Identifikasi sebaran dan Jenis Sesar Berdasarkan Analisis Data Anomali Gravitasi Topex Provinsi Maluku Utara Lembar Pulau Halmahera Utara

B. A. Sadjab, I. P. Indrayana, Kurnia Kurnia, Khafidh Nur Aziz, A. Nur, Harsen Berg Janis, Hanny F. Sangian
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Abstract

− North Maluku, especially Halmahera Island is part of the framework of Indonesia's complex tectonic system and has a high tectonic activity. This area has the meeting zone of the Eurasia plate, the Pacific plate, the Indo-Australian plate and other small plates such as the Philippine plate. As a result of geodynamics, the research area with high seismic activity is due to many geological structures such as anticlines, synclines, upward faults, horizontal faults and normal faults due to plate activity in this area. One of the methods t hat can be used to identify the faults and their types is the gravity method. this study was using the gravitational observation data of the Topex satellite with an area of 3,891.62 km 2 in the form of Free Air Anomaly (FAA), which is then corrected by bouguers and field correction yields a complete Bouguer Anomaly (ABL). Regional and residual anomalies show the good correlation with the geological map of the study area in delineating the distribution of faults with a range of positive anomalies ± 187 mGal and negative anomalies ± -14.8 mGal. Second Vertical Derivatif (SVD) anomaly analysis shows that the distribution of faults in the study area is a type of normal fault.
−北马鲁古,特别是哈马赫拉岛是印度尼西亚复杂构造体系框架的一部分,构造活动非常活跃。这里有欧亚板块、太平洋板块、印澳板块和菲律宾板块等小板块的交汇带。由于地球动力学的原因,研究区地震活动性高的原因是由于板块活动导致的背斜、向斜、向上断裂、水平断裂和正断层等地质构造。可用于识别断层及其类型的方法之一是重力法。本研究利用Topex卫星3891.62 km2的重力观测数据,以自由空气异常(FAA)的形式,经布格校正,得到完整的布格异常(ABL)。区域异常和残余异常与研究区地质图的断层分布具有较好的相关性,正异常范围为±187 mGal,负异常范围为±14.8 mGal。二次垂直导数(SVD)异常分析表明,研究区内的断层分布属于正断层类型。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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