吉林大学学报(地球科学版) ›› 2017, Vol. 47 ›› Issue (1): 113-125.doi: 10.13278/j.cnki.jjuese.201701111
齐忠友1, 冯志强2,3, 温泉波2, 张铁安1, 刘宾强2, 李小玉1, 杜兵盈1
Qi Zhongyou1, Feng Zhiqiang2,3, Wen Quanbo2, Zhang Tiean1, Liu Binqiang2, Li Xiaoyu1, Du Bingying1
摘要: 东北兴安地块与松嫩地块的拼贴演化历史一直存在较大争议,而早古生代岩浆记录的发现无疑对该问题的解决具有重要意义。笔者在黑龙江省嫩江依克特地区识别出了早古生代闪长岩体,其LA-ICP-MS锆石U-Pb年龄为(435.3±1.1)Ma,该闪长岩体的SiO2质量分数为55.01%~61.82%,全碱(Na2O+K2O)质量分数为4.55%~6.94%,Na2O/K2O值变化(2.01~48.60)较大,Al2O3质量分数为14.97%~16.67%,具有中等程度的K2O(0.10%~2.12%)、TiO2(0.99%~1.42%)和P2O5(0.33%~0.49%)以及低的TFeO/MgO(0.51~0.96)值,属于中钾钙碱性系列。其A/CNK值为0.78~1.35,A/NK值为1.63~2.21,大体符合I型花岗岩特点。依克特闪长岩的稀土总量较高(w(ΣREE)=227.02×10-6~289.17×10-6),轻重稀土分异明显[(La/Yb)N=9.86~13.93],并具有弱的铕异常(Eu/Eu*=0.88~1.02);具有明显高场强元素(Nb和Ti)亏损的特征。上述特征表明,岩浆源区为受俯冲流体交代地幔楔的部分熔融。结合区域资料,本文认为依克特闪长岩体形成于活动大陆边缘环境,与嫩江-黑河洋的洋壳持续俯冲相关。
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