吉林大学学报(地球科学版) ›› 2017, Vol. 47 ›› Issue (6): 1589-1619.doi: 10.13278/j.cnki.jjuese.201706101
• 地质与资源 • 下一篇
孟恩1, 王朝阳1, 刘超辉1, 施建荣2, 李艳广3
Meng En1, Wang Chaoyang1, Liu Chaohui1, Shi Jianrong2, Li Yanguang3
摘要: 辽东半岛东南部地区出露大面积南辽河群变质表壳岩系,其下部尤以广泛发育变质火山岩为特征。本文通过对黑云斜长片麻岩、斜长角闪岩以及黑云母变粒岩等岩石系统的岩石学、全岩地球化学研究,并结合锆石U-Pb年代学以及Lu-Hf的研究结果来制约其物质组成、原岩形成和变质时代、岩石成因及形成环境,进而探讨胶-辽-吉活动带的大地构造属性。锆石显微结构、微区成分及LA-ICP-MS U-Pb年代学分析结果表明,研究区南辽河群变质火山岩原岩可能形成于2.19 Ga左右,并记录了1.90 Ga左右的变质事件。元素和同位素地球化学分析结果表明,其原岩以玄武安山岩-安山岩和英安岩及少量的流纹岩为主,主体属于亚碱性系列,具有钙碱性演化趋势。其中,基性端元以相对较低的SiO2质量分数,富集MgO、TFe2O3和轻稀土元素(LREE)及Cr、Co和Ni为特征,强烈亏损重稀土元素(HREE)和高场强元素(HFSE,如Nb、Ta和Ti),岩浆应起源于受俯冲流体或熔体交代的亏损岩石圈地幔楔;而中-酸性端元则具有高的SiO2质量分数和较低的MgO、TFe2O3质量分数,富碱,富集Ba、Th、U和K,以及亏损Nb、Ta、P和Ti等特征,应来自于新生地壳物质的部分熔融。结合区域地质资料表明,南辽河群变质火山岩应形成于一个典型的活动大陆边缘的构造环境,暗示胶-辽-吉活动带北段古元古代中期以前的形成演化机制应与弧-陆碰撞作用有关。
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