Mobile travel my world mining Perspective
The attachment I uploaded is the 1.6 general version perspective material package, and the 1.5 version perspective material package. Please see my other answer http://..com/question/575374098.html?oldq=1& From = evaluateto#reply box-1447463831
as long as you don't take a screenshot of your game screen, no one knows you use perspective material, please rest assured
if you still don't understand, please ask in time ~
if you think it's good, please adopt ~
< file FSID = "977629577" link = / share / link? Shareid = 907277003 & UK = 1294942082 "name =" sc16-64 20 1point6. Zip "health =" 0 "/ >in addition, when the OP is online, you can follow you stealthily, such as taking an op that is afraid of chaos, or a cheap primary school OP, and you will find it, You can see it after several times of mining.
in addition, there are plug-ins on the server that can detect it. If any nosy OP looks at the records in the background, it will also see
others. If you don't use the plug-ins on the server, you can see the news that players report you, Otherwise, it will be better than the above heavyweight gods (it seems that this situation does not exist)
PS: if you want to use perspective, you can use mods of K and j to see map data, which is better than perspective, but it may be ban because of power promotion. I remember Jones was on my city server. I should be able to find him there; Gosling, you have to go to the official website of minecraft and leave a message for him; K can be found in 3DM; Steve, it's said that the cup has been blackened by MCBS
I have 1.3 step Dashen and K Dashen mod. If I need to leave an email, don't leave QQ. Be careful that someone in MCBS will delete your minelog in number, ha ha
I hope it will be useful to you
or search for perspective or transparent material packages in material packages. I use transparent materials. The stone is transparent. Minerals are leaking out. Great
for adoption
In fact, the perspective material is not very good, and it will hit the wall when mining. I'll give you a mod to track minerals. Any version can be used
< file FSID = 1890922455 "link = / share / link? Shareid = 1463484607 & UK = 4078388463" name = "scenter-2.2.0_ 20130827134659.zip" wealth="0" />perspective material package, hope to adopt~
here is one:
legal, no risk, no franchise fee
the procts are of high quality and low price
the bonus system is simple and easy to double
no harm to others, no harm to oneself, no worry about contacts
sustainable business
welcome to exchange
Fig. 2-5-1 traffic location map of huyanqingshan iron mine in Lingqiu County, Shanxi Province. The iron ore area is about 8km away from Lingqiu County in the West and 1.5km away from Shanxi Hebei Province in the East (Fig. 2-5-1)
the huyanqingshan iron deposit in Lingqiu, Shanxi Province, is a new discovery recently. Many iron deposits have been found in this area before, such as damingyan and Banyu iron deposits in Fanshi County discovered by 1 ∶ 200000 geological survey in 1956. In 1959, the Ministry of Geology and the Ministry of metallurgy carried out 1:200000 and 1:50000 aeromagnetic survey in the Wutai Mountain area, respectively. Nearly 100 significant aeromagnetic anomalies were found. After medium and large-scale ground survey and detailed investigation, many ore inced anomalies were inferred and verified. After decades of surface magnetic method, geological survey and exploration, more than ten large and medium-sized sedimentary metamorphic "Anshan type iron deposits" have been identified, with a total reserves of 1.7 billion tons. So far, there are still many significant anomalies in this area
The 1 ∶ 50000 aeromagnetic anomaly in the area is composed of three parallel ne aeromagnetic anomalies. From west to East, they are numbered as M121 (47), M122 (47) and M120 (47). Among them, the M120 (47) anomaly is the largest one among the unexamined aeromagnetic anomalies in Wutai Mountain area. The anomaly strike is northeast and the anomaly area is 30km < sup > 2 < / sup > From 2006 to 2008, in the process of implementing the project of "Shanxi Hengshan Wutaishan iron ore general survey", Shanxi Geological Survey Institute carried out the general survey and prospecting for the anomaly of M120 (47), mainly carried out the high-precision magnetic survey and deep drilling verification First of all, the 1 ∶ 2000 high-precision magnetic profile survey was carried out from sparse to dense, and the line distance was 100-400m, which verified the existence of aeromagnetic anomalies, determined the distribution range of anomalies, and delineated four surface magnetic anomalies C Ⅰ, C Ⅱ, C Ⅲ and C Ⅳ. The forward and inverse calculation, depolarization and inference interpretation are carried out. Combined with the surrounding geological conditions, it is determined that the anomaly is caused by multi-layer magnetite ore body. According to the results of magnetic anomaly, 9 drilling projects were arranged to verify the anomaly, and a buried magnetite ore body with a thickness of about 20 m was found in the depth of 200-600 M. It is preliminarily estimated that the iron ore resources will reach large scale
