石英脉金，是岩金的一个重要类型。
The quartz vein of gold-bearing is an important type in rock-gold.
乱泥沟矿区第四系砂金矿产丰富，是寻找岩金的有利靶区。
The Luannigou ore field riches with alluvial gold of Quaternary Period and is the favorable target for rock gold.
青海省岩金的分布受四个成矿亚带控制，分布上呈现九个矿化集中区。
The distribution of the gold deposits in Qinghai province is mainly controlled by four sub belts of mineralization and fault structure along NWW EW trending.
砂金样品则以较富集轻稀土为特征，稀土元素含量继承了岩金的部分特点。
Placer gold samples are rich in light REE, the characteristics of REE contents of which partly inherited from hard rock gold.
并以这种认识规律在嘉荫凹陷周边进行岩金找矿预测，明确了岩金矿找矿方向。
With the cognition, we do some predictions on the rock gold deposits around the Jiayin Depression, and determine the ore-prospecting direction of rock gold deposits.
黑龙江北部砂金矿的金主要来源于经过壳幔作用使金再次富集的含金建造和岩金矿。
The gold in gulch-gold mines locating in northern region of Heilongjiang Province mainly originates from the gold-containing structure and lode gold mines enriched by crust-mantle action.
岩金氧化矿中金的后生富集及成矿作用研究，对找矿及矿产资源的开发具有重要价值。
The study on postnatal concentration and mineralization of gold in oxidized rock ore is of great significance to ore prospecting and exploitation of mineral resources.
对黑龙江省84个砂金样品及7个岩金样品，用等离子质谱仪分析了它们的稀土元素含量。
The REE contents of 84 placer gold samples and 7 hard rock gold samples in Heilongjiang province are determined by plasma mass spectrographic analysis.
不同地区剥蚀程度各有不同，剥蚀较严重的地区砂金分布广泛，化探异常与砂金分布相对应，而对寻找岩金关系不大。
The geochemical exploration anomaly is similar to the distribution of alluvial gold, and has not relation to the looking for the rock-gold.
在没有月光的金顶之夜，漆黑一片的摄身岩下，忽见一光如豆，冉冉而动，渐渐成了数点，渐至万各。
In the moonless night Jinding, dark rock body photo, suddenly saw a light such as beans, move slowly, gradually became gradually to the million points.
该构造杂岩带成矿条件良好，是金成矿的有利靶区。
This structure complex rock zone is good in gold mineralization condition, this advantageous prospecting target area.
作为一个绿色城市，南宁有许多风景点：人民公园、南湖公园、滨江公园、民族风情园、青秀山、伊岭岩、金伦洞等等。
As a green city, Nanning has a lot of beautiful scenery, such as the People's Park, Nanhu Park, Binjiang Park, the National Amorous Park, Qingxiu Hill, Yiling cave, Jinlun cave.
另外，砂质单元金含量比细粒的粉砂岩和泥岩要高，从浊积岩序列的底部旋回至上部回金的含量降低并由不稳定到稳定等规律。
At other hand, the golden content of the sandstone is higher than that of fine grain siltstone and mudstone, and tends to decrease and stabilize upward in the turbidite sequence.
容矿角闪质糜棱岩中金与钯关系研究结果不支持金矿质直接来自于矿体附近的角闪质上壳岩包体说法。
Relationship of palladium and gold in the mylonite reveals no evdence to support direct source of Au ore materials from the upper crustal amphibolitic rock inclusions.
探讨了用离子交换分离富集极谱法测定岩矿样品中的痕量金的方法。
The method to determine trace gold in rock salt samples with ion exchange separation and enrichment is approached.
本文通过对杂岩体的成因、成岩时代、岩石类型以及岩体的含金性和部分同位素的特征分析，探讨了岩体与矿床的成岩关系。
Based on researching of the age, rock types genesis, gold content and the stable isotope composition of the complex, the relation between the deposit and the complex is discussed.
该区主要分布有以金为主的多金属矿床和以煤、大理岩为主的非金属矿床。
In the area, the main polymetallic mineralization is gold deposits and the nonmetallic mineralization is coal and marble.
而且含金构造中岩石的组构特征、糜棱岩类型、应变幅度、石英变形机制与金矿富集程度都有密切的关系。
The gold abundance is also related to the type of mylonite, the feature of micro-fabric, the mechanism of quartz deformation and the size of strain.
流体不混溶、水-岩反应及古大气水的混入是造成本区金沉淀成矿的主要因素。
Fluid immiscibility and fluid rock interaction may be the main causes for gold deposition in the mine.
运用数理统计和地质统计学方法，从矿区地层岩性、构造、岩浆岩、矿体的空间分布等方面研究了墨江金厂金矿床金元素的空间富集规律。
In this paper, the spatial enrichment regularities of gold are studied from the spatial distribution of ore bodies, lithology, construction and magmatic rocks with the methods of statistics and geos.
湖南变质岩区的内生与外生金矿床均以高成色的单一自然金产出为特征。
Endogenic and exogenic gold deposits in metamorphic regions in Hunanare characterized by occurrence of high-percentage single natural gold.
还包括一个金岩崖模型文件。
上述同位素地球化学证据表明，金成矿与岩浆岩有一定的成因关系。
The aforesaid isotope geochemical evidence indicates that there is a certain genetic relation between gold mineralization and magmatism.
庞西垌银（金）矿床是粤西北地区构造蚀变岩型银（金）矿床的典型代表之一。
The Pangxidong Ag(Au) deposit is a representative of its type in Northwest Guangdong Province.
花岗质岩石的地球化学类型属钙碱系列的改造型花岗岩和安粗岩系列的花岗岩，具有金的潜在含矿性。
The geochemical types of granitic rocks belonging to the regenerated granite of calc-alkali series and granite of latite series are good for latent ore-forming of gold.
流体不混溶、大气降水的不断加入以及水-岩交换作用是导致本区成矿流体中金、锑淀积成矿的主要因素。
Fluid immiscibility, continuous influxing of meteoric water and water-rock exchange are very important factors that caused gold and stibnite to deposit.
伴生金矿床可分为含金(银)多金属矽卡岩硫化锡铜矿床及含金脉(层)状锡铅矿床。
The associated gold mineralization can be classified into two types: Au (Ag) -bearing polymetallic skarn sulphide Sn-Cu deposit and Au-be.
冈底斯成矿带的矽卡岩型矿床与长江中下游的铁铜金矽卡岩型矿床在许多方面可以相比较。
The skarn deposits in the Gangdise metallogenic belt are comparable to Fe-Cu-Au skarn deposits in the middle and lower Yangtze Valley metallogenic belt in many aspects.
运用沉积学的原理和方法，对银洞坡歪头山组中段含金绿片岩系进行了细致的原岩恢复和成因地层分析。
The sedimentary principles and methods are employed to reconstruct the protolith and to analyse the genetic stratigraphy in middle Waitoushan Formation, Yindongpo.
自然金主要赋存在少硫化物蚀变岩型金矿石中，自然金分布不均匀。
There is less natural sulfide deposits are mainly conferred altered rock type gold ore, the uneven distribution of natural gold.
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