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韧性剪切断裂带
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  “韧性剪切断裂带”译为未确定词的双语例句
     The Baoban gold ore belt occurs in the contact zone of the Middle Proterozoic granite on the western side of the Gezhen brittle-ductile shear fault.
     抱板金矿带产于戈枕脆韧性剪切断裂带西侧中元古代花岗岩体内接触带上.
短句来源
  相似匹配句对
     THE BASEMENT DUCTILE SHEAR ZONE OF THE MIDDLE YIHE-SHUHE FAULT BOET
     沂沭断裂带中段基底韧性剪切
短句来源
     Mineralization of gold by dynamics was first presented by the author.
     是脆性断裂带控金,而非韧性剪切带控金。
短句来源
     SHEAR BAND BIFURCATION IN DUCTILE MATERIALS
     韧性材料的剪切带状分叉
短句来源
     Some evidence shows that in anearly stage the fracture zone was a ductile shear zone.
     许多证据表明这断裂带的早期阶段是一条韧性剪切带。
短句来源
     Determination of the formation temperature of the earlier ductile shear zone in the Tan-Lu fault zone,eastern Dabie Mountains
     大别山东缘郯庐断裂带早期韧性剪切带的形成温度
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W-Sb-As-Au ore deposits are mainly occurred in tenacity shear structural zone of low grade metamorphic rocks of Proterozoic Erathem, and are controlleb by stratigraphy hor-rizon and structures.

钨锑砷金矿床主要赋存于元古界线变质岩系之韧性剪切断裂带内,受地层层位和构造控制。 金为自然金,主要呈显微和次显微粒状,以机械混入物或微包体赋存于硫(砷)矿物裂隙、晶隙间和晶面上。 成矿作用是在晚元古代火山—碎屑沉积矿源层的基础上,经变质溶液,在中低温偏低盐度和中偏弱酸性条件下完成的。属火山沉积—变质热液型矿床,主要成矿期为加里东早期。 安化-溆浦-洪江深大断裂两侧的元古代地层中韧性变形带是主要找矿对象。

The Longwangjiang mineralized zone consists of about 80 antimony-gold quartz veins,hosted in ductile shear zone within the upper part of Wuqianxi Formation. Banxi Group. The quartz veins are various in dimension, and different in gold content.The gold enrichment is closely connected with metal sulfide(or arsenide). and arsenopyrite is the main gold-bearing mineral. The silisification and arsenopyritization within the decolored zone are the indicators for near-ore wall rocks, and arsenic is their typomorphic...

The Longwangjiang mineralized zone consists of about 80 antimony-gold quartz veins,hosted in ductile shear zone within the upper part of Wuqianxi Formation. Banxi Group. The quartz veins are various in dimension, and different in gold content.The gold enrichment is closely connected with metal sulfide(or arsenide). and arsenopyrite is the main gold-bearing mineral. The silisification and arsenopyritization within the decolored zone are the indicators for near-ore wall rocks, and arsenic is their typomorphic element.

矿带主要赋存于板溪群五强溪组上段之韧性剪切断裂带内,由近80条规模不等、含金性不一的锑金石英脉组成。金的富集与金属硫(砷)化物关系密切,毒砂是其主要载金矿物。褪色带内硅化、毒砂化是近矿围岩标志,砷是其标型元素。

The Baoban gold ore belt occurs in the contact zone of the Middle Proterozoic granite on the western side of the Gezhen brittle-ductile shear fault. There exist three types of gold deposits,i.e., shear altered rock type, quartz vien type and auriferous pegmatite type, with the first type being most important. The Pb, S, H, O, Rb-Sr isotopic data and fluid inclusion studies show that different gold deposits were formed in different geological epoch.es, thus exhibiting polyphase ore-forming features: pegmatites...

The Baoban gold ore belt occurs in the contact zone of the Middle Proterozoic granite on the western side of the Gezhen brittle-ductile shear fault. There exist three types of gold deposits,i.e., shear altered rock type, quartz vien type and auriferous pegmatite type, with the first type being most important. The Pb, S, H, O, Rb-Sr isotopic data and fluid inclusion studies show that different gold deposits were formed in different geological epoch.es, thus exhibiting polyphase ore-forming features: pegmatites and quartz veins were formed in Hercynian period, and their ore-forming substances and hydro-thermal soluion were mainly derived from Hercynian magma; mylonite type gold mineralization in the ductile shear zone took place in Indosinian period; shear altered rock type deposits were formed in Yanshanian period, and their ore-forming materials and hydrothermal solution were mainly derived from the same deep magma as the Yanshanian andesitic basalt porphyrite, with the addition of meteoric water and materials from the Middle Proterozoic granite and sedimentary sequence.

抱板金矿带产于戈枕脆韧性剪切断裂带西侧中元古代花岗岩体内接触带上.有剪切带蚀变岩型、石英脉型和含金伟晶岩型三种主要类型的矿床,以前一类最为重要。经多年研究认为,不同类型矿床的成矿时代不同,具多期成矿的特点。含金伟晶岩型和石英脉型金矿形成于海西期,成矿物质主要来自同期岩浆热液,含金剪切带的糜棱岩型金矿化发生于印支期;剪切带蚀变岩型金矿床形成于燕山期,成矿物质主要来自于与燕山期安玄玢岩同源的深部岩浆,但有大气水和老岩体及地层物质加入。

 
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