...
首页> 外文期刊>Journal of Seismic Exploration >ANALYSIS OF EFFECTIVE PARAMETERS FOR SEMBLANCE-BASED COHERENCY ATTRIBUTES TO DETECT MICRO-FAULTS AND FRACTURES
【24h】

ANALYSIS OF EFFECTIVE PARAMETERS FOR SEMBLANCE-BASED COHERENCY ATTRIBUTES TO DETECT MICRO-FAULTS AND FRACTURES

机译:基于实例的相干性属性检测微断层和断裂的有效参数分析

获取原文
获取原文并翻译 | 示例

摘要

Coherency attributes are useful in the interpretation of seismic data and can be applied to 3D seismic data. When coherency attributes are applied to seismic data, they indicate the continuity between two or more traces within a seismic window. The rate of seismic continuity is an index of geological continuity. Areas of traces that change with faults or other geological phenomena have lower coherency in comparison with adjacent traces. Coherency attributes can be divided into three major groups: (1) cross-correlation, (2) eigenstructure and (3) semblance. In this paper, first, the ability of the three coherency attributes mentioned above to detect micro-faults was tested over 3D real data. The results proved that the semblance algorithm was much more powerful than the other algorithms in detecting micro-faults. Therefore, in the remainder of the study only the semblance attribute was employed. The effect of the dominant frequency, the signal-to-noise ratio, the dimensions of the analysis cube, and the apparent dip in the x- and in the y-directions on the semblance coherency attribute was investigated. The effects of these parameters were tested on 3D synthetic seismic data consisting of (1) horizontal layers, (2) dipping layers, and (3) cross-dipping layers. It is shown that for frequencies up to 20 Hz, there was no clear image of the micro-faults. However, for frequencies above 20 Hz, the resolution of micro-faults was increased. The results indicate that micro-faults are detectable with a signal-to-noise ratio of 1 or higher. When a signal-to-noise ratio of 0.5 is selected, micro-faults can still be detectable but with a lower resolution. According to synthetic models, a temporal window of 32 ms (k = 8) showed the best results for horizontal and dipping layers. The best size for the spatial window is 10x10 for horizontal and dipping layers. Therefore, the optimum cube dimensions of analysis are 10 × 10×8. For these dimensions, the signal-to-noise ratio increases and micro-faults are clearly detectable. Regarding the cross-dipping model, apparent dip directions, p and q, were analyzed. The same optimum value of 10 ms/m was obtained for both. Real data which is related to carbonate units showed satisfactory results as well: micro-faults and minor fractures hidden in the primary data were detectable after applying the algorithm.
机译:相干属性在解释地震数据时很有用,并且可以应用于3D地震数据。将相干属性应用于地震数据时,它们指示地震窗口内两条或更多条迹线之间的连续性。地震连续性的速率是地质连续性的指标。与邻近的迹线相比,随断层或其他地质现象而变化的迹线区域的一致性较低。相干属性可以分为三大类:(1)互相关,(2)本征结构和(3)相似性。在本文中,首先,在3D真实数据上测试了上述三个一致性属性检测微故障的能力。结果证明,在检测微故障方面,相似算法比其他算法功能强大。因此,在其余的研究中,仅使用了外表属性。研究了主频,信噪比,分析立方体的尺寸以及在x和y方向上的表观倾角对表面相似性属性的影响。在由(1)水平层,(2)浸入层和(3)交叉浸入层组成的3D合成地震数据上测试了这些参数的影响。结果表明,对于高达20 Hz的频率,没有清晰的微故障图像。但是,对于20 Hz以上的频率,微故障的分辨率有所提高。结果表明,以1或更高的信噪比可以检测到微故障。当信噪比选择为0.5时,仍然可以检测到微故障,但分辨率较低。根据综合模型,对于水平层和浸入层,时间窗为32 ms(k = 8)显示出最佳结果。对于水平和浸入层,空间窗口的最佳大小是10x10。因此,分析的最佳立方体尺寸为10×10×8。对于这些尺寸,信噪比增加,并且可以清楚地检测到微故障。关于交叉浸入模型,分析了视在浸入方向p和q。两者均获得了10 ms / m的最佳值。与碳酸盐岩单元有关的真实数据也显示出令人满意的结果:应用该算法后,可检测到隐藏在原始数据中的微断层和小裂缝。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号