What bus should I take to Xusheng Street 22 from the resettlemen
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1 Overview the mining area is located 32km northwest of Qinhuang City, under the jurisdiction of Zushan Town, Qinglong Manchu Autonomous County
From 1959 to 1994, the prospecting units of metallurgical and geological systems successively carried out general survey and exploration work, and submitted geological reports for many times. According to the No. 44 document issued by Hebei provincial mineral resources and reserves Commission in 1994, the total identified resource reserves are 5341.6 × The average ore grade (SFE) is 26.80%. It is a medium-sized deposit. It was built in 1990 with a proction scale of 122 × 104t/a As of October 26, 2008, the reserve is 3499.98% × 104t During the exploration, a total of 1 ∶ 2000 geological survey of 2.4km < sup > 2 < / sup >, trenching of 4288.3m < sup > 3 < / sup >, drilling of 8376.44m (37 boreholes) and 2587 basic analysis samples were completed The highest elevation is 685.32m, and the lowest elevation is 482.37m (2) metallogenic geological conditions1
(1) the Archean yuluanxian group is a set of metamorphic rocks with medium and low metamorphic degree (amphibolite facies), mainly composed of granulite, schist and magnetite quartzite. Granodiorite is mainly hornblende granodiorite, followed by biotite granodiorite and biotite hornblende granodiorite; The schist is mainly hornblende quartz schist, followed by sericite and mica quartz schist. The granulite is mainly distributed in the roof of the ore body and the surrounding rock far away from the floor, and the schist is mainly distributed in the floor of the ore body. In the amphibolite granulite not far from the floor, there is a relatively stable metamorphic conglomerate about 20m thick The results show that the migmatization is not uniform, the floor and surrounding rock of the orebody have not been migmatized, and the resial volcanic pores and porphyry structures of hornblende quartz schist are obvious; The roof and surrounding rock of the ore body are generally subjected to migmatization, especially the surrounding rock far away from the ore body is more intense, forming a large area of migmatite and migmatite (2) quaternary system of Cenozoic is composed of resial slope and alluvial proluvial deposits, mainly distributed in mountain valleys. Generally, the thickness is 2-5M, and the thickest is about 15m The geotectonic location of the mining area is the Sino Korean paraplatform (I) Yanshan platform fold belt (II) Shanhaiguan platform arch (III) northwest zone There is no fold structure inarea. The fault structure is not developed, only two small-scale faults can be seen, which has a certain destructive effect on the II ore body. In a word, the structure in the area is simple, showing a monoclinic structure as a whole, and the strike of the strata to the north of line 4 is 40 ° From the south to the north and south; It is inclined to northwest or west, and opposite in some parts (line 7-13), with an inclination of 75 °~ eighty-five °
Magmatic rocks are located between the anziling mixed dome and Xiangshan granite body, and the magmatic activities are strong in the area Porphyry granite: the porphyry granite is the northern marginal facies of Xiangshan rock mass, and the southern end of No. II ore body pinched out in the rock mass e to large-scale intrusion. The rock body intrudes from northwest to Southeast, which becomes the southern boundary of the ore body and limits the extension of the ore body. The South No. II ore body floats on the rock body in a wedge shape. The contact surface between rock mass and ore body is 45 °~ fifty ° There are also some small branches penetrating into the ore body Rhyolitic tuff: mainly distributed in the southwest of the mining area, covered by metamorphic rocks in an angular unconformity, forming steep cliffs The dykes are mainly quartz syenite porphyry and olivine pyroxene According to the contact relationship, Xiangshan intrusion was formed later than rhyolitic tuff (3) geological characteristics of ore body1. The scale, shape and occurrence of ore body
there are four ore bodies arranged in parallel belts in the range of 1530m long from north to South and 100-250m wide from east to West in the mining area. The scale of ore bodies is different, among which the No.2 ore body is the main ore body, accounting for 96.5% of the total resource reserves; Other ore bodies are small in scale, 145-235m in length. The buried depth of ore body is generally 0 ~ 300m
