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1)  Dabeiwu area
大背坞地区
1.
In this paper, the authors first elaborate on macroscopic and microscopic features of the ductile shear zone in epimetamorphic rocks of Dabeiwu area, and classify the tectonite in it.
以江西大背坞地区为例,阐述了在浅变质碎屑岩中鉴别韧性剪切带的标志,提出这种变形的构造岩的分类方案,同时对大背坞地区韧性剪切带进行应变测量和剪切位移估算,最后在岩石组构特征和综合分析基础上指出这种韧性变形机制是粒间滑动和粒内变形,其形成深度5~8km、温度250~350℃、压力010~020GPa,是一种发育在地壳浅层次的低温低压条件下的韧性变形,其变形变质作用相当于低绿片岩相。
2.
The mottled structure in the Dabeiwu area can be classified into syngenetic fragments and porphyroblasts, including seven types.
大背坞地区的斑点构造分为同生碎屑和变斑晶两大类共7种。
3.
The syntectonic porphyroblasts of pyrite and siderite in the ductile shear zone developed in epimetamorphic clastic rocks in Dabeiwu area are the products and marks of ductile shear deformation during progressive metamorphism.
大背坞地区浅变质碎屑岩内的韧性剪切带中发育有同构造成因的菱铁矿变斑晶和黄铁矿变斑晶,它们是进变质剪切变形的产物和标志。
2)  Dabeiwu
大背坞
1.
Study on Geochemistry of Dabeiwu Gold Deposit,Jiangxi Province;
江西大背坞金矿床地球化学研究
3)  Ciwu area
次坞地区
4)  Dabeiwu gold ore field
大背坞金矿田
1.
This article discusses tectonic deformation facies of controlling miner and the relationship between it and metallogenic in Dabeiwu gold ore field.
以面线理构造为依据,结合相关的岩矿测试结果,论述了大背坞金矿田控矿构造变形相及其与成矿的关系,并从大地构造演化体制探讨了其成矿机制。
2.
By study on the features of foliation and lineation structures in the Dabeiwu gold ore field in Jiangxi Province,with correlative rock and mineral testing,the structural deformation facies are established corresponding to the regional tectonic development.
依据大背坞金矿田控矿构造带中面、线理构造特征,结合相关的岩矿测试结果,建立了与区域构造发展相对应的构造变形相,分析了其与成矿的关系。
3.
According to the feature of folia-lineation structure and related mineral test results,this article makes a tectonic analysis about the tectonic belt of controlling mineral in Dabeiwu gold ore field reasonably,establi- shes tectonic deformation facies corresponding to Regional tectonic development,analyzes the relationship between the tectonic belt of controlling mineral and metallogenic.
本文依据面线理构造特征和相关的岩矿测试结果,对大背坞金矿田控矿构造带进行了合理的构造解析,建立了与区域构造发展相对应的构造变形相,分析了其与成矿的关系。
5)  Geological background areas
地质背景区
1.
To effectively formulating the animal feed for cattle this study analyzed the concentration of potassium,magnesium,copper,zinc,manganese,cobalt,iron,selenium and iodin in rock,soil and forage from the main ruminant production bases,which belong to six different geological background areas in Yunnan province,China.
对云南省反刍家畜主要生产基地所属的6个地质背景区的土壤、岩石和饲料样品的钾、镁、铜、锌、锰、钴、铁、硒和碘等9种元素进行分析测定,结果表明:土壤和饲料中大多数矿物质元素含量在玄武岩(Ⅴ)和碳酸岩红壤区(Ⅰ)相对较丰富;碳酸岩盐、碎屑岩和玄武岩混合型黄红壤区(Ⅱ)居中;而由碎屑岩(Ⅲ)和变质岩(Ⅵ)发育的土壤区土壤和饲料中元素含量相对最低。
6)  A surrounding area; a background.
背景周围的地区;背景
补充资料:太平洋地区标准会议标准(见太平洋地区标准会议)


太平洋地区标准会议标准(见太平洋地区标准会议)
standards of PASC: see Pacific Area Standards Congress; PASC

Ta iPingyang Diqu Bioozhun Hu呼ib沁幻Zhun太平洋地区标准会议标准(s切md田心sofR巧C)见太平洋地区标准会议。
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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