辽西东南部中生代花岗岩时代

吴福元 杨进辉 张艳斌 柳小明. 辽西东南部中生代花岗岩时代[J]. 岩石学报, 2006, 22(2): 315-325.
引用本文: 吴福元 杨进辉 张艳斌 柳小明. 辽西东南部中生代花岗岩时代[J]. 岩石学报, 2006, 22(2): 315-325.
WU FuYuan , YANG JinHui, ZHANG YanBin and LIU XiaoMing. Emplacement ages of the Mesozoic granites in southeastern part of the Western Liaoning Province[J]. Acta Petrologica Sinica, 2006, 22(2): 315-325.
Citation: WU FuYuan , YANG JinHui, ZHANG YanBin and LIU XiaoMing. Emplacement ages of the Mesozoic granites in southeastern part of the Western Liaoning Province[J]. Acta Petrologica Sinica, 2006, 22(2): 315-325.

辽西东南部中生代花岗岩时代

  • 基金项目:

    国家自然科学基金(40325006,40421202)和中国科学院“百人计划”项目成果,并得到西北大学大陆动力学国家重点实验室资助.

Emplacement ages of the Mesozoic granites in southeastern part of the Western Liaoning Province

  • 辽西东南部是华北地台中生代花岗质岩浆作用较为发育的地区,并产有著名的杨家杖子钼矿床。但关于该区花岗岩的形成时代,一直缺乏深入的研究。本文通过细致的野外考察和系统采样,对该区不同类型的花岗质岩石进行了锆石u—Pb同位素测年。结果显示,该区的碱厂-杨家杖子岩体主体形成于180—190Ma,部分岩石形成于150—160Ma左右。东部海棠山-医巫闾山岩体主要形成于150—170Ma左右。因此,该区的中生代花岗质岩浆作用主要发生在侏罗纪,而白垩纪花岗质岩浆作用相对较弱。同时。这些年代学资料还反映,区内的杨家杖子钼矿形成于中侏罗世,其东部的瓦子峪变质核杂岩形成于早白垩世。对比整个燕辽地区中生代岩浆作用的年代资料发现,该区中生代花岗岩且有自东向西逐渐年轻的趋势,且与火山作用的年代学格架有所不同。岩石中含有的捕获的古老锆石还表明,区内的早前寒武纪岩浆作用主要发生在25和18.5亿年左右。
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出版历程
收稿日期:  2005-10-19
修回日期:  2006-01-16
刊出日期:  2006-02-28

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