Fig. 2-5-2 aeromagnetic anomaly (NT) distribution map of huyanqingshan Iron Mine. Sedimentary metamorphic iron ore is the main type. The geological environment is located at the junction of two grade II structural units, Shanxi Fault uplift and Yanshan platform fold belt. In Shanxi Province, Wutaishan fault arch belongs to grade III structural unit of Shanxi Fault uplift. According to the division scheme of metallogenic belt in the second round division summary report of the original Ministry of mines, it belongs to Wutai Precambrian iron and gold metallogenic belt (iv-16) in the middle part of the grade III metallogenic belt (iii-17) of the North China platform. Lingqiu huyanqingshan iron mine is located at the junction of the western end of Yanshan platform fold belt and the eastern end of Hengshan uplift of Shanxi Fault uplift
(2) the exposed strata are relatively complete in the area, from old to new, they are: Shizui subgroup of Wutai Group in Neoarchean, Changcheng System, Jixian system and Qingkou system in Mesoproterozoic, Cambrian system, Ordovician system and Carboniferous System in Paleozoic, Jurassic system in Mesozoic and quaternary system in Cenozoic. The iron bearing rock series of Jingangku formation in Shizui subgroup of Wutai Group is the main ore bearing strata in the area The exposed strata in the mining area are mainly Gaoyuzhuang Formation of Changcheng System, Wumishan formation of Jixian system, xiawanggu formation of Qingkou system, Ordovician system, Jurassic system and quaternary system, and sporadically distributed with ganggangku formation of Wutai Group, Maozhuang formation and Xuzhuang formation of Cambrian system The Jingangku formation is only sporadically exposed in the northern part of the M120 (47) aeromagnetic anomaly in the mining area, and largely concealed in the lower part of the Gaoyuzhuang Formation of the Changcheng System. Its lithology is mainly biotite granulite, biotite plagioclase gneiss, plagioclase amphibolite, magnetite quartzite, etc., which are the main iron bearing strata in the area. In space, it is nearly east-west. It can be seen from the drilling that the buried depth of ore bearing strata graally deepens from west to East and from north to south. The burial depth is generally 200-600mthe prominent feature of this set of strata is that it is rich in metamorphic mafic assemblages, and most of the iron bearing rock series are associated with plagioclase amphibolite, while a few are associated with granulite and gneiss. There are five layers of magnetite quartzite in Gushan area, with the thickness of 0.4-1.8m, and the thickest is about 13m
The great wall system strata are the caprock in the area, which are unconformably contacted with the Jingangku formation in an angle, and are exposed in a large area in the mining area. It is mainly a sedimentary formation composed of a set of carbonate rocks with chert bands and chert noles and a small amount of clastic rocks. The lithology is mainly chert banded argillaceous powdery dolomite, dolomitic sandstone, manganese bearing argillaceous dolomite with shale. On the whole, the normal stratum (north central part) inclines to the southeast with an dip angle of 11 °～ thirty-three °; However, in the northeast or northwest, the dip angle changes greatly, 26 °～ sixty-five °， Up to 80% locally ° about. This is mainly e to the influence of fault structure. The maximum thickness of this stratum is 764.8m (3) ore controlling factors the ore bearing strata in the area are Jingangku formation of Wutai Group, and the lithology is mainly biotite granulite, biotite plagioclase gneiss, plagioclase amphibolite, magnetite quartzite, etc. This stratum is the main iron bearing rock series in Lingqiu area The iron bearing rock series of Jingangku formation is distributed in a Syncline in Lingqiu area. There are iron ore bodies in the north and South wings of the syncline, and the turning end of the syncline is located in the east of Lingqiu. This set of strata has experienced many stages of fold tectonic movement, which makes the thin layer magnetite quartzite thicken in some sections to form thick iron ore body. From west to East, there are Zhaobei, Heishi, xixuanfeng, wenzibao and other small and medium-sized iron deposits in the area, and the thickness of each ore body shows a trend of thickening from west to East. The huyanqingshan iron ore area is located at the turning end of syncline and has great prospecting potential There are M120 (47) aeromagnetic anomalies distributed in the mining area, which are large in scale and regular in shape, and verified to be caused by concealed magnetite ore body According to the results of geomagnetic anomaly, Shanxi Geological Survey Institute carried out drilling engineering verification in this area. One zkh141 drilling project was carried out in the Western C Ⅱ abnormal