强蚀变糜棱岩即为金矿体及金矿化体。
Strongly altered mylonite is gold orebody and gold mineralized body.
有规模的金矿体一般产在岩体的接触带上。
Important gold ore bodies generally occur in the contact zone of rock bodies and country rocks.
东风山金矿体赋存在含铁层之下的东风山群角岩层中。
Dongfengshan gold deposit is occurred in hornstone of Dongfengshan group under iron bearing stratum.
由此可以推测晋宁期是蚀变岩型金矿体形成的主要时期。
It is thus held that the Jinning Period is the main time for the formation of the metamorphic gold deposit.
根据无根金矿体的成因机制，提出追踪原生金矿体的方法。
On the basis of the genetical mechanism of rootless gold orebody, this paper put forward the searching methods of primary gold orebody.
根据无根金矿体的成因机制，提出追踪原生金矿体的方法。
On the basis of the genetical mechanism of rootless gold orebody, this paper put forward the searching methods of primary g...
对双王含金角砾岩带中其它金矿体的勘查及开发也有重要的指导意义。
It is also very important to the exploration and mining to other analogus gold deposits at Shuangwang gold-bearing breccia belt.
金山金矿床明显受金山—西蒋剪切带控制，金矿体产于剪切糜棱岩带中。
The Jinshan gold deposit is obviously controlled by the Jinshan - Xijiang shear zone, and the ore bodies are occurred in the shear mylonite zone.
利用这种矿化空间分布的有序性规律，在老青—小青地区发现了金矿体。
The application of the orderly rule of mineralization space distribution in the location prediction of orebody with the example in Rushan region is discussed.
控矿构造主要为NNE向断裂，具明显的双重结构面特征，金矿体严格受其控制。
The ore controlling structure is mainly NNE strike fault with double constructional surface.
金矿体的产状严格受铜官山倒转背斜不同部位地层岩石的产状及其层间断裂的控制。
The attitude of gold ore bodies are strictly controlled by that of the strata in different parts of the Tongguanshan overturned anticline and interlayer faults.
金矿床严格受剪切构造带的控制，金矿体一般赋存于韧—脆性构造和构造扩容带中。
The gold deposit is totally controlled by shear structures and is formed in the ductile brittle structures and structural extension zone.
根据化探结果圈定了两个异常区，目前都已发现具有相当规模的蚀变带和一些金矿体。
According to anomaly of gold geochemical prospecting delineated to two anomalous areas. Up to now there have been discovered on a quite scale of alteration zone and some gold ores.
黔西南水银洞金矿为产于上二叠统龙潭组中的超大型、高品位金矿床，矿床由多个金矿体组成。
The Shuiyindong gold deposit, which occurs in the Longtan Formation of the Upper Permian series, is a super-large, high-grade gold ore deposit.
沿甘孜-理塘断裂带发育的韧性剪切带，控制了区内金矿化、金矿床(点)、金矿体的形成和分布。
Gold mineralization and deposits (occurrences) in Garze-Litang fracture zone are controlled by a ductile shear zone along the fracture zone.
富金矿体在走向上一般分布于NNE向断裂的转折地段，倾向上分布于断裂产状由陡变缓的过渡部位。
The gold-rich ore bodies occurrs in the winding part of NNE-trending fractures on strike and transforming part from steeply dipping to gently dipping on dip direction.
文中主要论述11号系脉特征、系脉中铜金矿体和铜矿体的分布规律，以及断裂构造组合对矿体的制约。
The paper primarily discusses the characteristics of the vein, the distribution of gold orebody and copper orebody, and the confinement of fracture tectonic association to the orebody.
主要控矿条件为小岩株状石英闪长玢岩（次火山岩），其中寄生的隐爆角砾岩筒及外围裂隙中赋存着金矿体；
The main control condition is quartz diorite-porphyrite with the shape of small rock stub(subvolcanic rocks), among the parasitic rubblerack tube and the off-lying crack, the gold orebody occurs.
不论岩浆成因还是构造成因，金矿体均受断裂破碎带、断层带或片理化带等构造带控制，产于大断裂带旁侧。
Whether magma reason or structure reason, the gold mine is all controlled by fracture zone beside large fracture.
断裂构造不仅控制着金矿化的时间，而且控制着金矿体（床）的空间分布及产状，同时也控制着金矿化类型。
The faults not only controlled the timing and the type of gold mineration, but also the distribution and occurrence of gold ore bodys.
该矿床主要受安昌河—观音坝断裂带控制，带内一系列次级层间剪切带或次级断裂是金矿体的有利赋矿部位。
The deposit is mainly controlled by the Anchanghe-Co-Guanyinba fault, the sub-interlayer shear belts and sub-fault belts of it are the favorable place where gold ore body occurrence.
金矿化受脆-韧性剪切带控制，并伴随着多期构造变形和多期矿化作用，金矿体就产于脆-韧型剪切带的中部；
The gold minerilization is controlled by brittle-tenacity shear belt and along with the action of multi-periodic structure distortion and multi-periodic minerilization.
每一次的脉动和幔涌形成的金矿体都表现了各自的地球化学特征和元素组合特征，成矿微量元素在垂向上具有各自的规律性。
Gold ore bodies formed by every pulse and mantle-surge all show respective geochemical and element combination characteristics. Each mineralized trace element show regularity in vertical section.
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.
通过对望儿山金矿床i - 2矿体成矿规律的分析和研究，指出了今后的找矿方向，为金矿进一步找矿提供重要依据。
Through the analysis and study of mineralization law of I-2orebody of Wangershan gold deposit, the prospecting orientation is pointed out, and it provides important basis for further prospecting.
对新房金矿深部矿体开拓的必要性进行了探讨，提出了深部开拓的可行性方案。
The necessity of the development of deep orebody is studied and the feasible plan is put forward in this paper.
运用回归分析，模拟出原生金矿化元素地球化学模型。利用变异性指数法确定了矿体原生晕垂向分带。
Element geochemistry model of the primary mineralization halo is simulated by regression analysis and vertical zoning of the ore body primary halo by variable index method.
其形态、成分、物性及时空分布规律的研究，是从矿物学角度进行中深脉状金矿矿体定位预测研究的最重要内容。
Their crystal form, composition, physical features and distribution in time and space make up one important line of information when carrying out site prediction of ore bodies.
其形态、成分、物性及时空分布规律的研究，是从矿物学角度进行中深脉状金矿矿体定位预测研究的最重要内容。
Their crystal form, composition, physical features and distribution in time and space make up one important line of information when carrying out site prediction of ore bodies.
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