首页> 外文期刊>Journal of Petroleum Exploration and Production Technology >Integrated reservoir characterization of the Paleocene Farewell Formation, Taranaki Basin, New Zealand, using petrophysical and petrographical analyses
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Integrated reservoir characterization of the Paleocene Farewell Formation, Taranaki Basin, New Zealand, using petrophysical and petrographical analyses

机译:利用岩石物理和岩石学分析对新西兰塔拉纳基盆地古新世告别组进行综合储层表征

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A reservoir characterization study, using petrophysical and petrographic analyses, has been made on the Paleocene Farewell Formation in the Taranaki Basin, New Zealand, based on five selected wells. Farewell Formation is largely a sandstone formation belonging to the Kapuni Group. The integrated study has shown that Farewell Formation is a good promising reservoir with average effective porosity of 17.7% and permeability of 415 mD. The petrographic study indicates the occurrence of abundant intergranular and secondary pores. It also proved that the Farewell Formation has been affected by several diagenetic features. Compaction, cementation and clay mineral authigenesis are the most common. Quartz and feldspar overgrowths have been recorded in many samples, and secondary porosity due to dissolution is also observed. In general, good reservoir quality features are dominant in the Farewell Formation and diagenesis has little effect on the reservoir quality. These findings are supported by well log interpretation results, which confirm good sand and net pay zones are available with very low average water saturation (24.9%).
机译:利用岩石物理和岩石学分析,在新西兰塔拉纳基盆地的古新世告别地层进行了储层表征研究,该研究基于五口选定的井。告别地层主要是属于Kapuni集团的砂岩地层。综合研究表明,告别地层是良好的储层,平均有效孔隙度为17.7%,渗透率为415 mD。岩石学研究表明存在大量的粒间孔和次生孔。还证明了告别组已受到多种成岩作用的影响。压实,胶结和粘土矿物的成因是最常见的。在许多样品中都记录了石英和长石的过度生长,并且还观察到由于溶解引起的二次孔隙。通常,良好的储层质量特征在告别组中占主导地位,并且成岩作用对储层质量影响很小。这些发现得到了测井解释结果的支持,这些结果证实了可以得到良好的砂层和净产层,平均水饱和度非常低(24.9%)。

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