No. II orebody is distributed from the north of No. 9 line to the south of No. 14 line, with a length of 1400m and a large variation in thickness. It is generally a stratoid body with wide south, narrow north and large middle thickness. Expansion and contraction and branching compound phenomena can be seen along the strike and dip. The ore body of line 5 is thicker to the south, the thickest of line 2 is 125m (including the true thickness of rock inclusion), and the thinnest of line 7 is 22m, with an average thickness of 65m. The highest elevation of ore body exposed is 660m, the lowest is 547m, generally about 600m. Due to the restriction of Xiangshan granite, the South extension depth of ore body line 6 is relatively small, and the north extension depth is relatively large, generally about 300m, with the maximum oblique depth of 520m (line 0). The occurrence of ore body is basically consistent with that of surrounding rockthe ore bodies are mainly magnetite bearing quartzite and hornblende granulite, and locally plagioclase hornblende
(1) the mineral composition and structure of the ore is magnetite quartzite, and the mineral composition is relatively simple. The ore mineral is mainly magnetite, with a small amount of pseudo hematite locally; Quartz is the main gangue mineral, followed by mafic amphibole, amphibole and so onthe ore is dominated by allomorphic subhedral medium fine grained structure, and the magnetite particle size is mostly 0.05-0.25 mm; Quartz is mostly heteromorphic granular, and its particle size is slightly larger than magnetite; Some of the dark minerals are metasomatized by tremolite and actinolite
The mineral grains of ore bodies near Xiangshan rock body are obviously coarsened and the grade is increased, such as the No.2 ore body in the southern Z K16. The ore structure is mainly striped, followed by fine striped and banded (2) the ore type and grade are classified as magnetite and hematite according to the main iron ore; According to the main gangue minerals in the ore, they are all quartz type iron ore. The instrial type of ore belongs to magnetite (lean ore) which needs to be beneficiated There are 2086 ore samples in thearea. The mathematical statistics of these samples are carried out to understand the mass fraction and change of TFE and SFE. See table 4-4 for details
It can be seen from table 4-4 that the ore grades (TFE, SFE) are mostly 25% - 35%, accounting for 71.24% (TFE) and 58.49% (SFE); The surface grade is higher than that of borehole, but it is not higher than that of borehole, which is 0.22% (TFE) and 0.92% (SFE) The grade variation coefficients of ore bodies in the whole area are 13.99% and 16.77% respectively, which belong to uniform type. Secondly, the ore grade of the orebody tends to become rich from north to south along the strike, which may be related to the orebody approaching Xiangshan granite from north to south; There is a lower grade ore bed with a thickness of 20-30m in the floor of ore body and nearby According to the ore structure, the fine grain is of high grade, followed by stripe and strip; According to the orebody, the grade of No. III orebody is higher, followed by No. IV, No. II and No. I orebodies
Table 4-4 statistical table of ore grade. The difference is related to the mass fraction of amphibole minerals in the ore. The more the mass fraction is, the greater the difference is; In addition, the higher the ore grade, the smaller the difference. See table 4-5 for details
Table 4-5 statistical table of difference between total iron and soluble iron; Two drill holes (zk001), tfe58.77%, sfe58.21%, tfe52.18%, sfe52.18%. The surface sample length is 2m, and the borehole sample length is about 0.90M. This indicates that there are sporadic rich iron ores in local lean ores in the area
(3) chemical composition and washability of the oreaccording to the results of chemical analysis, multiple analysis and spectral analysis, the chemical composition of the ore is mainly Si, Fe and O, followed by Mg, Ca and Al, and the mass fraction of associated useful components such as Ti and Mn is very small, which has no comprehensive utilization value
according to the statistics of 118 composite samples, the mass fraction of SiO < sub > 2 < / sub > was 58.75%, 33.08% and 45% - 55% respectively; However, the content of SiO < sub > 2 < / sub > is obviously related to the ore grade. The mass fraction of P was 0.03% - 0.05% (61.87%), the highest was 0.107%, the lowest was 0.017%, and the average was 0.048%. The mass fraction of S was generally less than 0.15% (69.49%), the highest was 1.27%, the lowest was 0.001%, and the average was 0.13%
