The Seismic Identification of Small Strike-Slip Faults in the Deep Sichuan Basin (SW China)

Processes Pub Date : 2024-07-18 DOI:10.3390/pr12071508
Hai Li, Jiawei Liu, Majia Zheng, Siyao Li, Hui Long, Chenghai Li, Xuri Huang
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Abstract

Recently, the “sweet spot” of a fractured reservoir, controlled by a strike-slip fault, has been found and become the favorable target for economic exploitation of deep (>4500 m) tight gas reservoirs in the Sichuan Basin, Southwestern China. However, hidden faults of small vertical displacements (<20 m) are generally difficult to identify using low signal–noise rate seismic data for deep subsurfaces. In this study, we propose a seismic processing method to improve imaging of the hidden strike-slip fault in the central Sichuan Basin. On the basis of the multidirectional and multiscale decomposition and reconstruction processes, seismic information on the strike-slip fault can be automatically enhanced to improve images of it. Through seismic processing, the seismic resolution increased to a large extent enhancing the fault information and presenting a distinct fault plane rather than an ambiguous deflection of the seismic wave, as well as a clearer image of the sectional seismic attributes. Subsequently, many more small strike-slip faults, III–IV order faults with a vertical displacement, in the range of 5–20 m, were identified with the reprocessing data for the central Sichuan Basin. The pre-Mesozoic intracratonic strike-slip fault system was also characterized using segmentation and paralleled dispersive distribution in the Sichuan Basin, suggesting that this seismic process method is applicable for the identification of deep, small strike-slip faults, and there is great potential for the fractured reservoirs along small strike-slip fault zones in deep tight matrix reservoirs.
四川盆地(中国西南部)深部小型走向滑动断层的地震识别
最近,在中国西南部四川盆地发现了由走向滑动断层控制的断裂储层 "甜点",并成为深层(大于 4500 米)致密气藏经济开采的有利目标。然而,垂直位移较小(小于 20 米)的隐伏断层一般很难利用低信噪比地震数据识别深部地表下的断层。本研究提出了一种地震处理方法,以改善四川盆地中部隐伏走向滑动断层的成像。在多方向、多尺度分解和重建过程的基础上,自动增强走向滑动断层的地震信息,从而改善其成像。通过地震处理,提高了地震分辨率,在很大程度上增强了断层信息,呈现出明显的断层面,而不是模糊的地震波偏转,同时断面地震属性图像也更加清晰。随后,通过对四川盆地中部数据的重新处理,发现了更多垂直位移在 5-20 米之间的三至四阶小型走向滑动断层。四川盆地的前新生代地壳内走向滑动断层系统也通过分段和平行分散分布得到了表征,表明这种地震过程方法适用于识别深部小型走向滑动断层,深部致密基质储层中沿小型走向滑动断层带的断裂储层潜力巨大。
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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