吉林大学学报(地球科学版) ›› 2018, Vol. 48 ›› Issue (1): 145-164.doi: 10.13278/j.cnki.jjuese.20170229
孙凡婷1,2, 刘晨3, 邱殿明4, 鲁倩5, 贺云鹏5, 张铭杰1
Sun Fanting1,2, Liu Chen3, Qiu Dianming4, Lu Qian5, He Yunpeng5, Zhang Mingjie1
摘要: 大兴安岭地区以发育显生宙花岗岩和火山岩为特征,基性和中性侵入岩不是十分发育,仅在塔河、塔源、富西里、乌拉山、碧流台等地有所报道,且规模相对较小,它们在形成时代和成因上的差别为我们深入揭示大兴安岭地区壳幔过程提供了重要依据和线索。近期我们在大兴安岭东坡北部红花尔基地区开展了基础地质调查,在小奎勒河中游花岗杂岩体内部发现并确定了两处不规则中基性岩体,经系统的岩相学、年代学、元素和Hf同位素地球化学研究揭示:两处中基性岩体由细粒角闪辉长岩岩相和辉长闪长岩岩相构成; LA-ICP-MS单颗粒锆石U-Pb同位素定年结果显示,其成岩作用于310~293 Ma;岩石系列为准铝质、钾质-钠质、拉斑玄武质-钙碱性过渡岩系;初始岩浆为来自熔体-流体交代作用的富集地幔低程度(<5%)部分熔融作用,源区主要残留矿物相为辉石和石榴石、钙钛矿等;岩浆演化过程以结晶分离作用为主,伴随堆晶作用;形成于松嫩地块-兴安地块碰撞拼合晚期向初始大洋岛晚期大洋弧初始环境。
中图分类号:
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