大别山岳西县石关混合岩锆石SHRIMP定年及其地质意义
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国家自然科学基金项目(面上项目,重点项目,重大项目)


SHRIMP U-Pb dating and Geological Gignificance of Migmatite in Shiguan of Yuexi County, Dabie Mountains
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    摘要:

    岳西县石关混合岩属于原北大别变质杂岩的一部分。锆石SHRIMP U-Pb定年结果:第一次变质时间为232 Ma,相当于晚三叠世早期,第二次变质时间为207Ma,相当于晚三叠世晚期。复合锆石的核部(继承锆石),为发育韵律环带的岩浆碎屑锆石,其年龄值分别为560、444、394、378和331Ma,暗示其原岩非岩浆岩,而应为沉积岩;研究结果还表明,北大别石关混合岩经历了两次变质作用:1)超高压变质作用,变质时间为232 Ma(n=5加权平均年龄);2)退变质作用,时间为207Ma。与苏鲁地区超高压变质和退变质时间一致。

    Abstract:

    Shiguan migmatite of Yuexi County, belong to the part of former North Dabie Complex. The result of zircon SHRIMP U-Pb dating shows: the first time of metamorphism is 232Ma, equivalent to early period of Late Triassic, and the second time of metamorphic is 207Ma, equivalent to late period of Late Triassic., There are prosodic clitellum in Composite core of zircon (inherited zircon) ,and that’s detrital zircons from the magma, the age value of 560、444、394、378 and 331Ma respectively. These phenomena suggest that the original rock is not magmatic rocks, but sedimentary rocks. Research findings also showed that the Shiguan migmatite of the North Dabie has gone through two times of metamorphism: 1) ultra-high pressure metamorphism, the time of 232 Ma (n = 5, mean age); 2) retrograde metamorphism, the time of 207Ma. the time of the two times of metamorphism is consistent to time of ultrahigh-pressure metamorphic and retrograde metamorphism in Sulu region.

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夏斌,蔡周荣,张玉泉,李建峰,吴维平,杨之青,董春艳,王洪,刘立文.2010.大别山岳西县石关混合岩锆石SHRIMP定年及其地质意义[J].地质学报,84(2):206-210.
XIA Bin, CAI Zhourong, ZHANG Yuquan, LI Jianfeng, WU Weiping, YANG Zhiqing, DONG Chunyan, WANG Hong, LIU Liwen.2010. SHRIMP U-Pb dating and Geological Gignificance of Migmatite in Shiguan of Yuexi County, Dabie Mountains[J]. Acta Geologica Sinica,84(2):206-210.

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  • 收稿日期:2009-03-04
  • 最后修改日期:2009-08-07
  • 录用日期:2009-08-25
  • 在线发布日期: 2010-01-08
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