1) Changdi fault belt
长堤断裂带
1.
Control factors of remaining oil distribution and potential exploitation measures in the northern part of Changdi fault belt;
长堤断裂带北部地区剩余油控制因素与挖潜对策
2) Changyuan Defaults belt
长垣断裂带
3) Changzhao fault zone
长诏断裂带
1.
Preliminary study on the relation between vertical deformation and earthquake in Changzhao fault zone;
长诏断裂带垂直运动与地震关系初探
4) structural belt of the Yangtze River
长江断裂带
5) Lintong-Chang an fault zone
临潼-长安断裂带
1.
The Lintong-Chang an fault zone consists of two main faults and two branch faults.
临潼-长安断裂带主要由两条主断层和两条分支断层组成,断层基本沿北东向的黄土塬陡坎展布,陡坎高30~128m不等。
2.
Our results suggest that these four paleoearthquake events have relation with the activity of Lintong-Chang an fault zone which is then believed to have no strong seismic risk.
根据探槽中地层没有明显错动和临潼-长安断裂带在晚更新世晚期和全新世早期活动较弱,以及历史上无6级以上地震活动记录的特点,本文认为4次古地震事件与临潼-长安断裂带无关,该断裂未来发生强震的危险性不大。
6) Changliu-Xiangou fault zone
长流-仙沟断裂带
1.
The Holocene volcanic activity of the Leihuling Group are distributed mainly along the Changliu-Xiangou fault zone in the Shishan-Yongxing area Many large-scale faults are found in the base-surge deposits which are created by phreatomagmatic eruptions in Shishan area.
琼北地区的火山活动以裂隙喷溢为主,晚更新世道堂期的射气岩浆喷发形成了众多的低平火山口,全新世雷虎岭期火山口主要分布于石山、永兴一带,沿NW向长流-仙沟断裂带分布。
补充资料：长堤风貌街
长堤风貌街
位于美丽的蓬江河畔，全长0.8千米，是江门市老商业区和历史街区。这里的商铺几乎是独具岭南特色的“骑楼”建筑群，充满了浓厚的文化氛围和内涵。街内有江门国际青年旅馆、高档的酒吧啡厅以及旅游购物商店等。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。