1) detrital material,fragmentary material
碎屑物质
2) Debris
碎屑
1.
Debris scores were calculated after photographing with a digital camera.
冲洗后纵向劈开标本,采用数码照相机照相和扫描电镜观察,分别计算比较根管内碎屑百分数及牙本质小管开口数。
2.
Debris scores were calculated after photographing with a digital camera and the number of visible open dentinal tubules was evaluated by SEM.
采用数码照相机照相和扫描电镜观察,分别比较根尖1/3区和根中1/3区根管内的碎屑百分数和牙本质小管开口数。
3.
Objective To explore the best way to reduce the forming of debris of rubber stopper by using No.
目的探讨用12号侧孔针头与斜面针头穿刺胶塞配药减少碎屑形成的最佳方法,为临床提供指导。
3) clastic rock
碎屑岩
1.
Promising natural gas exploration belts in clastic rock formations,Sichuan Basin;
四川盆地碎屑岩领域有利天然气勘探方向浅析
2.
Feasibility of time-lapse seismic monitoring in long-period water-drive continental facies clastic rock reservoir.;
陆相碎屑岩油藏长期水驱时移地震监测的可行性
3.
Sedimentary facies of lower Cretaceous clastic rock in Hongshan area in the north edge of Qaidam Basin;
柴达木盆地北缘红山地区下白垩统碎屑岩沉积相特征
4) clastic rocks
碎屑岩
1.
Application of paleosols in terrigenous clastic rocks to stratigraphic analysis;
陆源碎屑岩中的古土壤在地层分析中的应用
2.
The clastic rocks in Permian System at the southeast area of Ordos Basin contain tremendous potential in exploration of natural gas.
鄂尔多斯盆地东南部二叠系碎屑岩具有巨大的天然气勘探潜力。
3.
The middle-upper Jurassic clastic rocks in Qiangtang basin, north Tibet are characterized by their great thickness.
详细野外剖面测量基础上,对羌塘盆地东部中-上侏罗统剖面主要岩类的宏观特征(颜色和构造)、物质组分、结构及磁化率等特征进行系统研究,研究区碎屑岩主要为砾岩、砂岩、粉砂岩和泥岩等岩类,磁化率值呈现低→高→低→高→低(雀莫错组→布曲组→夏里组→索瓦组→雪山组)的规律性变化。
5) Detrital zircon
碎屑锆石
1.
Pre-Mesozoic basement provenance tracing of the Songliao Basin by means of detrital zircon SHRIMP chronology;
用碎屑锆石SHRIMP年代学方法恢复松辽盆地南部前中生代基底的源区特征
2.
Formation time of supracrustal rocks in Tiejiashan granite of the Anshan area:evidence from detrital zircon SHRIMP dating;
鞍山地区铁架山花岗岩中表壳岩的碎屑锆石SHRIMP年龄及其地质意义
6) coarse fragment
粗碎屑
1.
Based on analysis of heavy minerals, detrital components of gravel - bearing coarse fragments, maturity of minerals and clay components of mudstones, it is believed that Jurassic would have sourced mainly from two directions, which are the southern Kuluke Mountain and the western Tashidian area respectively.
通过对该区重矿物、含砾粗碎屑组分、矿物成熟度及泥岩粘土成分等的分析,认为该区侏罗系存在两个主要的物源方向,一个来自南部库鲁克山,另一个来自西部的塔什店地区。
2.
Methods Using the three parameters of heavy mineral assemblage of detrital rock,coarse fragment component and mineralogic maturity,the basin sedimentary boundaries will be foun and studied.
方法从大量的地质资料入手,利用碎屑重矿物组合、粗碎屑组分和矿物成熟度3种参数确定古盆地边界。
参考词条
补充资料：火成碎屑岩
| 火成碎屑岩 pyroclastic rock 由火山碎屑物质堆积而成的岩石。又称火山碎屑岩。其特征介于熔岩与正常沉积岩之间。火山碎屑物的含量一般大于50％，其次为正常沉积物或熔岩物质。碎屑物的种类有岩屑、晶屑、玻屑、火山弹、浮岩及火山渣等。碎屑物的大小不一，常见棱角状。具集块结构、火山角砾结构、凝灰结构、火山尘结构等和假流纹状、斑杂状、火山泥球状、层理状等构造。分为两大类型：①熔结火山碎屑岩。由火山碎屑物经熔结而成。通常火山碎屑物含量大于90％。包括熔结集块岩、熔结角砾岩、熔结凝灰集块岩和熔结凝灰岩等。②正常火山碎屑岩。由火山碎屑物质经一定的压实作用形成。包括集块岩、火山角砾岩、火山凝灰角砾岩和凝灰岩等。其中凝灰岩分布最广。此外，火山碎屑岩与熔岩和正常沉积岩之间还存在一系列过渡类型。广义上，含火山碎屑物质大于10％的岩石都可称作火山碎屑岩。与火山碎屑岩有关的矿产有各种金属和非金属矿产（如Fe、Cu、Pb、Zn、S、B等）。如中国甘肃的白银厂铜矿床、镜铁山铁矿床等。 |
说明：补充资料仅用于学习参考，请勿用于其它任何用途。