FWI velocity and imaging: A case study in the Johan Castberg area

N. Salaun, M. Reinier, I. Espin, G. Gigou
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引用次数: 3

Abstract

The Greater Castberg survey was acquired in 2019 using a source-over-spread acquisition design with an additional source at the front of the streamers, towed by the receiver boat, to permit recording of longer offsets. Starting from an initial anisotropic model, time-lag full waveform inversion (TLFWI) was used to compute a 13 Hz velocity model over the 5000 km2 area, which led to a much improved migration image (e.g., better imaged reservoir flat spots). When pushing the inversion frequency up to 90 Hz, the resultant TLFWI velocity model enabled more detailed delineation of reservoir boundaries compared to the migration image. Furthermore, the FWI Image as an alternative view of the FWI velocity model, provided access to new reflectivity information, overcoming some limitations of current migration tools. The use of the full wavefield, including refraction, reflection of primary, multiple and ghost, greatly enhanced image without needing the complex data pre-processing required by conventional imaging. In the context of thick gas clouds, this new imaging technique provided accurate sub-gas reflectivity, which effectively enhanced event continuity compared to reverse time migration (RTM) results.
FWI速度和成像:以Johan Castberg地区为例
Greater Castberg调查于2019年进行,采用了一种信号源过扩频采集设计,在拖缆前面有一个额外的信号源,由接收船牵引,以便记录更长的偏移量。从初始各向异性模型开始,使用时滞全波形反演(TLFWI)计算5000平方公里面积上的13 Hz速度模型,从而大大改善了迁移图像(例如,更好地成像了油藏平坦点)。当将反演频率提高到90 Hz时,所得的TLFWI速度模型能够比迁移图像更详细地描绘储层边界。此外,FWI图像作为FWI速度模型的另一种视图,提供了新的反射率信息,克服了当前迁移工具的一些局限性。利用全波场,包括折射、反射的一次波、多次波和鬼波,大大增强了图像,而无需传统成像所需的复杂数据预处理。在厚气体云的背景下,这种新的成像技术提供了精确的亚气体反射率,与逆时偏移(RTM)结果相比,有效地增强了事件的连续性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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