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   韧性剪切 在 矿业工程 分类中 的翻译结果: 查询用时:0.044秒
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韧性剪切     
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  ductile shear
    A NEW VIEWPOINT──IRON ORE DEPOSIT─CONTROLD BY DUCTILE SHEAR ZONES AT WAITOUSHAN
    本溪歪头山铁矿控矿构造的新认识──韧性剪切带的控矿作用
短句来源
    DUCTILE SHEAR ZONE AND THE RELATIONSHIP WITH GOLD DEPOSITS IN SHENGLIDABAN GOLD FIELD, XINJIANG
    新疆胜利达坂金矿区韧性剪切带与金矿关系
短句来源
    CHARACTERISTICS AND STUDY SIGNIFICANCE OF STRUCTURAL DEFORMATION IN DUCTILE SHEAR ZONE OF SHANMEN SILVER ORE DISTRICT,SIPING, JILIN PROVINCE
    吉林四平山门银矿区韧性剪切带构造变形特征及研究意义
短句来源
    CHARACTERISTICS AND ORE—CONTROLLING PROCESS OF DUCTILE SHEAR ZONES IN THE TNAJIANSHAN GOLDFIELD
    滩间山金矿田韧性剪切带特征及其对金矿的控制作用
短句来源
    A STUDY OF INCLUSIONS FROM THE DUCTILE SHEAR BELT TYPE GOLD DEPOSITS IN HUANGTULING,HENAN
    河南鲁山黄土岭韧性剪切带型金矿床包裹体研究
短句来源
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  ductile shearing
    GEOLOGICAL CHARACTERISTICS OF DUCTILE SHEARING ZONE TYPE Au DEPOSITS AND ORE-SEACHING DIRECTION IN THE SOUTH BELT, BEISHAN REGION, GANSU PROVINCE
    甘肃北山南带韧性剪切带型金矿床(点)地质特征及找矿方向
短句来源
    Further quantitative calculations demonstrate that during the ductile shearing,gold was leached out of the wall rocks and then concentrated in the central part of the Shear zone together with gold carried by the external flulds.
    进一步的定量计算表明,韧性剪切过程中,Au从围岩中淋失,并与外来流体所携带的Au一起,在剪切中心带富集。
短句来源
    The paper discusses geological features of Dexing nappe structure and its orecontrol significance and builds a polygenetic metallogenic model in which gold deposit and porphyry copper deposits are controlled by the ductile shearing nappe structure.
    论述了德兴推覆构造的地质特征及控矿意义。 建立了以韧性剪切为特征的推覆构造控制金矿和斑岩铜矿的多因复成成矿模式。
短句来源
    During ductile shearing action, the compress is high (△Vr <0) and the mineralization didn't occur.
    在韧性剪切阶段,围压较大,△Vr<0,不能产生流体压力,也不能形成金矿化;
短句来源
    All of these show that Xilekuola is a promising area to find large-middle scale gold deposit of tectono-fractured alteration rock type or ductile shearing zone type.
    所有这些都说明,希勒阔腊是寻找构造破碎蚀变者型或韧性剪切带型大、中型金矿的有利地区。
短句来源
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  the ductile shear
    A STUDY OF INCLUSIONS FROM THE DUCTILE SHEAR BELT TYPE GOLD DEPOSITS IN HUANGTULING,HENAN
    河南鲁山黄土岭韧性剪切带型金矿床包裹体研究
短句来源
    TECTONO GEOCHEMICAL CHARACTERISTICS OF THE DUCTILE SHEAR ZONE TYPE GOLD DEPOSIT IN KANGGUL,XINJIANG
    康古尔韧性剪切带型金矿构造地球化学特征
短句来源
    TECTONIC CHARACTERISTICS OF THE DUCTILE SHEAR ZONE IN MAOPAI GOLD DEPOSIT AREA, JIANGXI PROVINCE, CHINA
    江西茅排金矿床含金韧性剪切带构造特征
短句来源
    GEOLOGICAL CHARACTERISTICS AND GENESIS OF THE DUCTILE SHEAR ZONE TYPE GOLD DEPOSIT IN MATOUTAN EASTERN TIANSHAN
    东天山马头滩韧性剪切带型金矿地质特征及成因
短句来源
    MINERALIZATION SIGNIFICANCE OF GEOCHEMICAL BARRIER ON THE DUCTILE SHEAR BELT IN THE TIANWAN GOLD DEPOSIT,SHIMIAN,SICHUAN PROVINCE
    四川石棉田湾金矿床韧性剪切构造带地球化学障的成矿意义
短句来源
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  ductile sheer
    THE FEATURES OF THE GOLDCONTAINING DUCTILE SHEER ZONEAND THE GOLD MINERALIZATION IN 210# GOLD DEPOSIT
    210金矿床含金韧性剪切带特征与金矿化
短句来源
    The former is controlled by a ductile sheer zone, while the latter is controlled by a brittle-ductile fault.
    前者是韧性剪切带控矿,后者是脆—韧性断裂控矿;
短句来源
    The regionnal large ductile sheer belt controls the distribution of theore zone or are field, the secondary brittle faults control the range of the ore deposit and the local interlagerfracture zone and faults fracture control the sites of the ore bodies.
    区域性大型韧性剪切带控制金矿带、金矿区的展布,地区性二级脆性断裂控制金矿床的范围,局部的更次级层间破碎带、断裂裂隙带控制矿体的就位。
短句来源
    210# gold deposit is a nwe type gold deposit discovered in 1980.The hosting strata is tuffdite of Jinwozi Group of the upper Devonian sevies,the deposit is located in the ductile sheer zone.
    210金矿床为80年代发现的新金矿类型。 赋矿地层为上泥盆统金窝子组层凝灰岩,定位于矿区的韧性剪切带中。
短句来源
    By studying the macroscopic and microscopic features,the alteration and the geochemical characteristics of 210# sheer zone,it is shown that the enrichment and formation of gold mineralization is closely related with the stress evolution of 210# sheer zone. The gold mineralization mainly occurred in the formation stage of migmitization and alteration in the second period of the ductile sheer zone and was further enriched by the deformation of NE-SW anticlockwise strikeslip ductil sheering in the third period. 
    对210剪切带的宏观特征、微观特征、蚀变特征和地球化学特征的研究,揭示金矿化的形成、富集与210韧性剪切带应变演化过程密切相关,金矿化主要发生在第二期韧性剪切带形成糜棱岩化岩石、蚀变岩石阶段,第三期NE-SW左行走滑脆-韧性剪切变形阶段使金矿化进一步富集。
短句来源

