Distribution of subsurface anomalies in the Muria Peninsula and depth analysis with euler deconvolution

R. Indriana
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Abstract

Muria Peninsula is one of the regions in Central Java that is uniquely formed. The Muria Peninsula was originally separated from Java and is now connected. To complement the studies that have been done before, subsurface analysis using euler deconvolution method is carried out. Gravity data used is satellite data provided free by BGI. The results of the processing produced a residual anomaly which showed a fault that passed in the middle of the peak of Muria towards Mount Genuk. The anomaly depth of Mt. Muria is 1000 m to 2000 m, in the peak area of Muria and Genuk <1000 m, and in the east and west of the study area the anomaly depth is more than 2000 m. Euler deconvolution index 0 illustrates the body boundaries of Mt. Muria and Genuk in the form of dike and steep.
穆里亚半岛地下异常分布及欧拉反褶积深度分析
穆里亚半岛是中爪哇形成独特的地区之一。穆里亚半岛最初是从爪哇分离出来的,现在是相连的。为了补充之前所做的研究,使用欧拉反褶积方法进行了地下分析。重力数据为华大基因免费提供的卫星数据。处理的结果产生了一个残余异常,显示了一条断层从穆里亚峰的中间向格努克山穿过。Muria山异常深度为1000 ~ 2000 m, Muria和Genuk峰区异常深度<1000 m,研究区东部和西部异常深度均大于2000 m。欧拉反褶积指数0以堤防和陡坡的形式说明了穆里亚山和格努克山的体界。
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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