浙闽沿海晚中生代伸展构造的岩石学标志: 东极岛镁铁质岩墙群

董传万, 闫强, 张登荣, 杜振永, 竺国强. 浙闽沿海晚中生代伸展构造的岩石学标志: 东极岛镁铁质岩墙群[J]. 岩石学报, 2010, 26(4): 1195-1203.
引用本文: 董传万, 闫强, 张登荣, 杜振永, 竺国强. 浙闽沿海晚中生代伸展构造的岩石学标志: 东极岛镁铁质岩墙群[J]. 岩石学报, 2010, 26(4): 1195-1203.
Dong CW, Yan Q, Zhang DR, Du ZY, Zhu GQ. Late Mesozoic extension in the coastal area of Zhejiang and Fujian provinces: A petrologic indicator from the Dongji Island mafic dike swarms[J]. Acta Petrologica Sinica, 2010, 26(4): 1195-1203.
Citation: Dong CW, Yan Q, Zhang DR, Du ZY, Zhu GQ. Late Mesozoic extension in the coastal area of Zhejiang and Fujian provinces: A petrologic indicator from the Dongji Island mafic dike swarms[J]. Acta Petrologica Sinica, 2010, 26(4): 1195-1203.

浙闽沿海晚中生代伸展构造的岩石学标志: 东极岛镁铁质岩墙群

  • 基金项目:

    国家自然科学基金项目(40872051和40372035)与国家“973”项目(2007CB411706)联合资助

详细信息

Late Mesozoic extension in the coastal area of Zhejiang and Fujian provinces: A petrologic indicator from the Dongji Island mafic dike swarms

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  • 在浙江舟山群岛之东极岛上,出露大规模的镁铁质岩墙群,它们沿晚中生代花岗岩和火山碎屑岩的节理侵位,产状近于直立且与围岩截然接触,指示岩墙岩浆以主动方式沿构造裂隙侵入。东极岛镁铁质岩墙群的岩性主要是角闪辉绿岩,全岩Ar-Ar年龄为93.4Ma。在地球化学上,它们属弱碱性系列,SiO2含量为46.88%~52.55%,CaO 5.40%~7.82%,Al2O3 16.30%~17.31%,TiO2 1.53%~1.18%,(Na2O+K2O)4.62%~6.88%,Mg# = 34~42; 具有轻稀土元素和大离子亲石元素(LILE,如Sr、K、Rb、Ba等)富集、高场强元素(HFSE,如Nb、Ta 等)亏损等特点,它们的ISr为0.7084~0.7098,εNd(t)为-3.21~-8.11,与福建沿海的镁铁质岩墙群及浙闽沿海晚中生代基性岩浆岩(辉长岩/辉绿岩和玄武岩)相似。它们由起源于受消减作用影响的岩石圈地幔部分熔融而产生并受地壳混染的玄武岩浆,在伸展构造环境中形成,是浙闽沿海晚中生代伸展构造的重要岩石学标志。
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出版历程
收稿日期:  2009-09-09
修回日期:  2009-11-08
刊出日期:  2010-04-30

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