矿床地质:2017,Vol.>>Issue(3):643-658

新疆北部青河县阿斯喀尔特铍矿区花岗质岩石年代学及地球化学特征
陕西省地质调查中心, 陕西 西安 710068,陕西省地质调查中心, 陕西 西安 710068,新疆地质矿产勘查开发局第七地质大队, 新疆 乌苏 833000,陕西省地质调查中心, 陕西 西安 710068,陕西省地质调查中心, 陕西 西安 710068,陕西省地质调查中心, 陕西 西安 710068,太原理工大学矿业工程学院, 山西 太原 030024
Geochronology and geochemistry of granitoids of Ascalt beryllium deposit in Qinghe County, northern Xinjiang
ZHANG YaFeng,LIN XinWang,ZHAO YuMei,GUO QiMing,ZHAO DuanChang,WANG Xing,ZHU WeiPeng
(Shaanxi Center of Geological Survey, Xi'an 710068, Shaanxi, China;No.7 Geological Party of Xinjiang Bureau of Geology and Mineral Exploration and Development, Wusu 833000, Xinjiang, China;College of Mining Engineering, Taiyuan University of Technology, Taiyuan 030024, Shanxi, China)
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投稿时间:2015-07-15   修订日期:2017-04-01      网络发布日期:2017-07-04
中文摘要:新疆北部青河县阿斯喀尔特铍矿床的形成与岩浆活动密切相关,是中国花岗岩型铍矿床的典型代表。对矿区斑状二云母二长花岗岩进行LA-ICP-MS锆石U-Pb年龄测试,获得其加权平均年龄为(216.7±2.8)Ma(MSWD=0.48),表明该岩体形成时代为晚三叠世,据此限定阿斯喀尔特铍矿床成矿时代略晚于216 Ma,为晚三叠世-早侏罗世。岩石具有高硅(w(SiO2)=70.86%~76.34%)、富碱(ALK=5.54~9.30)、富铝(w(Al2O3)=13.00%~14.74%,A/CNK=0.99~1.23)、低钛(w(TiO2)=0.02%~0.18%)和镁(w(MgO)=0.02%~1.21%)特征,为过铝质中钾-高钾岩石系列。稀土元素配分型式显示LREE的相对弱富集,HREE较平坦以及Eu弱-中等的负异常(δEu=0.37~0.90),呈略右倾型。微量元素Ba、Sr、Hf、Ti等具负异常,Rb、Th、K、Nb、Ta、La、Ce、Nd、Sm等具正异常,Rb/Sr比值较高(9.34~26.81),显示出S型花岗岩特征。结合区域资料,认为阿斯喀尔特铍矿矿区印支期花岗岩形成于后造山构造阶段,可能是上地壳含砂泥质岩石部分熔融的产物。
Abstract:LA-ICP-MS zircon U-Pb geochronological studies were conducted for porphyritic two-mica adamellite from the Ascalt beryllium deposit in Aershat area of Qinghe County, northern Xinjiang. The results show that the zircon 206Pb/238U weighted average age of the rocks is (216.7±2.8) Ma(MSWD=0.48), indicating that the crystallization age of the plutons is late Triassic. The Ascalt beryllium deposit is the typical representative of the granite type beryllium deposits, closely related to the magmatic plutons. The authors hold that the beryllium deposit was formed slightly later than 216 Ma in late Triassic-early Jurassic period. The granites have high SiO2 (w(SiO2)=70.86%~76.34%), ALK(ALK=5.54~9.30) and Al2O3 (w(Al2O3)=13.00%~14.74%, A/CNK=0.99~1.23) and low TiO2 (w(TiO2)=0.02%~0.18%) and MgO (w(MgO)=0.02%~1.21%), suggesting middle-high K series with peraluminous features. The REE patterns are characterized by weak enrichment of LREE, with moderate-faint Eu negative anomalies (δEu=0.37~0.90). The trace elements show enrichment of Rb, Th, K, Nb, Ta, La, Ce, Nd, Sm and Rb/Sr ratios (9.34~26.81) and depletion of Ba, Sr, Hf and Ta, with the characteristics of S-type granite. Combined with the previous studies, the authors consider that the Ascalt granitic plutons were generated from the partially melting of the upper continental crust dominated by argillaceous rocks at the post-orogenic stage.
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中图分类号:P618.72     
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基金项目:本文得到中国地质调查局区域地质调查项目(编号:1212011120503、1212011120509、DD20160006)资助
引用文本:
张亚峰,蔺新望,赵玉梅,郭岐明,赵端昌,王星,朱伟鹏.2017.新疆北部青河县阿斯喀尔特铍矿区花岗质岩石年代学及地球化学特征[J].矿床地质,36(3):643~658
ZHANG YaFeng,LIN XinWang,ZHAO YuMei,GUO QiMing,ZHAO DuanChang,WANG Xing,ZHU WeiPeng.2017.Geochronology and geochemistry of granitoids of Ascalt beryllium deposit in Qinghe County, northern Xinjiang[J].Mineral Deposits36(3):643~658
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