 

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  ductile shear
These rocks occur exclusively in high-temperature ductile shear zones, which can develop either during the primary exhumation of rock complexes or during the overprinting by high-temperature dynamometamorphism.
      
Ductile shear zones developed in Archean granulite gneisses simultaneously with their exhumation, and, hence, their P-T trajectories are segments of decompression and/or isobaric cooling paths.
      
Straight gneisses in Proterozoic polymetamorphic complexes commonly compose high-temperature ductile shear zones overprinted on Archean granulite complexes, and the P-T paths of these rocks are Z-shaped.
      
Such ductile shear zones commonly have a strike-slip morphology and can be easily seen in aerial photographs and discerned during structural geological surveying.
      
Fluid participation in ductile shear zone: Evidence from geological, geochemical and13O/16O relations from south part of Tanchen
      
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  ductile shearing
The Duolanasayi gold deposit, 60 km NW of Habahe County in Xinjiang, is a medium-large scale gold deposit controlled by the coupled ore-forming processes involving brittle-ductile shearing, albitite veins, and post-stage magma solution.
      
The Duolanasayi gold deposit, 60 km NW of Habahe County, Xinjiang Uygur Autonomous Region, is a mid-large-scale gold deposit controlled by brittle-ductile shearing, and superimposed by albitite veins and late-stage magma hydrothermal solutions.
      
The second and main stage of gold mineralization was associated with renewed ductile shearing during D2.
      
To the south-west, in the Hornachos sector, large-scale recumbent folds associated with ductile shearing can be seen.
      
Later Devonian amphibolite-facies metamorphism caused ductile shearing of the pegmatites, leading to partial recrystallisation of pegmatitic material.
      
更多          
  the ductile shear
Jingshan superlarge gold deposit is a typical deposit closely related to the ductile shear zone, developing the economic enrichment during the transition form the ductile deformation to the brittle deformation.
      
The40Ar/39 Ar plateau ages, K-Ar date of K-feldspar and other geochronologic information suggest that the exhumation rate of the ductile shear zone is about 0.18-1.12 mm/a in the range of 107-70 Ma, which is mainly influenced by tectonic extension.
      
These kinds of shear types only produce a/ab strain facies, so the lineation in the ductile shear zone could not deflect 90° in the progressively deformation.
      
The present profile of the ductile shear zone with consistent SW-dipping mineral elongation lineation shows antiform and reversed S-shape from northeast to southwest respectively.
      
Exposure structures, microstructures and quartz C-axis fabric all indicate top-to-SW movement for the ductile shear zone.
      
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