首页> 外文会议>Indonesian Petroleum Association Twenty-Eighth Annual Convention Vol.1, Feb 26-28, 2002, Jakarta >EVALUATION OF NATURALLY FRACTURED RESERVOIRS IN INDONESIA USING FORMATION IMAGING AND SONIC LOGS
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EVALUATION OF NATURALLY FRACTURED RESERVOIRS IN INDONESIA USING FORMATION IMAGING AND SONIC LOGS

机译:利用地层成像和声波测井评价印尼天然裂缝性储层

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Electrical and ultrasonic borehole images along with sonic logs can be used to characterize fracture systems. For electrical imaging tools, algorithms exist to determine from Rm and Rxo the fracture aperture, fracture continuity, the frequency with which fractures intersect the borehole wall (fracture density) and, from these values, the fracture porosity of the formation. Electrical image methods, however, assume that all conductive fractures are open and can transmit fluids. In reality, the majority of fractured reservoirs flow hydrocarbons from only a few isolated fractures, or else from a specific fracture "set" or "system". The picture is further complicated by clay-filled fractures that are difficult to distinguish from open fractures on both electrical and acoustic images. Sonic Stoneley wave analysis from low frequency sonic logging modes provides a key analytical tool that is complimentary to the image logs. Stoneley waves are essentially insensitive to non-productive fractures. Open fractures that extend significant distances from the borehole are easily identifiable. Relative intensity and size of fracturing are also easily observed on the Stoneley analysis, though the vertical resolution of the Stoneley measurement is lower than that of the borehole imaging tools. The methodology is firstly to identify zones of open fractures on the Stoneley analysis, then evaluate the orientation and density of fractures using a higher resolution image log. Sonic cross-dipole measurements can locate vertical fractures and indicate tectonic stress imbalance direction. Examples from Indonesia are presented, in which sonic logs and borehole images combined have been used to characterize fractures in reservoir lithologies that include igneous and metamorphic basement, interbedded volcanics and volcaniclastics, and limestones. The conclusions are, in a number of these examples, supported by production tests.
机译:电和超声井眼图像以及声波测井曲线可用于表征裂缝系统。对于电成像工具,存在从Rm和Rxo确定裂缝口径,裂缝连续性,裂缝与井壁相交的频率(裂缝密度)以及从这些值确定地层裂缝孔隙度的算法。然而,电成像方法假定所有导电裂缝都是开放的并且可以传输流体。实际上,大多数裂缝性储层仅从少数几个孤立的裂缝中,或者从特定裂缝的“集合”或“系统”中流出烃。粘土填充的裂缝使图像变得更加复杂,这些裂缝很难用电图像和声图像区别开裂裂缝。低频声波测井模式的声波斯通利波分析提供了一种重要的分析工具,是对图像测井的补充。斯通利波基本上对非生产性裂缝不敏感。容易识别出距井眼很远的开放裂缝。尽管Stoneley测量的垂直分辨率低于钻孔成像工具的垂直分辨率,但在Stoneley分析中也很容易观察到相对强度和压裂大小。该方法首先是在Stoneley分析中确定开放性裂缝的区域,然后使用更高分辨率的图像测井评估裂缝的方向和密度。声波跨偶极子测量可以定位垂直裂缝并指示构造应力不平衡方向。列举了印度尼西亚的例子,其中结合了声波测井和井眼图像来表征储层岩性的裂缝,包括火成岩和变质基底,层间火山岩和火山碎屑岩以及石灰石。在许多示例中,这些结论得到了生产测试的支持。

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