吉林大学学报(地球科学版) ›› 2021, Vol. 51 ›› Issue (3): 749-766.doi: 10.13278/j.cnki.jjuese.20200117
田梦宇, 狄永军, 王帅, 贾一龙
Tian Mengyu, Di Yongjun, Wang Shuai, Jia Yilong
摘要： 华南地区印支期经历了强烈的构造运动和岩浆活动，印支期花岗岩的构造背景一直是地学界讨论的热点问题。本文对广西云开地区那蓬黑云母二长花岗岩体进行了详细的锆石年代学、地球化学特征及成因研究。结果显示：那蓬岩体LA-ICP-MS锆石U-Pb年龄加权平均值为（257.8 ±1.2） Ma，结晶年龄为晚二叠世；岩石主量元素具有富钾、富铝质特点，属于钙碱性岩石；微量元素主要富集大离子亲石元素（Rb、Th、U、K、Pb），亏损高场强元素（Nb、Ta、Ti、Zr、Hf）和Ba、Sr元素；稀土元素特征表现为轻稀土元素相对富集，重稀土元素亏损，稀土元素球粒陨石配分曲线呈右倾型，具有较明显轻重稀土分馏特征和负铕异常（δEu=0.41~0.66）。地球化学特征指示了花岗岩的物质来源主要为古老地壳杂砂-泥质源岩部分熔融，构造环境有可能形成于板块碰撞环境的后造山阶段。
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