| 谈谈浑河断裂带的新构造 |
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| 引用本文： | 何恃松.谈谈浑河断裂带的新构造[J].地震地质,1981,3(2):65. |
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| 作者姓名： | 何恃松 |
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| 作者单位： | 辽宁省冶金地质勘探公司研究所 |
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| 摘 要： | 浑河断裂带在前震旦纪就开始活动,中生代时期活动剧烈,至第三纪和第四纪初、浑河断裂带的构造活动更为频繁强烈。本文主要讨论浑河断裂带自沈阳至清原县草市地段从第三纪以来的新构造活动的一些形迹
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| 关 键 词： | 浑河断裂 新构造活动 逆断层 抚顺群 清原县 断裂带 构造运动 深震 浅震 鞍山群 |
ON NEOTECTONICS OF THE HUNHE FAULT ZONE |
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| Abstract: | The Hunhe fault zone is a western extension of the Shenyang-Dunhua Mishan fault and there can be found an evidence of Pre-Sinian movement. It is suggested that the faulting of Hunhe fault zone was significant in Mesozoic time and more intensive and frequent in Tertiary and Quaternary.Basing upon the data on geology, morphology and seismicity. this paper illustrates the trace of the neotectonic movement since Tertiary.Actually this fault acts as one of main faults of Cathaysian tectonic system |
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