首页> 外文会议>Indonesian Petroleum Association Annual Convention v.1; 20031014-20031016; Jakarta; ID >CHARACTERIZATION OF DEEP-WATER DEPOSITIONAL SYSTEMS IN THE BASIN PLAIN ENVIRONMENT USING SHALLOW 3D SEISMIC DATA ACROSS THE TOPAZ ANTICLINE, NORTH SUMATRA, INDONESIA
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CHARACTERIZATION OF DEEP-WATER DEPOSITIONAL SYSTEMS IN THE BASIN PLAIN ENVIRONMENT USING SHALLOW 3D SEISMIC DATA ACROSS THE TOPAZ ANTICLINE, NORTH SUMATRA, INDONESIA

机译:沿印度尼西亚北苏门答腊塔帕兹背斜的浅层3D地震资料表征盆地平原环境中的深水沉积系统

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This study uses high quality 3D seismic of the ENI Indonesia concession area in the Krueng Mane PSC in the North Sumatra Basin of Indonesia to characterize the Late Pliocene - Recent, deep-water basin plain depositional system. The data provide fine images of basin plain depositional elements and develops the depositional history from different seismic intervals, as it integrates Dip Azimuth, Amplitude Extraction and Seismic Facies Maps. The main deposits identified in the area are debrites, drape sediments and channel deposits. The study has concentrated on the channel deposits. They can be classified into 4 channel patterns, which are channel levee, parallel, braided, and feeder channel patterns. The channel patterns have been influenced by the development of the main anticlinal structure and the growth faults.
机译:这项研究使用印度尼西亚北部苏门答腊盆地Krueng Mane PSC的ENI印度尼西亚特许权区的高质量3D地震来表征上新世晚期-最近的深水盆地平原沉积系统。该数据集成了倾角方位角,振幅提取和地震相图,可提供盆地平原沉积元素的精细图像,并开发不同地震间隔的沉积历史。该地区发现的主要沉积物是碎屑,悬垂沉积物和河道沉积物。研究集中在渠道沉积物上。它们可以分为4个通道模式,分别是通道堤,平行,编织和馈线通道模式。通道模式受主要背斜构造的发育和生长断裂的影响。

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