角砾岩

基本解释 (translations)

breccia

与角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)。

Sub-volcanic rocks include andesitic porphyrite, rhylitic porphyry, cryptoexplosive breccia as well as autobreccia etc.(2) Volcanic lithofacies——through the observation of cores, identification of thin sections and interpretation of well logs and seismic data, there are 8 kinds of lithofacies for the volcanic rocks of Yingcheng Formation are identified: fallout facies, effusion facies, pyroclastic flow facies, base surges facies, lahar facies, eruption-sedimentary facies, subvolcanic facies and extrusion facies.(3) Three types of eruption——i. e. explosion, effusion and surge.(4) Two kinds of eruptive environments——Subaerial (e. g. volcano in Well Shangshen 3) and subaqueous .(5) Three remarkable volcanic apparatus in Shengping-Wangjiatun area——layered, micro-shield and cone volcanoes according to volcanic processes and lithofacies distribution.

次火山岩有安山玢岩、流纹斑岩、隐爆角砾岩及自碎角砾岩等；(2)火山岩相——通过岩芯观察、镜下鉴定、测井与地震资料解释，营城组火山岩中发育8种岩相类型，即爆发空落相、溢流相、火山碎屑流、基底涌流相、喷发沉积相、火山泥石流相、侵出相和次火山相等；(3)火山喷发的形式——有爆发、溢流和涌流三种；(4)火山喷发环境——有陆上(如尚深3井火山)和水下两种；(5)火山机构类型——根据火山作用特点和岩相分布特征，在升平—汪家屯地区识别出三类截然不同的火山机构，即层火山、微型盾火山和渣锥火山。

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。

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。

与角砾岩相关的网络解释 [注：此内容来源于网络，仅供参考]

volcanic breccia：火山角砾岩 火山角礫岩

■ volcanic bomb 火山弹 火山弾 | ■ volcanic breccia 火山角砾岩 火山角礫岩 | ■ volcanic chain 火山群(链) 火山列

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

desiccation breccia：干裂角砾岩

desiccating agent 干燥剂 | desiccation breccia 干裂角砾岩 | desiccation conglomerate 干裂砾岩

founder breccia：崩陷角砾岩

崩陷角砾岩 collapse breccia | 崩陷角砾岩 founder breccia | 崩陷坑 slump pit

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

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"

brecciate：合成角砾岩

7. impact crater陨石坑,撞击火山 | 8. brecciate合成角砾岩 | the zone of brecciation角砾岩地带

brecciate：作成角砾岩

breccia 角砾岩 | brecciate 作成角砾岩 | bred in the bone 根除不了的