1) Daxing conglomerate body
大兴砾岩体
1.
The origin and hydrocarbon accumulation of Daxing conglomerate body in Langgu Sag;
廊固凹陷大兴砾岩体成因与油气成藏
2) Dayi conglomerate
大邑砾岩
1.
The Dayi conglomerate is deposited in the foreland basin located in the Longmen mountains of the Tibetan plateau.
通过对龙门山前陆盆地大邑砾岩的发育层序、沉积特征及物源的分析 ,建立其垂向相序 ,总结出大邑砾岩的沉积具冲积扇相的特点 ;恢复大邑砾岩发育时期的古地貌 ,推断其至少由三个冲积扇组成 :古岷江扇 ,古青衣江扇 ,古玉溪扇。
3) Daxi Conglomerate
大溪砾岩
1.
The Daxi Conglomerate,Guankou Formation,and Mingshan Formation distributed inthe Tianquan-Lushan area belong to Late Cretaceous-Palaeogene.
分布于芦山—天全地区的大溪砾岩与晚白垩世灌口组、老第三纪名山组属同期异相沉积。
2.
The Daxi conglomerate is a suite of thick-bedded, massive carbonate-conglomeratewith a maximum thickness of 2000 m.
大溪砾岩为一套厚层块状碳酸盐质砾岩,最大厚度达2000m以上,出露于四川盆地西缘的天全、宝兴、芦山一带,出露面积达100km2以上。
3.
Daxi conglomerate is massic carbonate conglomerate with high pebble content, well-sorted and well-rounded, which belongs to fluvial origin.
大溪砾岩为一套厚层碳酸盐质砾岩,具有砾石含量高,砾石分选、磨圆较好的特点。
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) conglomerate
[英][kən'ɡlɔmərət] [美][kən'glɑmərət]
砾岩体
1.
Comprehensive evaluation on the classification of conglomerate reservoirs in Luojia area.;
罗家地区砾岩体储集层分类综合评价
2.
Based on using such techniques as Jason pseudo-acoustic inversion,EPS inversion,StratiMagic dip,and curvature measurement,research on conglomerate in Caiyu area is conducted,which precisely shows the distribution of conglomerate,favorable sedimentary facies zones,and fracture development zones.
采育砾岩体研究的一套方法和技术是砾岩油气藏研究的成功范例,对整个大兴断层下降盘的砾岩体及其他地区砾岩油气藏的勘探具有一定的指导意义。
6) 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。
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。
参考词条