吉林大学学报(地球科学版) ›› 2016, Vol. 46 ›› Issue (6): 1754-1768.doi: 10.13278/j.cnki.jjuese.201606113
尹继元1,2, 陈文1, 肖文交2, 罗勇3, 张斌1, 杨莉1, 喻顺1, 徐翠4
Yin Jiyuan1,2, Chen Wen1, Xiao Wenjiao2, Luo Yong3, Zhang Bin1, Yang Li1, Yu Shun1, Xu Cui4
摘要： 西准噶尔包古图地区发育一些小型的闪长质岩体。前人对这些小岩体开展了岩石学、年代学和地球化学等研究，然而，其成因机制和构造背景仍然存在争议，阻碍了区域构造演化和成矿作用的认识。本文在前人研究的基础上，选择包古图I号岩体为研究对象，有望揭示包古图岩体的岩石成因和构造背景。锆石U-Pb年代学研究显示，包古图I号岩体形成于（313.8±1.1）Ma。包古图I号闪长岩体以富SiO2（58.0%~59.0%）、Al2O3（16.6%~17.4%）和Sr（757×10-6~882×10-6），低的Y（14.6×10-6~15.7×10-6）和Yb（1.51×0-6~1.60×0-6）质量分数为特征，具有高的Sr/Y（50~59）值和弱的Eu异常，类似于俯冲成因的埃达克岩。另外，这些闪长岩具有较高的Mg（w（MgO）=3.46%~3.77%，Mg#=52.8~53.2），高的Cr（63.8×10-6~74.7×10-6）和Ni（45.2×10-6~49.8×10-6）质量分数，亏损HFSE（Nb，Ta和Ti）。该闪长质岩体可能由俯冲的板片熔体与上覆地幔相互作用而成。它的形成可能与西准噶尔地区晚石炭世的洋脊俯冲作用有关。
中图分类号:
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