福建晋江中-基性岩墙群的锆石SHRIMP U-Pb定年和岩石地球化学

董传万,张登荣,徐夕生,闫强,竺国强. 福建晋江中-基性岩墙群的锆石SHRIMP U-Pb定年和岩石地球化学[J]. 岩石学报, 2006, 22(6): 1696-1702.
引用本文: 董传万,张登荣,徐夕生,闫强,竺国强. 福建晋江中-基性岩墙群的锆石SHRIMP U-Pb定年和岩石地球化学[J]. 岩石学报, 2006, 22(6): 1696-1702.
DONG ChuanWan~1 ZHANG DengRong~1 XU XiSheng~2 YAN Qiang~1 ZHU GuoQiang~1 1.Department of Earth Sciences,Zhejiang University,Hangzhou 310027,China 2.Department of Earth Sciences,Nanjing University,Nanjing 210093,China. SHRIMP U-Pb Dating and lithogeochemistry of basic-intermediate dike swarms from Jinjiang,Fujian Province.[J]. Acta Petrologica Sinica, 2006, 22(6): 1696-1702.
Citation: DONG ChuanWan~1 ZHANG DengRong~1 XU XiSheng~2 YAN Qiang~1 ZHU GuoQiang~1 1.Department of Earth Sciences,Zhejiang University,Hangzhou 310027,China 2.Department of Earth Sciences,Nanjing University,Nanjing 210093,China. SHRIMP U-Pb Dating and lithogeochemistry of basic-intermediate dike swarms from Jinjiang,Fujian Province.[J]. Acta Petrologica Sinica, 2006, 22(6): 1696-1702.

福建晋江中-基性岩墙群的锆石SHRIMP U-Pb定年和岩石地球化学

  • 基金项目:

    国家自然科学基金(批准号:40372035),国家杰出青年科学基金(批准号:40125007)资助项目成果之一。

  • 福建晋江晚中生代中-基性岩墙群可分为两期:早期岩墙群,岩性为角闪辉绿岩,近东西走向(N70-85E),锆石SHRIMP U-Pb年龄为90±2Ma;晚期岩墙群,岩性为微晶闪长岩,北东走向(N35~50E),锆石SHRIMP U-Pb年龄为87±2Ma。两期岩墙群沿晚中生代花岗片麻岩的节理侵入。在地球化学上,它们具有轻稀土元素和大离子亲石元素富集、高场强元素亏损等特点,I_(Sr)=0.7045~0.7053,ε_(Nd)(t)=-1.18~-1.97,与金门、小金门岛的镁铁质岩墙群相似,也和闽东南晚中生代基性火成岩(辉长岩、玄武岩)的一致。它们是起源于受消减作用影响的岩石圈地幔部分熔融而产生的玄武岩浆,经岩浆分异作用,在拉张的构造环境中侵入形成。
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