砾岩

基本解释 (translations)

conglomerate  ·  conglomerated  ·  conglomerates  ·  conglomerating

词组短语

conglomerate rock · bibbey-rock

与砾岩相关的网络例句 [注：此内容来源于网络，仅供参考]

Rheomorphic breccia in the middle segment of the pipe, hydrofracturing breccia in the boundary of the pipe and ...

根据角砾岩的垂直分带特点，该角砾岩筒剥蚀较浅，矿床保存条件良好，具有较大的深部找矿潜力。

The copper-molybdenum ore bodies are controlled by the crypto-explosive breccia pipe and rock body.

铜钼矿体受隐爆角砾岩筒和岩体控制，矿化产在蚀变隐爆角砾岩和硅化带中。

The migration of carbonate breccia wedge also reflects the shifting of the platform margin and the relative sea level changes . Among them , the Guli breccia wedge extended the furthermost distance to the platform , which represents that the platform margin shifted to the platform for the furthermost distance .

碳酸盐岩角砾岩楔的位置迁移反映了台地边缘位置的迁移和海平面相对变化幅度的大小，其中谷立角砾岩舌相对于其他角砾岩楔向台地方向延伸距离最远，代表了台地边缘位置向台地方向迁移的距离最大，张家湾角砾岩楔代表了安尼初期的海平面快速下降。

The migration of carbonate breccia wedge also reflects the shifting of the platform margin and the relative sea level changes. Among them, the Guli breccia wedge extended the furthermost distance to the platform, which represents that the platform margin shifted to the platform for the furthermost distance. The Zhangjiawan breccia wedge represents a rapid sea level falling in the Early Anisian.

碳酸盐岩角砾岩楔的位置迁移反映了台地边缘位置的迁移和海平面相对变化幅度的大小，其中谷立角砾岩舌相对于其他角砾岩楔向台地方向延伸距离最远，代表了台地边缘位置向台地方向迁移的距离最大，张家湾角砾岩楔代表了安尼初期的海平面快速下降。

In Late Jurassic period (159-135Ma), when the orientation of maximum principal compressive stress was NW direction, the Wuzhangshan granite intruded to upward, accompanied the formation of NW trending Sanrenchang and Huangshuian breccia pipe belts; In the Early Cretaceous period (135-120Ma), when the orientation of maximum principal compressive stress was NNW trending, the second stage of Huashan granite intruded to upward, accompanied the formation of NW trending Qiyugou breccia pipe belts; In 120-105 Ma, when the orientation of maximum principal compressive stress changed to NE direction, the gold-bearing quartz veins and gold orebodies in breccia pipes were formed along the NE trending fractures; In the Middle Cretaceous period (105-85 Ma), when the orientation of maximum principal compressive stress was NEE, the NEE trending Leimengou granite porphyry intruded to upward, accompanied the formation of NEE trending Leimengou breccia pipe belts.

在晚侏罗世(159～135Ma)，构造应力场最大压应力方向为NW向，形成了NW走向的五丈山岩体以及NW向展布三人场、黄水庵两个角砾岩带；在白垩纪早期(135～120Ma)，最大压应力为NNW向，形成了花山岩体第二期上侵，并伴有NW向的祁雨沟角砾岩带；其后(120～100Ma)，构造应力场最大压应力方向变为NE向，形成了NE向含金石英脉及角砾岩体中金矿体；最后(100～80Ma)，形成了雷门沟花岗斑岩以及NEE向展布的雷门沟-杨河沟角砾岩带(区域构造应力场的最大主压应力方向为NEE向)。

Seismites can be subdivided into many types,such as seismic corrugated rock,shattered rock,seismic collapse rock,autoclastic breccias,intraclastic parabreccia,liquefied breccia and seismoturbidite rock.

研究区震积岩的岩石类型则主要包括震褶岩、震裂岩、震塌岩、自碎屑角砾岩、自碎屑副角砾岩、液化角砾岩及震浊积岩等。

Collapse breccias in the superficial parts or topside of the hypabyssal pipe are related with the gold-copper mineralization.

