磁资料的二维反演以满足布拉、PRELUME的碳氢化合物安全性

JGE Pub Date : 2020-01-17 DOI:10.23960/JGE.V4I3.1071
Elen Novia Limswipin, Syamsurijal Rasimeng, Karyanto Karyanto, Noor Muhammad Indragiri
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引用次数: 0

摘要

已经进行了一项区域研究,题为“二维反演大地电磁数据,用于了解马鲁古布拉的碳氢化合物存在”。本研究旨在根据大地电磁数据确定电阻率分布区域,根据大地电磁二维反演数据的电阻率值确定碳氢化合物的存在。进行数据处理的方法是(i)将原始数据从时域变换到频域,(ii)通过稳健处理来降低噪声,(iii)过程组合,(iv)选择交叉功率,(v)1D和2D反演。二维反演结果为剖面地下电阻率分布,沿MT1和MT7点1000米深处电阻率值为7-16Ωm的层为粘土岩,显示为盖层。电阻率值为34-120Ωm的层,位于MT6点和MT7点之间,深度为1500米,被指示为砂岩储层。根据地质信息和剖面2D反演,他们的断层基于电阻率对比是在点MT2和MT3、MT3和MT4以及MT6和MT7之间。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
INVERSI 2D DATA MAGNETOTELURIK UNTUK MENGETAHUI KEBERADAAN HIDROKARBON DAERAH BULA, MALUKU
There had been done a regional research which tittle is “2D inversion magnetotelluric data for understanding the hidrocarbon presence in Bula, Maluku”. This study aims to determine the resistivity distribution area of research based on data Magnetotelluric, identifying the presence of hydrocarbons based on the value of the resistivity of the results of 2D inversion of data Magnetotelluric. Methods of data processing done are (i) transform raw data from the time domain into the frequency domain, (ii) reduce noise by robust processing, (iii) process combine, (iv) Selection cross power, (v) inversion 1D and 2D. 2D inversion results is sectional subsurface resistivity distribution, layer having resistivity values 7-16 Ωm along MT1 and MT7 point at a depth of 1000 meters is a clay stone which is indicated as cap rock. Layer with resistivity values 34-120 Ωm, which is between the point MT6 and MT7 at a depth of 1500 meters is indicated as the sandstone reservoir. Based on geologic information and sectional 2D inversion seen their fault based on the resistivity contrast is between the point MT2 and MT3, MT3 and MT4 and MT6 and MT7.
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JGE
JGE
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