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首页> 外文期刊>Earthquake Research in China >Preliminary study on paleoearthquake chronology on the northern Liulengshan piedmont fault in Yangyuan, Hebei Province, China
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Preliminary study on paleoearthquake chronology on the northern Liulengshan piedmont fault in Yangyuan, Hebei Province, China

机译:中国河源阳源六棱山山前断裂北部古地震年代学初步研究

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摘要

The northern Liulengshan piedmont fault is located along the southern margin of the Yangyuan basin and represents a dip-slip normal fault, generally NEE-trending and NNW-dipping. Landforms offset by the fault are fairly developed and well preserved in the Dushanpu area of Yangyuan County, Hebei Province. Two trenches were excavated in front of a scarp of the northern Liulengshan piedmont fault at Dushanpu and two paleoseismic events were revealed in the trenches, from which several samples were collected for dating.
机译:六棱山北部的山前断裂带位于阳源盆地的南缘,代表着滑滑正断层,通常为北东向和北北向倾斜。断层抵消的地貌在河北省阳源县独山铺地区较为发达,并得到很好的保存。在独山铺六连山北部山前断裂的陡坡前开挖了两个沟,沟中发现了两个古地震事件,从中收集了一些样品进行测年。

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