Marine Seismic Tomography for Detecting Fracture and Void of Subsurface Seabed : a Theoretical Framework Development and Application of Wide-Band Fresnel Tomography

B. Nurhandoko, F. Ambia, Kaswandhi Triyoso, M. Choliq, Mahatman L. Budi, A. Suhendi, Wahyu E. Abdianto
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引用次数: 2

Abstract

Fracture as well as void can generate unstable structure in offshore building. We use seismic tomography based on scattering wave instead of conventional raypath seismic tomography. Conventional raypath tomography usually needs dense source-receiver configuration as well as wide-angle measurement. Therefore, it will be high cost in field data acquisition. We propose scattering wavepath tomography by means of Fresnel interpolated wavepath (FIW) wide-band inversion. FIW is an interpolation between imaginary part of Rhytov scattering wavepath and raypath. Then, FIW is combined with wide band inversion procedure to handle sparseness configuration of measurement. By this method, smooth constraint is implemented more naturally by based on wave's spectrum. In this paper, we showed some applications of Wide-band inversion of FIW tomography in imaging fracture and void in marine carbonate sea bed.
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海底裂缝空洞探测的海洋地震层析成像:宽带菲涅耳层析成像的理论框架、发展与应用
在海上建筑中,裂缝和空隙都会引起结构失稳。我们采用基于散射波的地震层析成像技术来代替传统的射线路径地震层析成像技术。传统的射线路径层析成像通常需要密集的源接收器配置和广角测量。因此,现场数据采集成本较高。本文提出了利用菲涅耳插值波路径(FIW)宽带反演的散射波路径层析成像方法。FIW是瑞托夫散射波路的虚部与射线路径之间的插值。然后,将FIW与宽带反演程序相结合,处理测量的稀疏配置。该方法可以更自然地利用波的谱来实现平滑约束。本文介绍了FIW层析成像宽频带反演在海相碳酸盐岩海底裂缝和孔隙成像中的一些应用。
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