辽西新太古代钓鱼台花岗岩成因及演化过程:来自岩石组构的证据

张媛媛, 蔡丽斌, 金巍, 刘婷, 郑培玺, 李婧. 辽西新太古代钓鱼台花岗岩成因及演化过程:来自岩石组构的证据[J]. 岩石学报, 2016, 32(9): 2867-2880.
引用本文: 张媛媛, 蔡丽斌, 金巍, 刘婷, 郑培玺, 李婧. 辽西新太古代钓鱼台花岗岩成因及演化过程:来自岩石组构的证据[J]. 岩石学报, 2016, 32(9): 2867-2880.
ZHANG YuanYuan, CAI LiBin, JIN Wei, LIU Ting, ZHENG PeiXi, LI Jing. The petrogenesis and evolutionary process of Neoarchean Diaoyutai granite in western Liaoning Province: Evidences from petrofabric[J]. Acta Petrologica Sinica, 2016, 32(9): 2867-2880.
Citation: ZHANG YuanYuan, CAI LiBin, JIN Wei, LIU Ting, ZHENG PeiXi, LI Jing. The petrogenesis and evolutionary process of Neoarchean Diaoyutai granite in western Liaoning Province: Evidences from petrofabric[J]. Acta Petrologica Sinica, 2016, 32(9): 2867-2880.

辽西新太古代钓鱼台花岗岩成因及演化过程:来自岩石组构的证据

  • 基金项目:

    本文受国家自然科学基金项目(41172170、41230206)和岩石圈演化国家重点实验室开放课题联合资助.

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The petrogenesis and evolutionary process of Neoarchean Diaoyutai granite in western Liaoning Province: Evidences from petrofabric

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  • 辽西兴城钓鱼台地区分布一套花岗质杂岩,是新太古代“绥中花岗岩”的重要组成部分。花岗质杂岩以似斑状花岗闪长岩和石英闪长岩为主,少量细粒黑云闪长岩(包体)及脉状花岗岩,各类岩石接触关系明确,本文定义为“钓鱼台花岗岩”。锆石U-Pb同位素测试结果显示似斑状花岗闪长岩、石英闪长岩、脉状花岗岩的形成年龄分别为2538±20Ma、2476±56Ma、2470±18Ma,同为新太古代末期热事件的产物。通过该花岗岩组合的宏观-微观组构解析表明,似斑状花岗闪长岩表现为均匀块状构造,具有深熔花岗质岩浆的典型堆晶结构;细粒黑云闪长岩为细粒结构,呈小型暗色包体分布在似斑状花岗闪长岩中,包体的塑性变形、捕掳晶、淬冷边及反向脉等组构发育,具有铁镁质基性岩浆加入同深熔花岗闪长岩并快速冷却的特征;暗色的石英闪长岩主要分布在似斑状花岗闪长岩之下,接触带附近似斑状花岗闪长岩中的钾长石变斑晶明显增多,显示闪长质岩浆“底垫”侵位加热的特征;脉状花岗岩同时穿切似斑状花岗闪长岩和石英闪长岩,具有熔体富集脉体的结构特征。各类岩石中变形组构均不发育。钓鱼台花岗岩记录了新太古代末期地壳深熔和壳幔相互作用过程,岩石组构研究表明新太古代地壳再造作用是一个“静态”多期次的缓慢深熔过程,伴有同期幔源基性物质加入并混合,以及随后大规模的基性岩浆底侵。由此推断钓鱼台花岗岩形成的构造背景为幔源岩浆垂向底侵过程,可能是与俯冲带关联不明显的岩浆弧环境。
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收稿日期:  2016-04-21
修回日期:  2016-07-30
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