大兴安岭中部乌兰浩特地区中生代花岗岩的锆石U-Pb年龄及地质意义

葛文春 吴福元 周长勇 张吉衡. 大兴安岭中部乌兰浩特地区中生代花岗岩的锆石U-Pb年龄及地质意义[J]. 岩石学报, 2005, 21(3): 749-762.
引用本文: 葛文春 吴福元 周长勇 张吉衡. 大兴安岭中部乌兰浩特地区中生代花岗岩的锆石U-Pb年龄及地质意义[J]. 岩石学报, 2005, 21(3): 749-762.
Ge WenChun;Wu FuYuan;Zhou ChangYong;Zhang JiHeng. Zircon U-Pb ages and its significance of the Mesozoic granites in the Wulanhaote region, central Da Hinggan Mountain[J]. Acta Petrologica Sinica, 2005, 21(3): 749-762.
Citation: Ge WenChun;Wu FuYuan;Zhou ChangYong;Zhang JiHeng. Zircon U-Pb ages and its significance of the Mesozoic granites in the Wulanhaote region, central Da Hinggan Mountain[J]. Acta Petrologica Sinica, 2005, 21(3): 749-762.

大兴安岭中部乌兰浩特地区中生代花岗岩的锆石U-Pb年龄及地质意义

  • 基金项目:

    国家自然科学基金(40372038和40325006)、国家油气专项(XQ-2004-07)和西北大学地质学系大陆动力学实验室资助研究成果.

Zircon U-Pb ages and its significance of the Mesozoic granites in the Wulanhaote region, central Da Hinggan Mountain

  • 大兴安岭中生代花岗岩浆作用的时间和期次的确定对讨论东北地区中生代的构造一岩浆演化具有重要意义。本文采用激光ICP—MS技术进行锆石U—Ph年龄测定的结果表明,大兴安岭中部乌兰浩特一索伦地区的中生代花岗岩浆活动可以划分为3期:中-晚三叠世花岗岩岩浆侵位结晶年龄为235~225Ma;早一中侏罗世花岗岩岩浆侵位结晶年龄为182~175Ma;早白垩世花岗岩岩浆侵位结晶年龄为140~125Ma,与该区广泛分布的中生代火山岩时代一致。该区花岗岩的年代学格架与松辽盆地东缘的张广才岭-小兴安岭地区完全可以对比。花岗岩中的捕获锆石具有与额尔古纳地块新元古代花岗岩一致的的年龄信息(~800Ma),反映该区曾经具有前寒武纪结晶基底。结合岩石学特征和邻区的其它地质资料,该区三叠纪花岗岩的形成可能与古亚洲洋闭合造山后的岩石圈伸展体制有关,侏罗纪花岗岩可能是佳木斯地块西缘洋壳俯冲及与松嫩地块拼合作用的产物,而早白垩世花岗岩的形成则与板内拉张性构造体制有关.
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收稿日期:  2005-02-20
修回日期:  2005-02-20
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