黄子进;付建明;路远发;周洁;卢友月;程顺波;

• 1:长江大学资源与环境学院
• 2:中国地质调查局武汉地质调查中心
• 3:中国地质调查局花岗岩成岩成矿地质研究中心

摘要(Abstract)：

五团岩体位于南岭地区西段,主要岩性为黑云母二长花岗岩。利用LA-ICP-MS微区原位测试技术,对五团岩体黑云母二长花岗岩进行了锆石U-Pb定年及CL显微结构分析。结果表明:2件锆石样品的~(206)Pb/~(238)U加权平均年龄分别为(211±0.95)Ma(MSWD=0.08)和(227±3.2)Ma(MSWD=1.9),结合前人获得的年龄数据,认为岩体形成于晚三叠世中期且具有多次侵位;岩石具高硅、富铝、高钾特征,w(SiO_2)70.54%~72.55%,平均71.67%;w(Al_2O_3)13.62%~14.55%,平均14.03%;w(K_2O)4.18%~5.28%,平均4.85%;全碱(Na_2O+K_2O)7.09%~7.89%,平均7.51%;K_2O/Na_2O比值1.44~4.51,平均2.02;总体属铁质、高钾钙碱性-钾玄岩系列过铝质花岗岩类;Ba、Nb、Sr、P、Ti表现为明显亏损,Rb、Th、U、K、La、Ce、Nd、Zr、Hf、Sm、Y、Yb、Lu等则相对富集,w(∑REE)62.07×10~(-6)~149.58×10~(-6),平均126.68×10~(-6),δEu值0.26~0.50,地球化学特征表明花岗岩为S型花岗岩,源岩主要为中、上地壳变质杂砂岩;花岗岩微量元素构造环境判别图解主要显示为后碰撞构造环境。基于岩石成因、构造环境判别以及区域构造演化过程,推断五团岩体形成于印支晚期后碰撞环境,是加厚地壳在碰撞应力减弱、深部压力降低等条件下部分熔融的产物。

关键词(KeyWords)： 锆石LA-ICP-MS U-Pb年龄;地球化学特征;印支期;五团岩体;南岭地区

Abstract:

Keywords:

基金项目(Foundation): 中国地质调查局地质矿产调查评价专项项目“南岭成矿带资源远景调查评价”(12120114084501);“南岭成矿带中西段地质矿产调查”(121201009000150002)

作者(Author): 黄子进;付建明;路远发;周洁;卢友月;程顺波;

Email:

DOI:

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