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碎裂带
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  shattered zone
     The fenite is characterized by a zonation pattern in the sequence of shattered zone, aegirine and aegirine-augite zone, and arfvedsonite zone from o utside to the center.
     围绕碳酸岩杂岩广泛发育着霓长岩化 ,蚀变作用形成的霓长岩具有明显的分带特征 ,由内向外可分为 :钠铁闪石黑云母带、霓石霓辉石带、碎裂带
短句来源
  “碎裂带”译为未确定词的双语例句
     Cataclastic-altered granite type uranium deposit is one of the main prospecting objects inour country at present.
     碎裂蚀变花岗岩型铀矿床是当前我国找矿的主攻方向之一,它具有大碎裂带、以交代作用为特征的大蚀变带。
短句来源
     and in the more shallow level,has a series of breccia and high angle normal faults.
     在浅部构造层次上以碎裂带及高角度正断层为主。
短句来源
  相似匹配句对
     a. zone, E.
     C,E.
短句来源
     centrifugus zone,C.
     sakmaricus—C.
短句来源
     and in the more shallow level,has a series of breccia and high angle normal faults.
     在浅部构造层次上以碎裂及高角度正断层为主。
短句来源
     NUCLEAR MULTIFRAGMENTATION
     原子核的多重碎裂
短句来源
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  shatter belt
The Shatter Belt and the European Core - A Geopolitical Discussion on the Untypical Case of Slovenia
      
The paper is focussing primarily on the European Shatter Belt, formerly known as 'Eastern Europe'.
      
This is the decision of the member states of the European Union and NATO to incorporate some/several states of the Shatter Belt into their own zone of protection and/or federation.
      
  cataclastic zone
These veins roughly parallel the trend of the Ivanhoe Lake Cataclastic Zone.
      
A significantamplification (by a factor of 10 around 10 Hz) isobserved also at one of the rock sites, possibly dueto the presence of a cataclastic zone related to theactivity of a regional fault that altered themechanical properties of the rock.
      
In addition the behaviour of the interface between the intact rock and the cataclastic zone is studied by direct shear tests.
      
  shattered zone
Pressure wave amplitudes in an near the shattered zone of an underground explosion measured by piezophotographic method
      
Statistical determination of the law of dispersion of marking material in the shattered zone
      


The East Asian complex tectonic Iandform js the couple system of the East Asian tectonic landform formed by the Eurasian plate under the control of the field of the compound force engendered by the pushing and extrusion between the India-Australian plate and the Pacific plate. From inland to continental margin it can be separated Like this. Fault-splitting Zone; Broken-splitting Zone, and Separation-splitting Zone.

东亚复杂的构造地貌格局,是欧亚板块在太平洋板块和印—澳板块推挤作用产生的复合应力场的控制下,构成的东亚构造地貌力偶体系。陆内至陆缘可划分为:断裂带、破裂带和碎裂带

Cataclastic-altered granite type uranium deposit is one of the main prospecting objects inour country at present.It is characterized by large cataclasis and alteration zone and a greatvolume of low grade easily leached ore.The main geologic settings for its formation are upwarping region in the marginal mobile zone of platform or folding belt;doubly controlled bysmall intrusions with intensive autometamorphism within anorogenic multiple granitebatholith and by sandwiched block between two faults or fault intersecting...

Cataclastic-altered granite type uranium deposit is one of the main prospecting objects inour country at present.It is characterized by large cataclasis and alteration zone and a greatvolume of low grade easily leached ore.The main geologic settings for its formation are upwarping region in the marginal mobile zone of platform or folding belt;doubly controlled bysmall intrusions with intensive autometamorphism within anorogenic multiple granitebatholith and by sandwiched block between two faults or fault intersecting area;region withdevelopment of acidic or alkali alteration and region of negative relief,unconformably coveredby red beds and superimposed by supergene enrichment process.Emphasis should be placedon the in-situ leaching experiment and economic-technical evaluation in prospecting process.

碎裂蚀变花岗岩型铀矿床是当前我国找矿的主攻方向之一,它具有大碎裂带、以交代作用为特征的大蚀变带。低品位大矿量易浸出的特点。该类型矿床形成的主要地质条件是:地台边缘活动带或褶皱带的花岗岩隆起区;受非造山的大复式花岗岩基内自变质作用发育的小岩体和双断裂夹持区或断裂构造结的双重控制;酸交代或碱交代蚀变发育区;红层不整合覆盖、负地形、表生叠加富集区。同时,强调了在找矿过程中要加强地浸试验和经济技术评价。

Based on the field geological structure mapping,carefully observation of microstructure,in the copper mine of Zhongtiao Mountain,Shanxi,Zhongtiao group has experienced multiple deformations in early - middle Proterozoic era. The three episode extensional structures were the features of the denudational fault in the different level of the crust. The subhorizontal shear zone exists in the deep structural level; in the middle level,we can see mylonite to microbreccia;and in the more shallow level,has a series...

Based on the field geological structure mapping,carefully observation of microstructure,in the copper mine of Zhongtiao Mountain,Shanxi,Zhongtiao group has experienced multiple deformations in early - middle Proterozoic era. The three episode extensional structures were the features of the denudational fault in the different level of the crust. The subhorizontal shear zone exists in the deep structural level; in the middle level,we can see mylonite to microbreccia;and in the more shallow level,has a series of breccia and high angle normal faults.

通过对山西中条山铜矿区进行详细构造测量和显微构造观察,认为中条山地区早、中元古代经历了多期变形的叠加改造。三期伸展构造分别标志着剥离断层在地壳不同构造层次上的特征。在深部构造层次上表现为近水平的韧性剪切带;在中部构造层次以脆─韧性变形过渡性为标志;在浅部构造层次上以碎裂带及高角度正断层为主。

 
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