Advanced Multiple Attenuation and Model Building Techniques Provide New Insights Into the Jurassic Play of Timor sea, Offshore Australia

Tanporn Pitibhabhong, R. Chakraborty, S. H. Ng, C. K. Lim, I. Paton, N. Phantawee
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Abstract

The Sandalford area, located in Australia’s northwestern continental margin, is proximal to the Cash-Maple and Tenacious field discoveries. The area has Eocene-Paleocene Carbonates overlying siliciclastic Cretaceous section, resulting in a strong velocity inversion as well as generating complex free-surface and internal-multiple contaminations at the deeper Jurassic reservoir section. We present a reprocessing case study of a narrow-azimuth, towed-streamer seismic dataset acquired in shallow water using advanced multiple attenuation and earth model building techniques, with the main goal of improving our understanding of the complex geology beneath. The multiple attenuation part of the workflow employs a cascaded approach, initially addressing water-layer multiples, remaining free-surface multiples, and followed with internal multiples. Implementation of high-frequency visco-acoustic full-waveform inversion (Q-FWI) improved the overburden velocity model and combined with effective multiple attenuation algorithms, reduced the uncertainty of primary events in the pre-carbonate section, therefore reducing errors in common image point (CIP) tomography. The results were quality-controlled against the well data, providing new insights with improved structural and stratigraphic delineation.
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先进的多重衰减和模型构建技术为澳大利亚帝汶海侏罗系提供了新的认识
Sandalford地区位于澳大利亚西北大陆边缘,靠近Cash-Maple和Tenacious油田发现。该地区始新世-古新世碳酸盐岩覆盖在白垩纪硅质碎屑剖面上,速度反演强烈,深层侏罗系储层段形成复杂的自由面污染和内部多重污染。本文介绍了利用先进的多重衰减和地球模型构建技术在浅水中获得的窄方位角拖曳拖曳地震数据集的再处理案例研究,其主要目标是提高我们对水下复杂地质的理解。工作流程的多重衰减部分采用级联方法,首先处理水层倍数,剩余的自由表面倍数,然后处理内部倍数。实施高频粘声全波形反演(Q-FWI)改进了覆盖层速度模型,并结合有效的多重衰减算法,降低了碳酸盐岩前剖面主要事件的不确定性,从而减少了共同像点(CIP)层析成像的误差。结果与井数据进行了质量控制,为改进构造和地层圈定提供了新的见解。
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