the ore belongs to magnetite with easy separation. According to the test, no matter how high or low the ore grade is, good indexes of concentrate grade of 66% ~ 68% and recovery rate of 82% ~ 95% can be obtained, which fully meet the national standard. See table 4-6 for details
Table 4-6 statistical table of mineral processing results (4) characteristics of magnetic anomaly the anomaly is located in the north of Miaogou Yuguan anomaly area, with east-west direction and two anomaly centers in the middle. The highest value of the anomaly is in the northeast of the anomaly, with the intensity of more than 2000 NT. Affected by the geological background, the anomaly protrudes to the southeast and forms a small anomaly center with the intensity of 500 NT (Fig. 4-11)
Figure 4-11 magnetic anomaly of Miaogou Iron Mine (V) mining technical conditions of the deposit (1) hydrogeological conditions the exposed position of the ore body is high, most of the shallow ore body is above the local erosion base level, and the terrain slope is large, which is concive to rainfall discharge. The aquifer is mainly weathered fissure water with weak water content, which has little influence on open-pit mining. In the deep contact zone between Xiangshan granite and metamorphic rock, the water head of vein confined fracture is high, but the water volume is small. There is no large perennial water body on the surface, but sometimes the flood flow is large in rainy season, so flood control measures should be taken To sum up, the deposit belongs to the type with simple hydrogeological conditions2. Engineering geological conditions
the ore is compact and hard with strong compression resistance. According to statistics, the maximum compressive strength of ore is 2814kg / cm < sup > 2 < / sup >, the minimum is 897kg / cm < sup > 2 < / sup >, and the average is 1748kg / cm < sup > 2 < / sup >; The maximum weight of roof, floor and rock inclusion is 2615kg / cm < sup > 2 < / sup >, the minimum weight is 2581kg / cm < sup > 2 < / sup >, and the average weight is 1430kg / cm < sup > 2 < / sup >. The natural slope angle of rock and ore is more than 50 ° About 70 °~ eighty °
the structure in the area is relatively simple, the fault structure is not developed, and the mining has little influence on the stability of ore body and rock
In a word, the engineering geological conditions in the area are good, and the hydrogeological conditions are simple, so it has little impact on the slope stability of the open pit According to the statistics, the stripping ratio of the whole area is 3.3 according to 396m elevation (6) exploration type and instrial index: 1. Exploration type of ore deposit: the main ore body is 1400m long, stratoid, with great thickness variation and uniform ore grade; The structure in the area is simple and the faults are not developed, which has little damage to the ore body. In conclusion, the deposit can be divided into type II - III transitional type. According to the instruction of (79) jigedizi No. 123 issued by Hebei Provincial Bureau of geology, the exploration network of the deposit is determined as B-class 100m × 75m Class C 200m × 150m Level D: Level C extrapolation and insufficient level C network Instrial indexadopted (81) JYZ No.29 document (table 4-7) issued by Hebei Metallurgical Instry Bureau on September 12, 1981:
Table 4-7 instrial index
< P > the minimum minable thickness is 2m, and the thickness of rock inclusion removal is 2m
According to the geological characteristics of the mining area and ore body, qinglongmiaogou iron deposit belongs to metamorphic ferrosilicon formation iron deposit or sedimentary metamorphic iron deposit, also known as Anshan type iron deposit Except for the II ore body, the other scales in the area are very small, so there is no prospect. The exploration depth of II ore body is generally 300-400M elevation, and the deepest is 170m elevation (line 0). According to the ore body extension and exploration depth, the south of line 6 is restricted by Xiangshan granite, so there is no ore bodydate of establishment: March 15, 1993
registered capital:
region: Hebei Province
unified social credit Code: 91130321700615268q
business status: existing (in business, open, registered)
instry: mining instry
Company type: branch of other limited liability company
English Name: Tanggang Mining Co, Ltd. Miaogou Iron Mine
staff size: 100-500 people
business address: Baishu village, Zushan Town, Qinglong Manchu Autonomous County
business scope: iron ore mining and magnetic separation; Iron concentrate processing; Pellet, sinter and ferroalloy; Smelting (ferromanganese, ferronickel, ferrochrome, ferrotin, composite iron) (projects that need to be approved according to law can only be operated with the approval of relevant departments)**
No.
