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辫状河流相薄砂体地震子波效应和识别方法
Wavelet effect and recognition methods of thin sand bodies in braided river facies
【摘要】 在地震资料频率一定的情况下,地震子波旁瓣效应会增加薄砂岩识别和解释的难度。为了研究子波旁瓣的影响程度,设计系列正演模型,利用不同频率的零相位雷克子波合成人工地震剖面,确定砂体位置、频率与地震子波旁瓣效应的关系,研究振幅类属性与薄砂体描述的关系。结果表明,综合利用多频带地震剖面和振幅类属性,可以可靠地解释和描述厚度大于1/8波长的辫状河流相薄砂岩储层。
【Abstract】 Under a fixed seismic frequency,wavelet side lobes may increase the difficulty of interpreting and recognizing thin sand bodies.To investigate the impacts of wavelet side lobe effects,we design a series of forward models and produce synthetic seismic profiles using zero phase Ricker wavelets of different frequencies.The purpose is to identify the relationship of sand body location and frequency with side lobe effects.This study also aims at exploring the relationship between amplitude attributes and the description of thin sand bodies.The results show that,an integrated use of multi-frequency profile and amplitude attributes can reliably interpret and describe thin sand bodies of braided river facies which are thicker than 1/8 wavelength.
【Key words】 Ricker wavelet; amplitude attribute; side lobe of wavelet; side lobe effect; thin sand body;
- 【文献出处】 石油与天然气地质 ,Oil & Gas Geology , 编辑部邮箱 ,2010年02期
- 【分类号】P631.4
- 【被引频次】7
- 【下载频次】258