| 川东北下三叠统飞仙关组鲕粒白云岩孔喉的空间展布与刻画 |
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| 引用本文： | 张天付,寿建峰,郑兴平,佘敏,潘立银.川东北下三叠统飞仙关组鲕粒白云岩孔喉的空间展布与刻画[J].古地理学报,2012,14(2):187-196. |
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| 作者姓名： | 张天付 寿建峰 郑兴平 佘敏 潘立银 |
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| 作者单位： | 1.中国石油杭州地质研究院，浙江杭州 310023;2.中国石油天然气集团公司碳酸盐岩储层重点实验室，浙江杭州 310023 |
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| 基金项目： | 杭州地质研究院重点实验室技术方法基金项目(编号:131-01112B)资助 |
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| 摘 要： | 孔喉特征是储集层研究的核心，厘清储集层孔喉在三维空间中的展布对油气勘探与开发意义重大。文中借助微纳米CT立体成像技术和数字岩心技术对川东北飞仙关组残余鲕粒白云岩的孔喉特征进行刻画与描述，建立了微纳米级的孔喉三维空间展布模型，并计算了孔喉半径、形状因子、空间连通性等表征参数。此外，结合扫描电镜、压汞曲线等传统方法，对所建立的模型进行了有益的探讨和补充。结果表明，川东北地区残余鲕粒白云岩孔隙类型主要有粒间孔、粒间溶孔（铸模孔）、晶间（溶）孔、晶间缝和微裂隙等。其中，晶间孔和微裂隙为连通的喉道，其最小值可达20～30 nm。样品重结晶强烈，受重结晶晶体的生长及后期压实等改造作用的影响，喉道堵塞，储集层渗透性差。
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| 关 键 词： | 孔喉结构 微纳米CT 数字岩心 空间展布 |
| 收稿时间： | 2011-09-15 |
Spatial distribution and characterization of pore and throat of oolitic dolostone of the Lower Triassic Feixianguan Formation in northeastern Sichuan Province |
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| Zhang Tianfu
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Shou Jianfeng
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Zheng Xingping
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She Min
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Pan Liyin.Spatial distribution and characterization of pore and throat of oolitic dolostone of the Lower Triassic Feixianguan Formation in northeastern Sichuan Province[J].Journal of Palaeogeography,2012,14(2):187-196. |
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| Authors: | Zhang Tianfu Shou Jianfeng Zheng Xingping She Min Pan Liyin |
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| Institution: | 1.PetroChina Hangzhou Research Institute of Geology，Hangzhou 310023，Zhejiang;2.Key Laboratory of Carbonate Reservoir，CNPC，Hangzhou 310023，Zhejiang |
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| Abstract: | The research of pore and throat texture is a key issue for oil exploration and development.With micro-CT and numerical rock technology,the authors characterized the texture of pore and throat of residual oolitic dolostone of the Lower Triassic Feixianguan Formation in northeastern Sichuan Province,and established the 3D models in micro scale.Based on these models,its radius,shape factor and spatial connectivity were calculated.A further discussion on the models has been processed under the help of SEM and mercury injection.The result indicates that pore system of the residual oolitic dolostone include interparticle pore,interparticle dissolved pore(moldic pore),intercrystalline(dissolved)pore,intercrystalline aperture,microfracture etc.The intercrystalline pore and microfracture are the connectivity pathway as throat.Its minimal size could be reduce to 20～30 nm.Recrystallization of the experimental sample is heavy,so the throat would be blocked due to the growth of the crystal and tectonic compaction after later diagenesis. |
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| Keywords: | pore and throat texture micro-CT numerical rock spatial distribution |
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