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Slab tear and tensional fault systems in the Sunda?¢????Andaman Benioff zone: implications on tectonics and potential seismic hazard

机译:da他州安达曼贝尼奥夫地区的板片撕裂和张性断裂系统:对构造和潜在地震危险的影响

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Transverse slab tear faults and longitudinal trench parallel extensional faults present on the top part of Benioff zone in Sunda?¢????Andaman arc between latitude 6???°?¢????15???°N and longitude 90???°?¢????98???°E are marked by seismotectonic analysis using contemporary data related to regional tectonics, seismicity, centroid moment tensor (CMT) fault plane solutions, etc. Characteristics of ten numbers of transverse slab tear faults is taken from our previous studies, whereas four numbers of longitudinal trench parallel extensional faults are marked by the present study. These two sets of fault systems make high angle between them and tectonically complement each other. The disposition, origin, tectonic framework, depth of penetration and seismotectonic evaluations of the fault systems are analyzed. An effort is made to identify the potential seismic hazard in the zone between trench and forearc containing Andaman Group of Island.
机译:Sun达州贝尼奥夫区顶部的横向板片撕裂断层和纵向沟槽平行伸展断层位于北纬6°C至15°C至经度90°之间的安达曼弧利用与区域构造,地震活动性,质心矩张量(CMT)断层平面解等有关的当代数据,通过地震构造分析对°E进行了98°E标记。十个横向平板的特征撕裂断层取自我们先前的研究,而本研究标出了四个纵向沟槽平行伸展断层。这两套故障系统之间形成了很大的角度,并且在构造上相互补充。分析了断层系统的构造,成因,构造框架,穿透深度和地震构造评价。努力确定沟槽和前岛之间的区域中潜在的地震危险,该岛包含安达曼岛。

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