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Integrated geological and geophysical analysis by hierarchical classification: combining seismic stratigraphic and AVO attributes

机译:通过分层分类对地质和地球物理进行综合分析:结合地震地层和AVO属性

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摘要

The benefits of seismic attribute classification in subsurface studies have been published widely. The approach is usually the same and, in most cases, driven by a two-step procedure — an unsupervised classification and a supervised scheme where training is used to redefine classes based on well-log data flagging a specific fluid or lithology. In parallel to the multi-attribute analysis, interpreters have also benefited from recent advances in computing power, enabling the generation of multi-trace or texture attributes. In these two workflows, the focus is either on the seismic texture fades for seismic stratigraphic purposes, or on the reservoir facies for fluid and lithology mapping. This paper presents a case study in which both texture facies and fluid prediction are linked by performing a hierarchical classification scheme whereby a multi-attribute-based volume, which captures seismic texture information, is combined with amplitude versus offset (AVO) attributes to map fluid response into a single, coherent reservoir facies volume. This methodology is then applied for exploration data screening in offshore Borneo in the Greater Samarang sub-block (East Baram Delta, offshore Sabah, Malaysia). In this case study, the geological analysis, seismic geomorphology, seismic stratigraphy and combined fluid response from AVO attributes facilitate the development of new play concepts in the highstand system tracts and in the morphology generated by incised valleys in shoreface deposits.
机译:在地下研究中,地震属性分类的好处已被广泛发表。这种方法通常是相同的,并且在大多数情况下是由两步程序驱动的:无监督分类和监督方案,其中使用训练基于标记特定流体或岩性的测井数据重新定义类别。与多属性分析并行的是,解释器还受益于计算能力的最新发展,能够生成多迹线或纹理属性。在这两个工作流程中,重点要么是出于地震地层目的考虑的地震纹理衰减,要么是为了进行流体和岩性测绘的储层相。本文介绍了一个案例研究,其中通过执行分层分类方案将纹理相和流体预测两者联系在一起,从而将捕获地震纹理信息的基于多属性的体积与振幅与偏移量(AVO)属性相结合来绘制流体响应成一个单一,连贯的储层相。然后将这种方法应用于大萨马兰子区块(马来西亚沙巴近海的东巴拉姆三角洲)婆罗洲近海的勘探数据筛选。在本案例研究中,地质分析,地震地貌学,地震地层学和AVO属性的综合流体响应促进了高架系统区和岸面沉积物切谷形成的形态学中新游隙概念的发展。

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