许汉森;黄建桦;李宏卫;林小明;

• 1:广东省地质调查院

摘要(Abstract)：

对粤东北新丰地区基性岩脉进行了年代学、元素地球化学研究。结果表明:新丰地区近SN向和NWW向基性岩脉的锆石U-Pb年龄分别为(148.6±4.1)Ma(MSWD=1.3)和(85.7±2.0)Ma(MSWD=1.4),成岩时代为晚侏罗世和晚白垩世。基性岩脉具低碱富钠、较高钛含量、富铁、中等镁含量和准铝质特征。稀土元素标准化曲线呈小角度右倾斜型,轻重稀土元素中等分馏、轻稀土元素富集。微量元素表现出富集Ba、Rb、K,亏损Ta、Nb、Zr、Hf和P等特征。晚侏罗世基性岩脉轻微Ce负异常(δCe=0.89~0.93)和弱Eu正异常(δEu=1.00~1.05),Th/Yb比值比较高,表明岩浆源区可能遭受过富Th俯冲流体交代。2组基性岩脉岩浆源区均来自地幔,可能经历了石榴石-尖晶石二辉橄榄岩的部分熔融,并发生了单斜辉石、Ti-Fe氧化物矿物的分离结晶作用。新丰地区基性岩脉具有大陆裂谷玄武岩特征,形成于陆内裂谷环境,但早期基性岩脉(148.6 Ma)较晚期(85.7 Ma)具有相对较浅的岩浆源区。

关键词(KeyWords)： 粤东北;基性岩脉;年代学;地球化学

Abstract:

Keywords:

基金项目(Foundation): 中国地质调查局项目“广东1∶5万周陂公社、隆街公社、新丰县、马头等四幅区域地质矿产调查”(12120113063100)

作者(Author): 许汉森;黄建桦;李宏卫;林小明;

Email:

DOI: 10.19509/j.cnki.dzkq.2018.0302

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