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According to model, lead zinc ore bodies of mineral deposit, celestite ore bodies and gypsum ore bodies are distributed by the incomplete dome shape. The sandstone type ore bodies like a curved surface shape, is on the top, wide distribution, which like the top cover of a mushroom. The limestone breccia type ore bodies, under the sandstone type ore bodies, with mostly irregular vein shape, lens body shape, locate at the root of the mushroom. Gypsum and celestite ore bodies, accompanying with limestone breccia type ore bodies with the shape of vein, lens body, distribute under the sandstone type ore bodies.

根据模型显示,金顶矿床铅锌矿体、天青石矿体和石膏矿体呈不完整的穹隆状分布,砂岩型矿体在上,为曲面状,分布广,似一蘑菇的顶盖,而灰岩角砾岩型矿体分布局限,部分产于砂岩型矿体之下,多为不规则的脉状、透镜体状,构成蘑菇的根部;石膏和天青石矿体主要与灰岩角砾型矿体相伴产出,呈脉状、透镜体状,多分布于砂岩型矿体下部。

Seven molybdenite samples from greisen ore body and quartz vein tungsten ore body associated with black tungsten ore were chosen for Re-Os isotopic dating and model age of (141.4±2.2) Ma~(158.2±2.2) Ma were obtained. The isochrone age of molybdenites from greisen type tungsten-tin ore body is (156.8±3.9) Ma, which indicates that its mineralogenetic epoch is at the Middle Jurassic, corresponds to the second stage of early Yanshanian period. And the model age for the samples from greisen ore body and from quartz vein ore body are (150.7±2.4) Ma~(158.2±2.2) Ma and (141.4±2.2) Ma~(151.0±2.4) Ma respectively, which indicates that the mineralization time of the quartz vein ore body is slightly earlier than that of greisen ore body.

文章选取云英岩型矿体及上部石英脉型钨矿体中与黑钨矿共生的辉钼矿7件,进行Re-Os等时线年龄测定,得到其模式年龄为(141.4±2.2) Ma~(158.2±2.2)Ma,其中云英型钨锡矿体中辉钼矿等时线年龄为(156.8±3.9)Ma,成矿时代为中侏罗世,对应于燕山早期第二阶段;从云英岩矿体中样品模式年龄为(150.7±2.4)Ma~(158.2±2.2)Ma,石英脉型矿体中样品模式年龄为(141.4±2.2)Ma~(151.0±2.4)Ma。

The leucogranites veins occurred widespreadly in the para-metamorphic rocks, in which the hypersthene melagranulite distributed. That suggests the source rocks of leucogranites of the High Himalaya are para-metamorphic rocks. For the basement was uplifting, pressure relieved and lacked water, source rocks were melting partly and formed the leucogranite magma.

基底副变质岩中广泛分布淡色花岗岩脉体,在基底副变质岩中的淡色花岗岩脉体中发现紫苏辉石暗色麻粒岩残留体,这表明本区高喜马拉雅淡色花岗岩源岩为基底副变质岩,且基底副变质岩是在基底快速隆升降压的条件下发生缺水熔融生成的淡色花岗岩岩浆。

The physical characteristic of weathered lamprophyre has impenetrability and nonhomogeneity, however, the YDS epoxy resin possesses initial viscosity, strong affinity to mediums, excellent permeability and good ageing property. After chemical grouting, the rock mechanics characteristics are improved greatly and can meet the design requirements, it indicates that lamprophyre can be grouted by YDS epoxy resin.

为此,采用了高渗透性的YDS环氧材料对风化后的煌斑岩脉进行纯压式灌浆试验,试验结果表明:通过YDS改性环氧浆液的"浸透""浸渗"加固处理,风化的煌斑岩脉力学性能大幅提高,基本能满足设计的力学指标要求。

According to petrologic analysis of 18 samples of altered rock, phlogopite rock , with regard to its B 2O 3 content, it is generally restricted to the outside of the ore bed, having certain ties with the boron minerlization while no ties are found in altered rock of the same type associated with veins of diorite porphyrite.

其中金云母岩多分布在含矿层外带,通过对 1 8件金云母岩样品中B2 O3含量分析,表明正常蚀变岩中的金云母岩与硼矿有一定的关系,而由闪长玢岩脉体侵入影响下形成的金云母岩则与矿化无关。

In meymechite dike and phogopite-plagioclase peridotite dike, MgO content respectively is 28.86%~ 32.78% and 27.28%~ 34.99%., they belong to the ferrguinous ultrabasic rock .

玻质纯橄岩脉和金云斜长橄榄岩脉,它们的MgO含量分别为28.86%~32.78%和27.28%~34.99%,属于铁质超基性岩。

It has the metamorphic rock sight—"the Inartificial Gallery" which is black and white, devious and whirlabout and likes the reversal cloud-mist and rising sun, the granite vein injecting along the bedding of gneiss crossing the river-gorge—"the White Dragon Crossing River", nine veins apposing on the rock wall—"the Nine-dragon Wall","the Inartificial Wall " formed by the paragenesis of the level joint and the vertical joint, and the small and exquisite undercutting cave which is the wonder of the new tectonic movement.

有黑白相间、曲折盘旋,如云雾翻卷,似霞蔚蒸腾的变质岩景观――"天然画廊",有沿片麻岩层理贯入的花岗岩脉,横跨河谷的"白龙过江",有九条岩脉并列在岩壁之上的"九龙壁",有水平节理与垂直节理巧妙共生而形成的"天然城墙",有新构造运动遗迹――小巧玲珑的淘蚀洞穴。

The physical characteristic of weathered lamprophyre has impenetrability and nonhomogeneity, however, the YDS epoxy resin possesses initial viscosity, strong affinity to mediums, excellent permeability and good ageing property. After chemical grouting, the rock mechanics characteristics are improved greatly and can meet the design requirements, it indicates that lamprophyre can be grouted by YDS epoxy resin.

为此,采用了高渗透性的YDS环氧材料对风化后的煌斑岩脉进行纯压式灌浆试验,试验结果表明:通过YDS改性环氧浆液的&浸透&&浸渗&加固处理,风化的煌斑岩脉力学性能大幅提高,基本能满足设计的力学指标要求。

We think main metamorphic rock types of this area include mited granite ,mixed metamorphic rock,leptite,etc.

认为变质岩中混合花岗岩、混合岩化变质岩、变粒岩、浅粒岩、黑云斜长片麻岩等为本区的主要变质岩类型;沉积岩以云岩、硅质岩和石英砂岩为主;火成岩脉主要为辉绿岩、煌斑岩和闪长玢岩。

Most of small intrusive bodies are stocks or dikes, and each of the dimension is less than 1km2 ; they are mostly granite-porphyry、porphyritic-granite、monzogranite,a small amouts of them are quartz diorite or diorite; the chemical characters are high content of SiO2、K2O and low content of Mg and CaO, on the SiO2-K2O diagram all the samples fall in the field of high-K calc-alkalic series and shoshonite series.

小岩体多呈岩株或脉状产出,出露面积多数在1km2以下;岩性主要为花岗斑岩、似斑状花岗岩、二长花岗岩,少量为石英闪长岩及闪长岩等;岩石化学成份以高硅、富碱、多钾、贫镁、少钙为特征,属高钾钙碱性系列或钾玄岩系列。

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