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Ji 0815f E Qinglong County Dingfa iron ore
Ji 0816fe Qinglong County guozhangzi iron ore
Ji 0817fe Qinglong County Hebei Minyi Jinlong iron ore
Ji 0818fe Qinglong County Hongda second iron ore
Ji 0819fe Qinglong County Hongfa iron ore
Ji 0820fe Qinglong County Hongyuan iron ore
Ji 0821fe Qinglong County Huaxin iron ore
Ji 0822fe Qinglong County Liangshuihe iron ore
Ji 0823fe Qinglong County louzhangzi Township Shiren Jingou iron ore
ji0824fe Qinglong County Luanxin iron ore
ji0825fe Qinglong County maquanzi iron ore
ji0826fe Qinglong County Miaogou Iron Ore
ji0827fe Qinglong County nanzhangzi factory Fangfang iron ore
ji0828fe Qinglong County nanzhangzi yingwushan iron ore
ji0829fe Qinglong County Fangzi iron ore
ji0830fe Qinglong County Puying iron company langzhangzi iron ore
ji0831fe Qinglong County Qianwu iron ore Ma iron ore
Ji 0832fe Qinglong County qianzaoshan iron ore
Ji 0833fe Qinglong County Qinglong lamagou iron ore
Ji 0834fe Qinglong County qiuzigou iron ore
Ji 0835fe Qinglong County sanhe iron ore
Ji 0836fe Qinglong County shenzhangzi iron ore
Ji 0837fe Qinglong County Shenghua North iron ore
Ji 0838fe Qinglong County shuangshanzi Sanhedian iron ore
name of main ore origin
ji0839fe Qinglong County xiaolingxi iron ore
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ji0842fe Qinglong County Yongsheng iron ore
ji0843fe Qinglong County Zushan town anmenkou iron ore
ji0844fe Qinglong County Zushan town huachangyu iron ore
ji0845fe Qinglong County zhalanzhangzi iron ore
ji0846fe Senyuan Liyuan iron ore
ji0845fe 0847fe Xinghua Iron Ore
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Ji 0849fe magnetite changfangzi iron ore in nanzhangzi Township, Qinglong County
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Ji 0851pb Zn Cu zhouzhangzi lead zinc ore in Qinglong County
Ji 0852 dolomite (for metallurgy) dolomite ore in zhuaoying, Funing County
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Ji 0854 granite (facing) Qinglong County dahudian granite mine
Ji 0855 limestone (glass) Funing County Wangzhuang glass dolomite mine
Ji 0856 limestone (cement) Funing County Chazhuang cement limestone mine
Ji 0857 limestone (cement) Funing County chaoshuiyu cement limestone
Ji 0858 limestone (cement) Funing County shimenzhai cement limestone mine
Ji 0859 Limestone (for cement) Jining County zhuaoying cement limestone East Mine
Ji 0860 limestone (for cement) Funing County zhuaoying cement limestone West Mine
Ji 0861 limestone (for cement) Lulong County Wushan cement limestone
Ji 0862 limestone (for cement) Qinglong County shanshenshen Beigou cement limestone
Ji 0863 limestone (for alkali) Lulong County Wushan alkali limestone
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ji0866 coal Changli coal mine in Changli County
ji0867 coal Tangsu coal mine in Changli County
ji0868 coal Liujiang coal mine in Funing County
ji0869 coal Lulong coal mine in Lulong County
ji0870 coal Qinglong Coal Mine in Qinglong County
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ji0872 refractory clay Funing County shimenzhai fushuizhai refractory clay ore
ji0873 refractory clay Funing County shimenzhai Huanxiling refractory clay ore
ji0874 refractory clay Funing County shimenzhai Taoshugou refractory clay ore
ji0875 sandstone (for glass) Funing County Jiguanshan glass quartz sandstone ore
ji0876 sandstone (for cement proportioning) Funing County Panzhuang cement proportioning quartz ore Sandstone ore
ji0877 sandstone (for cement proportioning) sanyizhuang cement quartz sandstone ore in Funing County
ji0878 sandstone (for cement proportioning) xiapingshan cement quartz sandstone ore in Funing County
ji0879 fluorite (ordinary) muzaoyu ordinary fluorite ore in Funing County
ji0880 fluorite (ordinary) Shenhe Zhujiayu fluorite ore in Funing County
ji0881 oil shale luweishan oil shale ore in Lulong County
take the bus to Qinglong or Zushan at Haiyang Road bus station and get to Zushan town. After getting off, take a motorcycle or private car to Miaogou Iron Mine, about 5km
2. If you can take Qinhuang bus from Beidaihe railway station to siqiao bus station, walk 150m eastward to Haiyang Road, then turn left, and walk 250m northward to Haiyang Road bus station.