI JinWen,HE ShuJun.2014.Geochronology and geochemistry of granite in Aobaotu Pb-Zn deposit, Inner Mongolia[J].Mineral Deposits,33(2):323~338 |
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| Author Name | Affiliation | E-mail | | DONG XuZhou | School of Earth Science and Mineral Resources, China University of Geosciences, Beijing 100083, China | | | ZHOU ZhenHua | MLR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China | zhzhou@cags.ac.cn | | WANG RunHe | Inner Mongolia Institute of Geology and Mineral Resources, Hohhot 010010, Inner Mongolia, China | | | LI JinWen | MLR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China | | | HE ShuJun | School of Earth Science and Mineral Resources, China University of Geosciences, Beijing 100083, China | |
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| 基金项目:本文为中国地质调查局地质调查项目（12120113093600、1212011085260）联合资助成果 |
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| 中文摘要:内蒙古敖包吐铅锌矿是大兴安岭南段成矿带上新发现的矿床，成矿与花岗闪长斑岩关系密切。对矿区内花岗闪长斑岩和花岗岩的LA-ICP-MS锆石U-Pb测年结果表明，形成年龄分别为（140.0±0.5）Ma（MSWD=1.3）和（151.6±0.4）Ma（MSWD=1.2），为晚侏罗世—早白垩世岩浆活动的产物。岩石地球化学测试结果显示，花岗闪长斑岩具有高硅（w（SiO2）=65.51%~67.85%），富碱（w（Na2O+K2O）=6.86%~7.81%），贫P2O5的特征，A/CNK在0.95~1.02之间，富集微量元素K、Rb、Nd，亏损Ta、Nb、P、Ti，为I型花岗岩。花岗岩的A/CNK值为1.58，属强过铝质岩石。Rb/Sr比值大于0.9，为S型花岗岩。敖包吐花岗岩的全岩Pb同位素组成显示，其206Pb/204Pb为18.398~18.755，207Pb/204Pb为15.534~15.541，208Pb/204Pb为38.386~38.542，铅具有混合来源特征。岩浆很可能来源于岩石圈地幔，并受到一定程度的混染。敖包吐花岗岩类可能与兴蒙造山带东段的后碰撞环境有关，并受到与古太平洋板块俯冲有关的弧后伸展影响。 |
| 中文关键词:地球化学 花岗岩 LA-ICP-MS锆石U-Pb定年 敖包吐铅锌矿床 大兴安岭 内蒙古 |
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| Geochronology and geochemistry of granite in Aobaotu Pb-Zn deposit, Inner Mongolia |
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| Abstract:The Aobaotu ore deposit, located in the southern part of the Da Hinggan Mountains metallogenic belt, is a newly discovered lead-zinc deposit. The results of zircon LA-ICP-MS U-Pb dating for granodiorite-porphyries and granites in the study area show that granodiorite-porphyries were formed at (140.0±0.5) Ma(MSWD=1.3), meanwhile, the age of granites is (151.6±0.4) Ma (MSWD=1.2), which indicates that they are the products of magma movement during Late Jurassic-Early Cretaceous period. An analysis of major elements, trace elements and REE has revealed that the granodiorite-porphyries from the Aobaotu deposit are characterized by high silica (65.51%~67.85%) and alkali (w(Na2O+K2O)=6.86%~7.81%), low P2O5, with the A/CNK being 0.95~1.02, enrichment of K, Rb and Nd, and depletion of Ta, Nb, P and Ti, suggesting I-type granitoids. Characteristics of Aobaotu granites are similar to those of S-type granitoids. The Pb isotope values show crust-mantle mixing characteristics, with the 206Pb/204Pb values ranging from 18.398 to 18.755, 207Pb/204Pb values between 15.534 and 15.541, and 208Pb/204Pb values between 38.386 and 38.542. The magma source might have mostly originated from the lithospheric mantle components which were transformed or affected by the subduction components, and its formation was probably closely related to the post-collision of the Xing'an-Mongolia belt and the subduction of the Paleo-Pacific Ocean. |
| keywords:geochemistry granite LA-ICP-MS zircon U-Pb dating Aobaotu Pb-Zn deposit Da Hinggan Mountains Inner Mongolia |
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