首页> 外文会议>Proceedings of The 38th IPA convention and exhibition-Strengthening Partnership to Enhance Indonesia’s Energy Resilience and Global Competitiveness >PETROPHYSICS AND ROCK PHYSICS CORRELATION ANALYSIS IN DETERMINING FORMATION PROPERTIES ON SHALY SANDS FORMATION
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PETROPHYSICS AND ROCK PHYSICS CORRELATION ANALYSIS IN DETERMINING FORMATION PROPERTIES ON SHALY SANDS FORMATION

机译:确定泥质砂岩地层性质的岩石物理和岩石物理相关性分析

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Rocks cutting samples of the Barakuda well showrnthat the developing reservoir around the area isrnsandstone. The Barakuda well is an exploration wellrnlocated in the Tarakan basin. The low-resistivityrnphenomena that occur in the reservoir intervalrnindicate that the sandstone reservoir on this locationrnis a heterogeneous sandstone. This means all rocksrnin the interval, including dirty sands, can bernconstructed by mixing clean sand and shale. Thisrnkind of case has a significant effect in petrophysicsrnparameters if evaluated without considering thernheterogenity. For example, the porosity andrnhydrocarbon saturation values would bernunderestimated if we assume the reservoir rocks arernhomogenous. Thus, we need to determine thernreservoir sand types to evaluate the petrophysicsrnparameters in the most compatible way.rnIn this research, the heterogenity of the sandstonernwas analyzed using a correlation between thernThomas–Stieber (TS) and Yin–Marion (YM)rnmodels as petrophysics and rock physics analysis.rnThese analyses are used to determine sand types inrnthe reservoir interval. The TS model predicts thernporosity resulting from various modes of sand-shalernmixing. The YM model predicts the associated Pwavernvelocities. Together, they offer a higherrndegree of constraint of formation properties.rnThe results show that from eight zones reservoirrnrocks, the first five zones are laminar shale and thernlast three are dispersed shale. Both these modelsrnhad the same conclusion in determining sandstonerntypes.
机译:巴拉库达(Barakuda)井的岩石切割样品表明,该地区周围正在发育的储层是砂岩。 Barakuda井是位于Tarakan盆地的勘探井。在储集层段发生的低电阻率现象,表明该位置的砂岩储集层为非均质砂岩。这意味着可以通过混合干净的沙子和页岩来构造该区间内的所有岩石,包括脏沙。如果不考虑异质性来评估,这种情况对岩石物理学参数会产生重大影响。例如,如果我们假设储层岩石是非均质的,那么孔隙度和碳氢饱和度值将被低估。因此,我们需要确定储层砂的类型以最兼容的方式评估岩石物理参数。在这项研究中,我们使用了Thomas-Stieber(TS)模型和Yin-Marion(YM)rn模型之间的相关性来分析砂岩的非均质性。这些分析可用于确定储层层段中的砂类型。 TS模型预测了沙石混合的各种模式导致的孔隙度。 YM模型可预测相关的P波速度。结果表明,在八个区域的储层岩石中,前五个区域是层状页岩,最后三个区域是分散的页岩。两种模型在确定砂岩类型方面具有相同的结论。

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