IDENTIFIKASI CEKUNGAN HIDROKARBON “RAE” BERDASARKAN DATA MAGNETOTELURIK DI DAERAH BULA, MALUKU

JGE Pub Date : 2020-01-17 DOI:10.23960/JGE.V4I3.1073
Gita Purna Rae Wanudya, Syamsurijal Rasimeng, R. Rustadi, Noor Muhammad Indragiri
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Abstract

The research had been performed using Magnetotelluric to get a 2D model based on variations in resistivity of the subsurface rock. The purpose of this study was to determine the hydrocarbon formation zone. The research method to achieve the research objectives, among others, the first filtering performed on the data with a robust process. This process consists of Robust No Weight, Robust Rho Variance and Ordinary Cohenerency. The second step is done to change the format Selection XPR And Edi. A third inversion resistivity model for the review get a 2D cross section. Based on the findings of the eight data processing methods of measurement points obtained information Magnetotelluric rock formations. Formation hidrokrabon What are the areas is research a reservoir and caprock. The layer in 1600 m – 2700 m depth from the surface which resisvity 12 -33 m assumpted as clay cap. While the layer in 2700 m – 5000 m depth from the surface with high resistivity 41- 250 m is assumpted as oil sands (reservoir). The trap zone of this hidrocarbon formation categorized into structural trap which is the trap of anticline.
RAE碳氢化合物证书的鉴定提供了马鲁古布兰的磁电信数据
研究人员利用大地电磁法根据地下岩石的电阻率变化建立了二维模型。本研究的目的是确定油气形成带。该研究方法实现了研究目标,其中,首先对数据进行了稳健的过滤处理。该过程由鲁棒无权、鲁棒方差和普通相干性组成。第二步是更改“选择XPR和Edi”格式。第三个反演电阻率模型得到了二维截面。根据8种测点数据处理方法的发现,获得大地电磁地层信息。研究储层和盖层的区域是什么?假定距地表1600 ~ 2700 m深度电阻率为12 ~ 33 m的层为粘土盖层,假定距地表2700 ~ 5000 m深度电阻率为41 ~ 250 m的层为油砂(储层)。该组油气圈闭带可划分为构造圈闭,即背斜圈闭。
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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JGE
JGE
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