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QUALITATIVE AND QUANTITATIVE MONITORING OF SEISMIC QUALITY DURING DATA-PROCESSING FOR FUTURE SEISMIC RESERVOIR CHARACTERIZATION STUDIES(SISI-NUBI FIELD, INDONESIA)

机译:未来地震储层特征研究中数据处理过程中地震质量的定性和定量监测(SISI-NUBI田,印度尼西亚)

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A Multi-Azimuth Pre-Stack Depth Migration (PSDM) reprocessing was performed on Sisi-Nubi 3D seismic data in 2010. Besides its traditional purpose to obtain a better structural image, this reprocessed data is intended to be used for future pre-stack seismic reservoir characterization (SRC) studies, requiring amplitude and phase to be preserved. On Sisi-Nubi, the main geophysical challenges are related to a complex geological setting with strong lateral lithology variations, provoking important statics, seismic signal attenuation and amplitude variation. The standard processing quality control (QC) performed with the data-processing contractor cannot always guarantee that the final processing will deliver results that are appropriate for SRC studies. This paper describes a set of internal AVO (Amplitude Varitions with Offset)-based QCs whose main objective is to monitor the seismic quality in terms of signal preservation.The first stage of the method consists of building a referential of QCs on former 2005 Pre-Stack Time Migration (PSTM) data and of identifying the key steps of the 2010 processing sequence that may be detrimental to amplitude stability and may also have a negative impact on signal phase, signal-to-noise, etc. In the second stage, angle sub-stack cubes are produced after each of these key steps and QCs are performed on these intermediate results. The QCs consist of analyzing 10 parameters or Seismic Quality Indexes that can be grouped into 3 main categories: Geological Representativity (bandwidth index, resolution, and noise attenuation). Offset Consistency (cross correlation, phase & time-shift dispersions, and stretch), and Spatial Stability (stretch dispersion, lateral amplitude variation, andresolution dispersion). After compiling all the QC parameters, the evolution of each parameter is assessed using the former 2005 PSTM data as reference.Because it is performed all along the processing workflow, this monitoring introduces an approach that enables qualitative and quantitative control of the PSDM processing with regard to the AVO response in the pre-stack domain. Indeed, at every important stage, recommendations or modifications can be submitted to the contractor performing the data-processing. To conclude, the final processing results have to bring as much geological information as possible, producing preserved relative amplitudes with minimal artificial variations and laterally stable responses.
机译:于2010年在思思-努比三维地震数据执行的多方位叠前深度偏移(PSDM)后处理除了其传统目的,以获得更好的结构图像,该再加工数据旨在被用于将来的叠前地震储层表征(SRC)的研究中,需要的振幅和相位被保存。上思思-努比,主地球物理挑战涉及复杂的地质背景与强横向岩性变化,引起重要静力学,地震信号衰减和振幅变化。与数据处理承包商进行的标准处理的质量控制(QC)不能总是保证在最后的处理将提供的结果适用于SRC的研究。本文描述了一组内部的AVO(振幅Varitions使用偏移)系的QC,其主要目的是监测在信号preservation.The的方法的第一阶段包括建立QC的一个参考原上预2005的方面地震质量叠前时间偏移(PSTM)数据和识别2010处理顺序的关键步骤,可能是有害的振幅稳定性,并且还可以对信号相位有负面影响的,信号与噪声等。在第二阶段中,角之后的每个的这些关键步骤和QC的是在这些中间结果进行子堆立方体产生的。所述的QC分析由10个参数或地震质量指标可以被分成3个主要类别:地质代表性问题(带宽索引,分辨率和噪声衰减)。偏移一致性(互相关,相位和时间偏移的分散体,和拉伸),和空间稳定性(拉伸分散体,横向幅度变化,andresolution分散体)。编译所有的QC参数后,各参数的变化是使用作为reference.Because它沿处理流程进行所有前2005 PSTM数据评估,该监测引入了一种方法,使关于的PSDM处理的定性和定量控制在叠前域中的AVO响应。事实上,在每一个重要阶段,建议或修改可以提交给执行数据处理承包商。最后,最终的处理结果有使尽可能多的地质信息成为可能,产生具有最小的人工变化和横向稳定的响应保存相对幅度。

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