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N次根弱地震信号增强技术

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地震勘探区域已经进入了地表起伏剧烈和地下构造复杂的地区,称之为双复杂区.这样的地区地震采集的反射信号非常弱,即便采用多域多维的叠前噪音压制技术也难以增强地震弱信号.本文借助T-p变换对OVT域数据进行时空域倾角分析,提出了三维τ-p变换中的N次根倾斜叠加信号增强技术,建立零偏移距时间-倾角地震属性道,计算给定数据子体(主测线,联络侧线,时间)内的相干值,依据计算的相干值对数据进行重新排序得到N次根倾斜叠加数据,可作为精准的基础数据.我们将该方法用于中国西部W区域的低信噪比地震数据的压噪,选取合适的N值,使地层深部的信噪比得到大幅改善,实现了增强地震弱信号的目的,验证了该方法对低信噪比资料的良好压噪效果.
N-th root slant stack for enhancing weak seismic signals
Seismic imaging of complicated underground structures with severe surface undulation(i.e.,double complex areas)is challenging owing to the difficulty of collecting the very weak reflected signal.Enhancing the weak signal is difficult even with state-of-the-art multi-domain and multidimensional prestack denoising techniques.This paper presents a time-space dip analysis of offset vector tile(OVT)domain data based on the r-p transform.The proposed N-th root slant stack method enhances the signal in a three-dimensional τ-p domain by establishing a zero-offset time-dip seismic attribute trace and calculating the coherence values of a given data sub-volume(i.e.,inline,crossline,time),which are then used to recalculate the data.After sorting,the new data provide a solid foundation for obtaining the optimal N value of the N-th root slant stack,which is used to enhance a weak signal.The proposed method was applied to denoising low signal-to-noise ratio(SNR)data from Western China.The optimal N value was determined for improving the SNR in deep strata,and the weak seismic signal was enhanced.The results showed that the proposed method effectively suppressed noise in low-SNR data.

N-th rootWeak seismic signalτ-pOVT

李斐、谢俊法、姚宗惠、李美、赵玉莲、刘伟明、陈娟

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中国石油长庆油田勘探开发研究院,西安,710021

中国石油勘探开发研究院西北分院,兰州,730020

N次根 弱地震信号 τ-p变换 OVT域

2024

应用地球物理(英文版)
中国地球物理学会

应用地球物理(英文版)

影响因子:1.01
ISSN:1672-7975
年,卷(期):2024.21(3)
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