新疆库鲁克塔格阿訇开里得南石炭纪花岗岩LA-ICP-MS锆石U-Pb定年及其地质意义  

Zircon LA-ICP-MS U-Pb dating of South Ahongkailide Carbonifereous granite in Kuruktag of Xinjiang and its geological implications

作　　者：尼加提.阿布都逊 郭瑞清[1] 帕拉提.阿布都卡迪尔 贾晓亮[1] 秦切[1] 朱志新[1,3] 王克卓 

机构地区：[1]新疆大学地质与勘查工程学院,新疆乌鲁木齐830046 [2]新疆维吾尔自治区商务厅,新疆乌鲁木齐830046 [3]新疆维吾尔自治区地质调查院,新疆乌鲁木齐830011

出　　处：《地质通报》2013年第2期251-259,共9页Geological Bulletin of China

基　　金：中国地质调查局项目《兴蒙造山带基本构造格局综合调查和研究》(编号:1212011085476);《天山成矿带地质矿产调查评价》(编号:1212011120477)

摘　　要：对出露于新疆库鲁克塔格地块西段的阿訇开里得南花岗岩进行了详细的岩石学、地球化学及锆石U-Pb定年研究,并探讨了其构造背景及地质意义。岩体LA-ICP-MS锆石U-Pb原位定年获得年龄为340.6Ma±5.7Ma,属于石炭纪花岗岩。地球化学分析显示岩体具高硅、高铝、高钾,贫钠、低钙、低磷、低钛和贫镁的特征,铝饱和指数(A/CNK)为1.14-2.31,CIPW标准刚玉分子大于1%,属高钾钙碱性过铝质花岗岩。在稀土元素球粒陨石标准化配分模式图上,轻稀土元素(LREE)富集、重稀土元素(HREE)亏损,轻重稀土元素分馏明显,Eu出现中等负异常(δEu=0.52-0.62);在微量元素原始地幔标准化蛛网图上,明显富集大离子亲石元素Rb、Ba、Th和K,亏损高场强元素Nb、Ta、Ti。综合分析研究认为,岩体的形成与加厚地壳引起的地壳重熔有关,反映了塔里木板块与伊犁-中天山板块陆-陆碰撞的岩浆活动。The South Ahongkailide Carboniferous granite is exposed in the west segment of Kuruktag block in Xinjiang. This paper has studied petrographical, geochemical and zircon U-Pb chronolgical characteristics of this granite as well as its petrogenesis and geological significance. Zircon LA-ICP-MS dating yielded the age of 340.6Ma±5.7Ma, implying that the magmatic crystallization epoch of the granite is Carboniferous. Geochemical analyses show that the granite has high SiO2, Al2O3, K2O but relatively low CaO, P2O5, TiO2 and MgO. The ratios of A/CNK vary from 1.14 to 2.31, suggesting high-K calc-alkaline peraluminous syn-collision granite. The chondrite-normalized KEE patterns show that the granite is enriched in LKEE but depleted in HKEE, with high fractionations between LKEE and HREE and moderate negative Eu anomalies （（δEu=0.52-0.62）. In addition, the granite is relatively rich in such LILEs as Rb,Ba,Th and K, but poor in such HFSEs as Nb, Ta and Ti, with relative enrichment of Ce in the primitive mande-nor- mafized trace elements patterns. The authors have come to the conclusion that the formation of the granite was closely related to crustal partial melting caused by crustal thickening and represented the magmatic activities during the collisional event between Tarim plate and Yili-Central Tianshan plate.

关 键 词：过铝质花岗岩 地球化学 U-Pb锆石定年 库鲁克塔格 

分 类 号：P534.44[天文地球—古生物学与地层学]