基于波各向异性和电成像测井资料的地应力定向评价方法——以四川盆地永川地区龙马溪组为例

Song Hu, Jun Li, Mi Liu, Youlong Zou
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引用次数: 0

摘要

地应力定向是研究油气运移与聚集、分析钻井过程中井壁稳定性、进行水平井设计、压裂改造和注水开发井网布置的关键参数。准确预测储层的地应力方位对油气勘探开发具有重要意义。利用成像测井资料的诱发裂缝和破裂裂缝来评价原位定向是最有效、最常用的方法。然而,在钻井过程中无法形成有效的诱导裂缝或破裂裂缝的情况下,无法仅通过成像数据来评估原位定向。以永川地区龙马溪组页岩储层为例,提出了一种新的原位定向评价方法。首先,通过波速各向异性实验确定了相对于岩心样品标记线的原位方位。其次,旋转岩心样品以获得岩心表面的展开图像。然后通过将岩心图像与电成像测井图像进行比较来确定电成像中岩心标记线的方向。通过这样做,可以获得芯的真实方向。该方法与通过诱导裂缝评价确定的地应力方向吻合良好,解决了电成像数据在评价塑性地层地应力方向方面的局限性。
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Evaluation method for in-situ stress orientation using wave anisotropy and electrical imaging logging data: A case study from the Longmaxi Formation in Yongchuan area, Sichuan Basin

In-situ stress orientation is a key parameter in studying oil and gas migration and accumulation, analyzing the stability of borehole wall during drilling, carrying out horizontal well design, fracturing reconstruction and well pattern layout in water injection development. Accurately predicting the in-situ stress orientation of reservoirs is of utmost importance for oil and gas exploration and development. It is the most effective and commonly used method to evaluate the in-situ orientation by using the induced fracture and breakout fracture of imaging logging data. However, in cases where effective induced fracture or breakout fracture cannot be formed during drilling, the in-situ orientation cannot be evaluated by imaging data alone. Taking the shale reservoir of Longmaxi Formation in Yongchuan area as an example, this paper presents a novel method for evaluating in-situ orientation. Firstly, the in-situ orientation is determined relative to the core sample marker line through the wave velocity anisotropy experiment. Secondly, the core sample is rotated to obtain an unfolded image of the core surface. The orientation of the core marker line in the electrical imaging is then determined by comparing the core image with the electrical imaging logging image. By doing so, the true orientation of the core can be obtained. This method aligns well with the in-situ stress orientation determined through induced fracture evaluation, addressing the limitation of electrical imaging data in evaluating in-situ stress orientation in plastic strata.

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