1) Sandstone Coglomerate Body
砂、砾岩体
2) 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
3) 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。
4) 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。
5) Sandstone rock
砂砾岩体
1.
Sandstone rock in Zhengnan slope is sector sedimentary under water which is formed in the fourth section of Shahejie formation in Paleogene period.
东营凹陷郑南斜坡带砂砾岩体是古近纪沙四段沉积时期形成的以砂、砾岩为主的近岸水下扇沉积体。
6) glutenite body
砂砾岩体
1.
In the prediction of the space distribution of the glutenite body of steep slope zone in the Biyang Sag,seismic attribute analysis and seismic inversion techniques,based on the sequence stratigraphy researches and the corresponding relationship between palaeo-geomorphologic channel and fan,were utilized to determine the glutenite body and its distributing boundary.
在对泌阳凹陷陡坡带砂砾岩体空间展布预测中,以层序地层学研究为基础,依据古地貌沟扇对应理论,利用地震属性分析技术和地震反演技术,寻找砂砾岩扇体并确定其分布边界。
2.
Taking the glutenite body in abrupt slope belt of Dongying Depression as an example,the paper studied coupling effect of "facies-potential" upon reservoir forming.
根据东营凹陷洼陷带岩性油藏勘探形成的"相—势"控藏理论,结合国内外"相"、"势"控藏研究文献调研,对"相—势"控藏作用原理进行了解剖,并以东营凹陷陡坡带砂砾岩扇体为例进行"相—势"控藏作用研究,验证了北带砂砾岩体成藏受"相—势"控制,总结了东营北带的"相—势"控藏特征,完善和发展了"相—势"控藏理论。
参考词条
补充资料：角砾岩透镜体
分子式：
CAS号：
性质：简单撞击坑视坑底下伏一层较厚由回落角砾岩块、熔岩组成的透镜状沉积层，如Meteor、Brent、Lonar Lake、West Hawk Lake等简单撞击坑。通常上伏晚期湖相沉积物，下伏冲击压力15～20GPa的原生坑底单矿物碎屑角砾岩。整个撞击坑显示出地球物理场异常。这一沉积构造特征，可通过地球物理方法寻找被掩藏的撞击坑。
CAS号：
性质：简单撞击坑视坑底下伏一层较厚由回落角砾岩块、熔岩组成的透镜状沉积层，如Meteor、Brent、Lonar Lake、West Hawk Lake等简单撞击坑。通常上伏晚期湖相沉积物，下伏冲击压力15～20GPa的原生坑底单矿物碎屑角砾岩。整个撞击坑显示出地球物理场异常。这一沉积构造特征，可通过地球物理方法寻找被掩藏的撞击坑。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。