硒是湘黔汞矿带标型微量指示元素。
Selenium is the guide trace element in the western Hunan - eastern Guizhou mercury deposit.
深断裂或区域性大断裂控制了矿带部位。
铜矿分西矿带和东矿带。
武夷山稀有、贵金属矿带受ne向构造岩浆岩带控制。
Wuyishan rare and precious metal ore belt is controlled by NE trend tectonic-magmatite belt.
勒青拉铅锌多金属矿床位于冈底斯成矿带东段北矿带。
Leqingla Pb-Zn polymetallic deposit is located in the northern part of the eastern Gangdise metallogenic belt.
所以他大部分时间都在新矿带的西边界采集矿物标本。
So he spent most of his time collecting mineral samples from the western boundary line of the new frontier.
矾山岩浆的三相不混溶作用导致了矾山三个矿带的形成。
The three phase immiscibility of Fanshan magma resulted in the formation of three phosphorus ore zones.
研究区米粮金矿位于南秦岭地区金龙山矿带金龙山矿段。
The study area is located Minliang Gold Mine of Jinlongshan ore belt in the southern Qinling area.
北西向紧密线型褶皱、断裂及其次级构造控制矿带的展布。
The NW-trending tight linear folds and fractures and their secondary structures control the distribution of the ore belt.
两个矿带成矿作用的差异，主要与所处的区域地质背景不同有关。
The difference of these two belts in mineralization is mainly related to the different regional geological setting.
内蒙古东部的黄岗-甘珠尔庙矿带是地处大兴安岭南段的锡乡金属矿带。
The Huanggang-Ganzhuermiao ore belt of east Inner Mongolia is tin-polymetallic ore belt in Southern Da Hinggan Mountains.
本文以华蓥山锶矿带为例，介绍了运用GIS技术进行矿产预测的方法。
This paper introduces the application of GIS to prediction of mineral resources by taking the Huayingshan Sr mineralization belt as an example.
青海省阿尔金成矿带成矿地质条件优越，矿产资源丰富，具有很大的找矿潜力。
Aerjin metallogenic belt in Qinghai Province has superior ore-forming geological condition, abundant mineral resource, and the great ore prospecting potential.
武山铜矿南矿带采用上向水平分层进路水砂充填法回采，采场多次发生冒顶、片帮。
The South ore-bearing zone of Wushan copper mine is mined with ascending horizontal slicing hydraulic fill crosscut mining system. Roof falling and rib spalling occurred in any times.
深断裂带、大型剪切带及其旁侧的褶皱及断裂裂隙系统控制矿带、矿区、矿床和矿体。
The ore belts, mining area, deposits and ore-bodies are all controlled by the deep faults, large scale shear zones and the fold and fault-crack system aside.
通过分析金岭矿区区域构造及矿床地质特征，认为矿区矿床存在岩浆岩控矿带成矿特征。
Through analyzing the regional construction and deposit characteristics of Jinling diggings, it is considered that the deposit has characteristics of ore forming of magma rock-controlling belt.
通过分析东姚矿区地质构造及矿床地质特征，认为矿区矿床存在岩浆岩控矿带成矿特征。
Through analyzing the regional construction and deposit characteristics of Jinling diggings, it is considered that the deposit has characteristics of ore forming of magma rock-controlling belt.
对矿带内矿田地质和控矿构造的调查表明，本区的层控加热液改造型矿床与成矿构造关系密切。
Study of the ore-field geology and ore-controlling structure in the ore belt indicates that the stratabound plus hydro...
矿带级地球化学场中环带结构控制了元素的成矿区间，带状结构的局部区段构成相应的工业矿体。
The encircling texture in ore zone geochemical field control minerogenetic area, and local zone of zoning texture constitutes corresponding productive ore body.
简述了铲运机出矿的下向进路式水砂充填采矿法的主要技术特点和在武山铜矿北矿带的成功应用。
This paper describes main technical characteristics of underhand drift hydraulic sand filling method and its successful application at North Part of Wushan Copper Mine.
前者以黄铁绢英岩化为主，产于牛心山复式侵入体的内接触带，空间上形成一个近于闭合的含矿带；
The former mainly is the pyrite silky mica-quartzite, it is discovered in internal connection belt of compound irruptive rock and forms a closed mineral belt in space;
在主矿带外围，一些低缓磁异常以及主矿带东部以0 ~ 50伽玛圈闭的局部磁异常，应引起足够重视。
Some weak magnetic anomalies in the periphery of major ore belt, and local 0-50 gamma trap anomalies in the eastern part of the major ore beh should be taken into account adequately.
在此基础上对控制成矿带、矿田及矿床的构造特征进行了分析，总结了带内矿床定位的两类构造组合形式。
After analyzing structure characteristics controlling metallogenic belt, ore field, and deposits, two structure assemblage styles for ore depositing have been summarized.
始态可概括为源区、源岩、库岩、矿源层和剥蚀区等，终态可以概括为矿带、矿田和矿床等多个等级体制。
The initial state can be summarized as source region, source rock, reservoir rock, source bed, a denudation area, etc.
作者对产自云南马关-麻粟坡矿带、广西钟山八步矿区的黑色电气石进行了矿物组成及化学成分的分析测试。
It shows that there are apparent differences in black tourmalines mineral components and chemical elements from their different producing mines.
蔡凹锑矿位于陕豫锑矿带的西段，为矿带中典型的锑矿床。 其控矿岩系主要为秦岭群中部雁岭沟组石墨大理岩。
The Caiwa middle - sized antimony deposit is located on the western Shanxi-Henan antimony ore belt, The hosting rocks are Yanlinggou Formation graphite marble of the Qinling Group.
蔡凹锑矿位于陕豫锑矿带的西段，为矿带中典型的锑矿床。 其控矿岩系主要为秦岭群中部雁岭沟组石墨大理岩。
The Caiwa middle - sized antimony deposit is located on the western Shanxi-Henan antimony ore belt, The hosting rocks are Yanlinggou Formation graphite marble of the Qinling Group.
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