角砾岩筒上段的塌陷角砾岩与矿化关系密切，中段的流化角砾岩、边部的水压角砾岩和下段的爆发角砾岩还未出露。

Field survey and laboratory study of the "Zhuzhou conglomerate" at Zhuzhou Village near Dikou Township, Jian′ou City, Fujian, indicate that the "Zhuzhou conglomerate" is neither the basal conglomerate of the pre-Sinian Longbeixi Formation of the Mamianshan Group nor structural brecciate in the pre-Sinian basement, but the basal conglomerate stratigraphically equivalent to the Late Triassic Dakeng Formation (T3d), unconformably overlying the pre-Sinian Dikou Formation.

对发育于福建建瓯市迪口镇竹洲村的&竹洲砾岩&的野外调查和室内研究表明，该砾岩既不是前震旦系马面山群龙北溪组的底部砾岩，也不是构造砾岩，而是相当于晚三叠世大坑组(T3d)层位的底砾岩，不整合沉积在前震旦系迪口组之上。

They are characterize by irregular and subangular with sandy filling or no filling,and some of them are jointable.

经研究，金顶矿区存在两种成因的角砾岩：构造-膏溶角砾岩和底辟-侵位角砾岩。

Some spore-pollen assemblages of late Trias and the youngest zircon of 225Ma were also obtained in this type.Deriveration of the ore is from the upper crust according to the features of trace elements,zircorn U-Pb age and initial value of ~(87)Sr/~(86)Sr.It has not any charateristics of the mantle.

底辟-侵位角砾岩是本次工作新发现的，它在空间上与构造-膏溶角砾岩密切伴生，剖面上呈脉状或火焰状分布，局部呈脉状穿刺于围岩中，其胶结物中含有晚三叠世的孢粉组合，最年青锆石的年龄为225Ma，角砾岩本身是铅和锌的富矿体。

与砾岩相关的网络解释 [注：此内容来源于网络，仅供参考]

brecciation：角砾岩化作用

brecciated 角砾化的 | brecciation 角砾岩化作用 | breccio-conglomerate 角砾砾岩

brecciation：角砾岩化

brecciatedtexture 角砾结构 | brecciation 角砾岩化 | breccioid 似角砾岩的

the zone of brecciation：角砾岩地带

8. brecciate合成角砾岩 | the zone of brecciation角砾岩地带 | 9. mantle地幔

conglomerate：砾岩

1、砾岩(conglomerate)和角砾岩:碎屑岩中大于2mm的颗粒>50%的岩石称为砾岩,如果砾石为棱角状或次棱角状则称为角砾岩. 砾岩和角砾岩的砾石主要由岩屑组成,矿物成分则多为石英和燧石,胶结物可为泥质、铁质、钙质、硅质等.

founder breccia：塌积角砾岩,崩陷角砾岩

地基土壤 foundation soil | 塌积角砾岩,崩陷角砾岩 founder breccia | 岩浆蚀顶作用 foundering

pudding stone：圆砾岩;布丁砾岩

"钒铋矿","Pucherite" | "圆砾岩;布丁砾岩","pudding stone" | "球粒花冈岩","pudding granite"

cataclastic conglomerate：压碎砾岩,碎裂砾岩

压碎角砾岩,碎裂角砾岩 cataclastic breccia | 压碎砾岩,碎裂砾岩 cataclastic conglomerate | 压碎变质,碎裂变质作用 cataclastic metamorphism

conglomeratic：砾岩状

conglomeratetubercleofchoroid脉络膜集合结节 | conglomeratic砾岩状 | conglomeraticmudstone类砾岩 副砾岩

pseudoconglomerate：假砾岩;自碎屑砾岩

pseudoconformity 假整合 | pseudoconglomerate 假砾岩;自碎屑砾岩 | pseudocorposclerotinite 假浑圆菌质体

crush breccia：圧砕角砾岩","破砕角砾岩

1235,"cross-stratification","斜交层理" | 1236,"crush breccia","圧砕角砾岩","破砕角砾岩" | 1237,"crushed stone","砕骨物"