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Tectonics Earthquake Distribution Pattern Analysis Based Focal Mechanisms (Case Study Sulawesi Island, 1993-2012)

机译:构造基于地震分布模式分析的焦点机制(凯拉威西岛,1993-2012)

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Indonesia is the meeting zone between three world main plates: Eurasian Plate, Pacific Plate, and Indo-Australia Plate. Therefore, Indonesia has a high seismicity degree. Sulawesi is one of whose high seismicity level. The earthquake centre lies in fault zone so the earthquake data gives tectonic visualization in a certain place. This research purpose is to identify Sulawesi tectonic model by using earthquake data from 1993 to 2012. Data used in this research is the earthquake data which consist of: the origin time, the epicenter coordinate, the depth, the magnitude and the fault parameter (strike, dip and slip). The result of research shows that there are a lot of active structures as a reason of the earthquake in Sulawesi. The active structures are Walannae Fault, Lawanopo Fault, Matano Fault, Palu - Koro Fault, Batui Fault and Moluccas Sea Double Subduction. The focal mechanism also shows that Walannae Fault, Batui Fault and Moluccas Sea Double Subduction are kind of reverse fault. While Lawanopo Fault, Matano Fault and Palu - Koro Fault are kind of strike slip fault.
机译:印度尼西亚是三名世界主要印第摩莱之间的会议区:欧亚板块,太平洋板材和印度 - 澳大利亚板块。因此,印度尼西亚具有高地震性程度。苏拉威西是其中一种高震作率。地震中心位于故障区域,因此地震数据在某个地方提供了构造可视化。这种研究目的是通过使用1993年至2012年的地震数据来识别Sulawesi构造模型。本研究中使用的数据是由:原始时间,震中坐标,深度,幅度和故障参数组成的地震数据(罢工,蘸和滑动)。研究结果表明,有很多活跃的结构是苏拉威病的地震的原因。活跃的结构是瓦南缺陷,拉曼多,马塔诺故障,Palu - Koro断层,巴杜伊故障和Moluccas双俯冲。焦点机制还表明,瓦南缺陷,巴杜伊故障和Moluccas海双俯度是逆转故障。虽然拉美奥波奥断层,Matano Fault和Palu - Koro Fauft是罢工滑倒故障。

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