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Longling-Lancang fault zone in southwest Yunnan, China - A newly-generated ruptrue zone in continental crust

机译:中国云南西南部的龙陵-澜沧断裂带-大陆壳中的新生代岩浆带

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摘要

the Longling-Lancang fault zone, consisting of sets of en echelon or clustered faults, is a newly-generated rupture zone. It is characterized by the distribution of active faults, earthquake faults and earthquakes in zones. Formed in the Early-Middle Pleistocene, still active in the late, it moves dextrally and extensionally. It tends to cut off the locked segments and discontinuous segments at first, then pervades totally along the zone, accompanied by strong earthquakes.
机译:龙岭—澜沧断层带是由一系列梯形断层或簇状断层组成,是一个新生的破裂带。它的特征是活动断裂,地震断裂和区域地震的分布。它形成于早中更新世,直到后期仍活跃,它在右旋和向外移动。首先,它往往会切断锁定段和不连续段,然后完全沿该区域渗透,并伴有强烈地震。

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