The age of Xiannu Mountain fracture belt in Three-Gorge region -a fission track study

Zhang Feng; Lin Wenzhu; Zhou Jiyi

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The age of Xiannu Mountain fracture belt in Three-Gorge region -a fission track study

机译：三峡地区仙女山断裂带年龄-裂变径迹研究

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Apatite was separated from fault-clay, fracture-cliff rock and fracture wall rock, which were collected from Huangkou fracture north to Xiannu Mountain lying 20 km southwest to Three Gorge Dam Project-Sandouping dam. The fission tract characters and their length variations of Apatite show that Xiannu Mountain fracture belt was formed at(0.7±0.04)Ma, but its wall rock At(25.31±2.8)Ma. this result and previous studies show that no activity has happened since The Holocene, and the Three Gorges Dam Project is not affected by activity of the Xiannu Moun- Tain fracture belt.

机译：磷灰石与断层粘土，裂隙悬崖岩石和裂隙壁岩石分离，这些岩石从黄口断裂北至仙姑山西南20公里处的三女坝—三斗坪大坝采集。磷灰石的裂变特征及其长度变化表明仙女山断裂带形成于（0.7±0.04）Ma，而围岩形成于（25.31±2.8）Ma。这个结果和以前的研究表明，自全新世以来没有活动，而且三峡大坝工程不受仙女山-泰因断裂带活动的影响。

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《Chinese science bulletin》 |1999年第8期|p.744-747|共4页
作者
Zhang Feng; Lin Wenzhu; Zhou Jiyi;
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正文语种 eng
中图分类自然科学现状及发展;
关键词
fission track; Xiannu Mountain fracture belt; apatite;

机译：裂变径迹仙女山断裂带;磷灰石;

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The age of Xiannu Mountain fracture belt in Three-Gorge region -a fission track study

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