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1)  Sand body
砂岩体
1.
On the basis of slices,SEM,X-diffraction and physi- cal properties of sandstones from the sand bodies of Gudong, Shengtuo and Dongxin oilfields,analyses were performed on the pore distribution characteristics of sand body of different epochs,burial depths and diagenetie stages.
主要利用薄片、物性等资料,以孤东、胜坨、东辛油田诸砂岩体为例,分析了不同时代、埋深和成岩阶段的砂岩体孔隙分布特征。
2.
Comparison tracking for sand body is a difficulty task for seismic interpretation.
砂岩体的对比追踪,是地震解释工作的难点。
2)  sandbody
砂岩体
3)  sandstone body
砂岩体
4)  glutenite
砂砾岩体
1.
The Evaluation Tcehnique of the Gas Reservoir of Glutenite Reservoir in North Region of Dongying;
东营凹陷北带砂砾岩体天然气测井评价方法
2.
Study on sequence stratigraphy of glutenite in terrestrial lacustrine basin-taking Luojia & Kenxi area of Jiyang Depression as an example;
陆相湖盆砂砾岩体层序地层学研究——以济阳坳陷罗家—垦西地区为例
3.
Classification and distribution of glutenite on the steep slope of faulted lake basin in Jiyang depression;
济阳坳陷断陷湖盆陡坡带砂砾岩体分类及展布
5)  glutinite body
砂砾岩体
1.
The recognition on oil-gas reservoir of glutinite body of Sha 3 sub-interval of CH 66 Block in Taorhe Shallow Depression;
套尔河洼陷CH66区块沙三下亚段砂砾岩体油气藏认识
2.
Planar strips,vertical stages,continuous backpedal and strong succession are the characteristics of the glutinite body distribution in a rift extensional basin.
断陷伸展湖盆陡坡带上的砂砾岩体具有"平面分带、垂向分期、持续后退、继承性强"的分布特征。
6)  sandstone and conglomerate
砂砾岩体
1.
There are many sandstone and conglomerate in the sedimentry system in Jiyang depression.
济阳坳陷广泛发育各类沉积体系的砂砾岩体,而砂砾岩体油气藏一直是勘探的重点方向。
补充资料:粉砂岩
粉砂岩
siltstone

   由粒径为0.0625~0.0039毫米(mm)的粉砂的含量占50%以粉砂岩标本的一种碎屑沉积岩。除粉砂以外其它由砂、粘土或化学沉淀物组成。按粒度划分为粗粉砂岩(0.0625~0.0312mm)和细粉砂岩(0.0312~0.0039mm)。按碎屑成分划分为石英粉砂岩、长石粉砂岩、岩屑粉砂岩(少见)和它们间的过渡类型。根据胶结物成分划分为粘土质粉砂岩、铁质粉砂岩、钙质粉砂岩和白云质粉砂岩。黄土也是一种疏松的或半固结的粉砂质沉积物。粉砂岩多形成于河漫滩、三角洲、潟湖和海洋的较深水部位。
    
   

粉砂岩标本

粉砂岩标本

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