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1-D Seismic Velocity Model and Hypocenter Relocation using Double Difference Method around West Papua Region

机译:西巴布亚地区两差法使用双差法的1-D地震速度模型及脱发

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West Papua region has fairly high of seismicity activities due to tectonic setting and many inland faults. In addition, the region has a unique and complex tectonic conditions and this situation lead to high potency of seismic hazard in the region. The precise earthquake hypocenter location is very important, which could provide high quality of earthquake parameter information and the subsurface structure in this region to the society. We conducted 1-D P-wave velocity using earthquake data catalog from BMKG for April, 2009 up to March, 2014 around West Papua region. The obtained 1-D seismic velocity then was used as input for improving hypocenter location using double-difference method. The relocated hypocenter location shows fairly clearly the pattern of intraslab earthquake beneath New Guinea Trench (NGT). The relocated hypocenters related to the inland fault are also observed more focus in location around the fault.
机译:由于构造环境和许多内陆断层,西巴布拉地区具有相当高的地震活动。此外,该地区具有独特而复杂的构造条件,这种情况导致该地区地震危害的高效力。精确的地震效率位置非常重要,这可以为社会提供高质量的地震参数信息和该地区的地下结构。我们使用BMKG的地震数据目录进行了1-D P波速度,从2009年4月到2014年3月,在西巴布亚地区。然后使用获得的1-D地震速度用作使用双差异方法改善低缩小位置的输入。迁移的次级位置相当明显地显示出新的几内亚沟槽(NGT)下面的intraslab地震的模式。还观察到与内陆故障有关的重定位的低缩小器更加焦点在故障周围的位置。

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