苏鲁超高压带北部中生代岩浆侵入活动与同碰撞—碰撞后构造过程:锆石U-Pb年代学

郭敬辉 陈福坤 张晓曼 Siebel W  翟明国. 苏鲁超高压带北部中生代岩浆侵入活动与同碰撞—碰撞后构造过程:锆石U-Pb年代学[J]. 岩石学报, 2005, 21(4): 1281-1301.
引用本文: 郭敬辉 陈福坤 张晓曼 Siebel W  翟明国. 苏鲁超高压带北部中生代岩浆侵入活动与同碰撞—碰撞后构造过程:锆石U-Pb年代学[J]. 岩石学报, 2005, 21(4): 1281-1301.
GUO JingHui~1 CHEN FuKun~1 SIEBEL W~2 ZHAI MingGuo~11.State Key Laboratory of Lithospheric Evolution,Institute of Geology and Geophysics,CAS,Beijing 100029,China2.Institut fuer Geochemie,Universitaet Tuebingen,Tuebingen 72074,Germany. Evolution of syn- to post-collisional magmatism from north Sulu UHP belt, eastern China: zircon U-Pb geochronology[J]. Acta Petrologica Sinica, 2005, 21(4): 1281-1301.
Citation: GUO JingHui~1 CHEN FuKun~1 SIEBEL W~2 ZHAI MingGuo~11.State Key Laboratory of Lithospheric Evolution,Institute of Geology and Geophysics,CAS,Beijing 100029,China2.Institut fuer Geochemie,Universitaet Tuebingen,Tuebingen 72074,Germany. Evolution of syn- to post-collisional magmatism from north Sulu UHP belt, eastern China: zircon U-Pb geochronology[J]. Acta Petrologica Sinica, 2005, 21(4): 1281-1301.

苏鲁超高压带北部中生代岩浆侵入活动与同碰撞—碰撞后构造过程:锆石U-Pb年代学

  • 基金项目:

    本研究由国家重点基础研究发展规划项目(G1999075502)和中国科学院重大创新项目(KZCX1-07)共同资助.本研究由国家重点基础研究发展规划项目(G1999075502)、中国科学院重大创新项目(KZCX1-07)和NSFC与DFG的中德合作项目资助.作者真诚感谢刘敦一研究员、万渝生和宋彪研究员等在SHRIMPⅡ测试方面的全面支持,感谢彭澎、刘富、钱青和范宏瑞的大力协助.

Evolution of syn- to post-collisional magmatism from north Sulu UHP belt, eastern China: zircon U-Pb geochronology

  • 苏鲁超高压变质带北部威海地区发育大量中生代侵入体。本文报道了新的同位素稀释法和 SHRIMP 锆石 U-Pb 同位素年龄数据,确认该区中生代侵入岩浆活动主要有三期,分别是三叠纪晚期~210Ma,侏罗纪晚期160~140Ma 和白垩纪早期~110Ma。三叠纪晚期主要是橄榄安粗岩系列的侵入体,包括邢家碱性辉长岩(211±5Ma 和213±5Ma),甲子山辉石正长岩(211.9±1.5Ma 和209.0±6.5Ma),槎山正长花岗岩(205.7±1.4Ma),它们的形成可能指示深俯冲大陆的板片断离作用。侏罗纪晚期主要有垛崮山花岗闪长岩体(161±1Ma),文登花岗岩体(160±3Ma)和昆嵛山花岗岩体(142±3Ma)。大量700~800Ma 的继承锆石指示这些花岗岩是俯冲的扬子板块部分熔融的产物,它们可能起因于碰撞加厚地壳的拆沉作用。白垩纪早期的侵入体代表性的有六度寺辉石闪长岩(114.5±0.8Ma),秦薄顶钾长巨斑状花岗岩(114±1Ma),三佛山钾长斑状花岗岩(113±1Ma)和伟德山花岗岩(108±2Ma)。这些高钾钙碱系列侵入体,是中国东部普遍发育的岩石圈减薄过程中强烈的壳幔相互作用的产物。
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收稿日期:  2005-05-30
刊出日期:  2005-07-31

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