Study of the Late Quaternary Slip Rate Along the Northern Segment on the South Branch of the Longling-Ruili Fault-中国期刊网

摘要 Longling-Ruili差错是在西南的中国的一个重要活跃差错，向东北通常罢工。差错沿着它在Longling盆，Mangshi盆和Zhefang盆的它的二个方面，以及发展上控制沉积系列和magmatic行动的发展。由于有限第四级的沉积和严厉自然条件，Longling-Ruili差错的北片断上的近来第四级的差错活动正在缺乏的学习和最新的指责的时间并且第四级滑倒率不目前是清楚的。基于遥远的图象的解释，量的geomorphologic变丑大小并且年轻平台存款和冲积扇子，标明日期这份报纸如下获得一些新结果。Longling-Ruili差错的北片断是有正常的某部件的一个Holocene右罢工滑倒差错滑倒。主要在4kaB.P期间形成的冲积存款创作的平台T1。是由Longling-Ruili差错的北片断的偏移量并且它的左侧面并且它的垂直排水量分别地是8m12m和2m。迟了的更新世冲积扇子分别地与70m和18m的左侧面、垂直的排水量被代替。Longling-Ruili差错的罢工滑倒率是2.2mm/a2。5mm/a并且垂直滑倒率是0。6mm/a自从迟了的更新世时代。Longling-Ruili差错的罢工滑倒率是1.8mm/a3.0mm/a并且垂直滑倒率在Holocene时代期间是0.5mm/a。比例对垂直排水量水平是大约4：1，它意味着垂直在Longling-Ruili差错的北片断上滑动率是大约25%水平滑倒率。左侧面在迟了的Holocene滑动率与GPS测量一致。罢工滑倒自从迟了的更新世时代，率具有在不同时间规模的大一致性，显示Longling-Ruili的活动指责稳定性大。

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Study of the Late Quaternary Slip Rate Along the Northern Segment on the South Branch of the Longling-Ruili Fault

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Study of the Late Quaternary Slip Rate Along the Northern Segment on the South Branch of the Longling-Ruili Fault

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