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磷灰石裂变径迹年龄分析三峡仙女山断裂带构造活动性

DISCUSSION ON ACTIVITY OF XIANNUSHAN FAULT BELTS IN THE THREE-GORGES AREA IN TERMS OF FISSION-TRACKING AGE OF APATITE

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【作者】 张峰林文祝

【Author】 Zhang Feng Lin Wenzhu (The State Key Laboratory of Environment Geochemistry, Institute of Geochemistry, Chinese Academy of Science, Guiyang, 550002)

【机构】 中国科学院地球化学研究所环境地球化学国家重点实验室!贵阳550002

【摘要】 用磷灰石的裂变径迹年龄及径迹长度变化规律 ,证实仙女山断裂带发生断裂的时期为距今 0 .7Ma左右 ;从讨论的各种绝对年龄结果分析 ,均未见到全新世以来有明显的活动迹象 ,以此确定仙女山断裂的活动性对三峡枢纽工程并不构成威胁

【Abstract】 In terms of the fission tracking age of apatite and the changing trend of length of tracks, it was verified that the Xiannushan fault belt was formed at about 0.70 Ma B.P. From the analysis of the results of different absolute ages it is also found that there was no obvious tectonic activity since Holocene. The conclusion can be drawn that the tectonic activity of the Xiannushan fault belt will not endanger the Three Gorges projects.

【基金】 国家自然科学基金!(批准号 :4 9673 1 96)资助项目
  • 【文献出处】 矿物学报 ,Acta Mineralogica Sinica , 编辑部邮箱 ,1999年01期
  • 【分类号】P542.3
  • 【被引频次】1
  • 【下载频次】145
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