贵州南部地区安尼阶底界锆石SHRIMP年龄结果
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国家科技攻关计划


Zircon U-Pb Dating for the lower-middle Triassic tuff in Wangmo,Guizhou province
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    摘要:

    中国西南地区中下三叠统广泛发育多层凝灰岩,贵州望谟甘河桥剖面安尼阶底界,即中/下三叠统界线位于火山凝灰岩之下0.5m处为国际上奥伦尼克阶/安尼阶(Olenekian-Anisian)界线层型牙形石划分标志Chiosella timorensis首现的位置。从火山凝灰岩分离出20颗岩浆成因锆石的SHRIMP年龄测定,获得206Pb/238U加权平均年龄为247.6±1.7 (95% conf.) or ±1.4 (2σ) Ma,此结果与贵州关刀剖面Olenekian-Anisian界线附近凝灰岩用TIMS方法得出的247.2Ma±0.1Ma年龄有很好的一致性。望谟甘河桥剖面中下三叠统界线凝灰岩在华南地区大面积分布,本文的结果为区域地层对比和划分提供了新的年龄数据,同时为研究三叠纪初期生物复苏时限提供了新的年龄参考。

    Abstract:

    New zircon U-Pb age are obtained for late Early and Middle Triassic tuff layer from the Ganheqiao section, Wangmo country, Guizhou province. The first appearance of conodont Chiosella timorensis was discovered just 0.5m below the tuff, which is used to define the Olenekian-Anisian boundary in the lower/middle Triassic. Twenty zircons defined a weighted mean 206Pb/238U age of 247.6± 1.4 Ma (2σ). The new dates are in better agreement with a 247.2Ma age obtained from the Guandao section of Guizhou province, which were identified using TIMS method and were proposed for the boundary age of Olenekian-Anisian. The tuff layer found in the Ganheqiao section is wide distributed in southwest China. Our result defines a new dating for the regional stratigraphic correlation, and also provides a reliable dating for the duration of biological recovery in the early Triassic after the extinction of Permo-Triassic.

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杨振宇.2010.贵州南部地区安尼阶底界锆石SHRIMP年龄结果[J].地质学报,84(8):1112-1117.
Yang Zhenyu.2010. Zircon U-Pb Dating for the lower-middle Triassic tuff in Wangmo,Guizhou province[J]. Acta Geologica Sinica,84(8):1112-1117.

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  • 收稿日期:2010-03-29
  • 最后修改日期:2010-04-30
  • 录用日期:2010-05-27
  • 在线发布日期: 2010-07-28
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