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Petrophysical properties of deep Longmaxi Formation shales in the southern Sichuan Basin, SW China

机译:SW中国南部南部深龙马县岩浆岩石物理特性

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Deep shale layer in the Lower Silurian Longmaxi Formation, southern Sichuan Basin is the major replacement target of shale gas exploration in China. However, the prediction of “sweet-spots” in deep shale gas reservoirs lacks physical basis due to the short of systematic experimental research on the physical properties of the deep shale. Based on petrological, acoustic and hardness measurements, variation law and control factors of dynamic and static elastic properties of the deep shale samples are investigated. The study results show that the deep shale samples are similar to the middle-shallow shale in terms of mineral composition and pore type. Geochemical characteristics of organic-rich shale samples (TOC > 2%) indicate that these shale samples have a framework of microcrystalline quartz grains; the intergranular pores in these shale samples are between rigid quartz grains and have mechanical property of hard pore. The lean-organic shale samples (TOC < 2%), with quartz primarily coming from terrigenous debris, feature plastic clay mineral particles as the support frame in rock texture. Intergranular pores in these samples are between clay particles, and show features of soft pores in mechanical property. The difference in microtexture of the deep shale samples results in an asymmetrical inverted V-type change in velocity with quartz content, and the organic-rich shale samples have a smaller variation rate in velocity-porosity and velocity-organic matter content. Also due to the difference in microtexture, the organic-rich shale and organic-lean shale can be clearly discriminated in the cross plots of P-wave impedance versus Poisson's ratio as well as elasticity modulus versus Poisson's ratio. The shale samples with quartz mainly coming from biogenic silica show higher hardness and brittleness, while the shale samples with quartz from terrigenous debris have hardness and brittleness less affected by quartz content. The study results can provide a basis for well-logging interpretation and “sweet spot” prediction of Longmaxi Formation shale gas reservoirs.
机译:南四川盆地南部南部硅藻土的深层页面层是中国页岩气勘探的主要替代目标。然而,由于对深层物理性质的系统实验研究缺乏,对深层页岩气藏的“甜点”的预测缺乏物理基础。基于岩石学,声学和硬度测量,研究了深页样品的动态和静态弹性性能的变异法和控制因素。研究结果表明,在矿物成分和孔型方面,深层页岩样品类似于中浅页岩。有机丰富的页岩样品的地球化学特征(TOC> 2%)表明这些页岩样品具有微晶石英粒的框架;这些页岩样品中的晶状体孔位于刚性石英粒之间并具有硬孔的机械性能。瘦有机页岩样品(TOC <2%),石英主要来自人造碎片,特征塑料粘土矿物颗粒作为岩石纹理的支撑框架。这些样品中的晶状体孔位于粘土颗粒之间,并显示机械性能的软孔的特征。深层页岩样品的微调差异导致具有石英含量的不对称倒置的V型变化,有机型岩页样品在速度 - 孔隙率和速度 - 有机物质含量中具有较小的变化率。同样由于微纹理的差异,可以在P波阻抗与泊松比的交叉曲线图中明确区分有机质的页岩和有机贫物,以及泊松比的弹性模量。具有石英的页岩样品主要来自生物二氧化硅,表现出更高的硬度和脆性,而来自鸡血碎片的石英的页岩样品具有较低的硬度和脆性受石英含量的影响。该研究结果可以为龙马克地形成页岩气藏的良好测井解释和“甜点”预测提供基础。

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