- 更多网络例句与碎砾岩相关的网络例句 [注：此内容来源于网络，仅供参考]
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The former includes fault breccia and fault gouge which are characterized by loose consolidation of fractured rock fragment s.
前者包括断层角砾岩、断层泥，这类断层岩由碎裂的岩屑松散地聚集在一起。
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The former includes fault breccia and fault gouge which are characterized by loose consolidation of fractured rock fragments.
前者包括断层角砾岩、断层泥，这类断层岩由碎裂的岩屑松散地聚集在一起。
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The former includes fault breccia and fault gouge which are characterized by loose consolidation of fracture d rock fragments.
前者包括断层角砾岩、断层泥，这类断层岩由碎裂的岩屑松散地聚集在一起。
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The Laojunshan conglomerate is a suite of continental coarse clastic rocks consisting of conglomerate and graywacke.
老君山砾岩是一套由砾岩和杂砂岩组成的陆相粗碎屑岩。
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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。
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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。
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According to core observation and description, many deformation structures with seismite characteristics are recognized within sandstone and shale sedimentary strata of Paleogene continental faulted basin in Yangxin Subsag, such as micro-faults, earthquake fissures, liquefaction sandstone veins, water-escape structure, vibrational liquefaction deformation structure, seismic pillow structure and associated structure, etc. The vertical sequence of seismites in Yangxin Subsag, in ascending order, is underlying unshocked layer, micro-faults layer, autoclastic shattered breccia layer, vibrational liquefaction deformation structure layer, seismic pillow structure and associated structure layer, liquefied homogeneous layer and overlying unshocked layer, which corresponds to different earthquake intensity respectively.
通过岩心观察和描述，在阳信洼陷古近系陆源碎屑断陷湖盆砂泥质沉积地层中识别出大量具有震积岩特征的变形构造，如微断层和震裂缝、水下岩脉和泄水构造、振动液化卷曲变形构造、震积枕状层及伴生构造等，同时建立了阳信洼陷震积岩垂向序列，自下而上分别是下伏未震层段、微断层层段、震碎角砾岩段、振动液化卷曲变形层段、震积砂枕及伴生构造层段、液化均一层段和上覆未震层段。
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Fracturing of mineralization stage is found mainly concentrated in the early quartz veins or the hydrofracturing breccia in the sandy tectonic lenses, the lens-like orebody mainly consisting of the cataclastic quartz veins and hydrofracturing breccia form.
成矿阶段的破裂主要集中在砂岩构造透镜体中早期石英脉或液压角砾岩上，形成以碎裂石英脉及液压角砾岩为主要矿化母岩的透镜状矿体。
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Upper fans mainly consist of conglomerates which can be genetically classified as debris flow, braided stream and sheetflood flow deposits.
其中的扇根主要由砾岩组成，按其成因包括碎屑流、颗粒流、片流及河道砾岩等数种沉积。
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At least, three types of earthquake related fault rocks including pseudotachylyte formed by typical fast fault movement, no orientated ultra-cataclasite or sinter breccias may formed by weak earthquake faulting, and stockwork microbreccias formed by autochthonous powerful shock at the source are discovered, in which some of the original sources parameters are remained.
至少区分出三种地震断层产物和两种震源破裂方式：典型快速地震断层形成的假玄武玻璃；或许与弱震有关的无组构超碎裂岩或熔结角砾岩，以及强烈原地震动成因的网脉状微角砾岩。
- 更多网络解释与碎砾岩相关的网络解释 [注：此内容来源于网络，仅供参考]
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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.
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autoclastic breccia：自生碎屑角砾岩
autoclast 自生碎屑 | autoclastic breccia 自生碎屑角砾岩 | autoclastic melange 自生碎屑混杂岩
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cataclastic：压碎的,碎裂的
动力变质破裂碎屑,残碎斑晶 cataclast | 压碎的,碎裂的 cataclastic | 压碎角砾岩,碎裂角砾岩 cataclastic breccia
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cataclastic metamorphism：压碎变质,碎裂变质作用
压碎砾岩,碎裂砾岩 cataclastic conglomerate | 压碎变质,碎裂变质作用 cataclastic metamorphism | 压碎岩,碎裂岩 cataclastic rock
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cataclastic conglomerate：碎裂砾岩
cataclastic breccia 压碎角砾岩 | cataclastic conglomerate 碎裂砾岩 | cataclastic fabric 碎裂组构
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cataclastic conglomerate：压碎砾岩
压碎矿石 crushed ore | 压碎砾岩 cataclastic conglomerate | 压碎砾岩 crush conglomerate
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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
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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
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crush conglomerate：压碎砾岩
压碎砾岩 cataclastic conglomerate | 压碎砾岩 crush conglomerate | 压碎面 crush plane
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crush plane：压碎面
压碎砾岩 crush conglomerate | 压碎面 crush plane | 压碎强度 crushing strength