MARINE GEOMAGNETIC ANOMALY BELT AND ITS RELATIONSHIP TO THE REMNANT ARCS IN THE NORTHWESTERN JAVA SEA, INDONESIA

D. Kusnida, L. Arifin
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Abstract

The continuous marine geomagneticsurvey within a timeintervalof1-secondsampling and a precision of 0.1 nT was conducted in the northwestern Java Sea to identify and interpret the general trend of total marine magnetic anomalies and the possibility related to thegeological resourcepotential. These magnetic data were then processed according to the formula corrected and applied to marine magnetic data. The total marine magnetic anomalies of the northwestern Java Sea indicate a well-defined lateral trend belt of anomaly contours. Anomalies are divided into four delineation zones: Zones I, II, III, and IV. A preliminary analysis of these anomalies led to the interpretation, reflecting the residual of a slightly east-west trending geological body underneath.Examination of magnetic anomalies suggests Zone I and IV characterize a basinalarea, Zone II depicts a granitic belt, and Zone III describes a Cretaceousmagmatic arc system in the east that extends from Middle Java across the Java SeathroughSouthern Kalimantan. These magnetic anomalies seem to coincide with the free air gravity anomalies data derived from TOPEX satellite data.  
印尼爪哇海西北部海洋地磁异常带及其与残余弧的关系
在爪哇海西北部进行了采样时间间隔为1秒、精度为0.1 nT的连续海洋地磁测量,以识别和解释海洋总磁异常的总趋势及其与地质资源潜力相关的可能性。然后根据修正后的公式对这些磁数据进行处理,并应用于海洋磁数据。爪哇海西北部的海洋总磁异常显示出异常等值线的横向趋势带。异常被划分为4个圈定带:I区、II区、III区和IV区。对这些异常的初步分析导致了解释,反映了下面一个稍微东西走向的地质体的残余。磁异常检查表明,I区和IV区为盆地区,II区为花岗岩带,III区为东部的白垩纪岩浆弧系统,从爪哇中部延伸到爪哇海,穿过加里曼丹南部。这些磁异常似乎与TOPEX卫星数据得出的自由空气重力异常数据相吻合。
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