Penentuan Nilai Parameter Gempabumi Menggunakan Metode Geiger dan Hukum Laska pada Pulau Lombok

Bella Dessy Wulan Sari, Djayus Djayus, S. Supriyanto, Benny Hendrawanto
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Abstract

Earthquake is an event of the Earth vibration caused by the shifting of rock layers on Earth immediately that caused by the shifting of tectonic plates. The aim of this study is to know the Earthquake's Parameter. The Earthquake that happened in Lombok, August 5th 2018, at 18:46:37 (Western Indonesian Time), with magnitude 7,0 SR. By using six Earthquake recording stations, there are KLNI (in Mataram), TWSI (in Sumbawa), SRBI (in Buleleng), DNP (in Denpasar), PLAI (in Plampang) and BYJI (in Banyuwangi). The Coordinate of each Earthquake observer station, P Wave and S Wave are included. The Epicenter value is analyzed using the Laska Law and the Hypocenter value is analyzed using the Geiger Method. The results showed  the Earthquake Parameter with coordinates; Latitude: - 8.28 South; Longitude: 116,47 East, the Epicenter value of KLNI station is 100 km away, the TWSI station is 150 km away, the SRBI station is 300 km away, the DNP station is 300 km away, the PLAI station is 317 km away, the BYJI station is 483 km away and the hypocenter value is 30 km. Deduced from the depth, this Earthquake included into Shallow Earthquake and included as Main Shock or Main Earthquake.
龙目岛使用盖革法和拉斯卡法确定地震参数的价值
地震是由地球上岩层的移动引起的地球振动事件,与构造板块的移动引起的地球振动事件相对应。本研究的目的是了解地震的参数。2018年8月5日18:46:37(印度尼西亚西部时间)发生在龙目岛的地震,震级为7.0级。通过使用六个地震记录站,有KLNI(马塔兰),TWSI(松巴哇),SRBI(布莱伦),DNP(登巴萨),PLAI(普兰邦)和BYJI(班余旺吉)。各地震观测站坐标、纵波和横波均包括在内。震中值用拉斯卡定律分析,震源值用盖革法分析。结果表明:地震参数为坐标形式;纬度:-南纬8.28度;东经116、47,KLNI站震源值为100 km, TWSI站震源值为150 km, SRBI站震源值为300 km, DNP站震源值为300 km, PLAI站震源值为317 km, BYJI站震源值为483 km,震中值为30 km。根据深度推断,本次地震分为浅源地震和主震。
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