基于小波分频变换和动态时间规整的智能测井-地震综合地层对比方法——以拉兴油田为例

IF 3.6
Mian Lu , Dongmei Cai , Xiandi Fu , Shunguo Cheng , Yu Sun , Pengkun Liu , Yanli Jiao
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引用次数: 0

摘要

地层对比对于储层的精细表征是必不可少的。然而,对于复杂的沉积环境和多源地质环境,仅依靠测井数据的传统数据驱动方法难以构建等时地层格架。为此,本研究提出了一种结合小波分频变换(WFT)和动态时间规整(DTW)的智能、自动测井-地震综合地层对比方法(也称为WFT-DTW方法)。该方法将地震数据作为地层相关性的约束,通过WFT精确跟踪地震标志层位。在框架构造约束下,引入DTW算法自动关联子层边界。通过松辽盆地拉兴油田杏树岗区块SA0组地层对比实验,验证了该方法的有效性。该区块目标层亚层厚度为5 ~ 8 m,砂岩平均厚度为2.1 m,非均质性明显。160口后试井1760层的验证结果表明,WFT-DTW方法在断层发育不全、标志层位明显的地区具有较强的子层对比能力。结果,对1682层进行了后验相关,符合率高达95.6%。所提出的方法可以补充人工对比工作,同时也为储层岩性和砂体表征提供有价值的技术支持。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

An intelligent log-seismic integrated stratigraphic correlation method based on wavelet frequency-division transform and dynamic time warping: A case study from the Lasaxing oilfield

An intelligent log-seismic integrated stratigraphic correlation method based on wavelet frequency-division transform and dynamic time warping: A case study from the Lasaxing oilfield
Stratigraphic correlations are essential for the fine-scale characterization of reservoirs. However, conventional data-driven methods that rely solely on log data struggle to construct isochronous stratigraphic frameworks for complex sedimentary environments and multi-source geological settings. In response, this study proposed an intelligent, automatic, log-seismic integrated stratigraphic correlation method that incorporates wavelet frequency-division transform (WFT) and dynamic time warping (DTW) (also referred to as the WFT-DTW method). This approach integrates seismic data as constraints into stratigraphic correlations, enabling accurate tracking of the seismic marker horizons through WFT. Under the constraints of framework construction, a DTW algorithm was introduced to correlate sublayer boundaries automatically. The effectiveness of the proposed method was verified through a stratigraphic correlation experiment on the SA0 Formation of the Xingshugang block in the Lasaxing oilfield, the Songliao Basin, China. In this block, the target layer exhibits sublayer thicknesses ranging from 5 m to 8 m, an average sandstone thickness of 2.1 m, and pronounced heterogeneity. The verification using 1760 layers in 160 post-test wells indicates that the WFT-DTW method intelligently compared sublayers in zones with underdeveloped faults and distinct marker horizons. As a result, the posterior correlation of 1682 layers was performed, with a coincidence rate of up to 95.6 %. The proposed method can complement manual correlation efforts while also providing valuable technical support for the lithologic and sand body characterization of reservoirs.
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