area, and eight drilling projects were carried out in the eastern C Ⅳ abnormal area, including zkh221, zkh222, zkh241, zkh242, zkh243, zkh244, zkh261 and zkh281. Except for the latter two boreholes, magnetite orebodies are found in other boreholes (Fig. 2-5-3)according to the analysis of borehole and geomagnetic anomaly, the magnetic anomaly is caused by multi-layer magnetite. At present, from west to East, one iron ore body is controlled by boreholes zkh141, zkh221 and zkh242, with a length of about 2000m and a true thickness of about 20m. The length of the anomaly zone closed by 400nt high anomaly is about 6300m, 350m in the West and 1100m in the East. Combined with the abnormal scale, the iron ore resources in this area can exceed 100 million tons
the strike of ore body is nee, and the ore body is nearly vertical with a dip of 70 °～ eighty °
the deposit is a sedimentary metamorphic type iron ore. according to the analysis of existing test results, the average grade of MTE is 20.26%, the average grade of TTE is 27.70%, and MTE / TTE = 0.73, which is determined as a mixed ore type
(2) geophysical characteristics: the ore bearing strata are Jingangku formation of Wutai Group, most of which are concealed under Gaoyuzhuang Formation of Changcheng System. The aeromagnetic anomaly in the area is well developed and large in scale, which is one of the unexplained magnetic anomalies in the investigated area. It is characterized by a NE trending anomaly with a length of about 12000m and a width of about 2500m; The anomaly isoline is composed of 50nt, 150nt, 300nt and 500nt, which is a regular zonal anomaly with little gradient change. The gradient at the transition zone between positive and negative anomalies is larger, which shows that the north side of the magnetic body is steeper. The ground magnetic anomaly is similar to the aeromagnetic anomaly in strike and shape, which is composed of four local anomalies. This abnormal area is an important target for searching for gneiss heishanzhuang type iron deposit in the deepthe outcropping strata in the area are Gaoyuzhuang Formation of Changcheng System, xiawanggu formation of Qingkou system, Ordovician, Jurassic and Quaternary strata, and there are Jingangku formation of Wutai Group, Maozhuang formation and Xuzhuang formation of Cambrian system sporadically
the main rock (ore) magnetic parameters are shown in table 2-5-1 and table 2-5-2
Fig. 2-5-3 geological map of huyanqingshan iron mining area
table 2-5-1 statistical table of rock (ore) magnetic susceptibility of huyanqingshan working area in Lingqiu County
note: the data is from iron ore general survey project of Hengshan Wutaishan area, Shanxi Geological Survey Institute, 2008
table 2-5-2 statistical table of rock (ore) remanent magnetization in huyanqingshan instrial area, Lingqiu County
note: the data is from the iron ore survey project of Hengshan Wutaishan area, Shanxi Province Geological Survey Institute, 2008
it can be seen from the above table that the magnetite bearing quartzite has the strongest magnetism, and the magnetic susceptibility is (16016.3 ~ 97706.92) × four π× 10 < sup > - 6 < / sup > Si, the geometric mean is 45173.4 × four π× 10－6SI The remanent magnetization is up to 10 000 < sup > - 3 < / sup > A / m. The magnetic susceptibility of amphibolite, granulite and quartzite is only 4 π× The magnetic properties of the magnetite bearing quartzite are more than several orders of magnitude different from those of other rocks
The purpose of high-precision geophysical exploration in the area is to verify the existence of aeromagnetic anomaly, delineate the scope and distribution characteristics of magnetic body, infer its buried depth and occurrence, and provide basis for drilling verificationit can be implemented in the following stages: first, check the aeromagnetic anomaly at the initial stage of the work, that is, lay several high-precision magnetic survey sections (a total of 20km) at 800m line distance in the center of the aeromagnetic anomaly to confirm the existence and approximate range of the anomaly. The second is to delineate the range of magnetic body. In this stage, the line distance of high-precision magnetic survey is 400m and the point distance is 10m (the magnetic survey section is 20km in total), which completely closes the magnetic anomaly and understands its overall distribution law. The third is to understand the local characteristics of the magnetic body in detail, and carry out the densified magnetic section survey in the abnormal center. The distance between the abnormal center lines is 100m, and the rest parts are 200m (the magnetic section is 45km in total). This paper analyzes the characteristics of magnetic body dislocation and pinchout caused by local structure, and analyzes the spatial storage characteristics of magnetic body. Combined with the geological and physical properties of the area, the plane anomaly characteristics and profile curve characteristics are used to infer the strike, length, thickness, buried depth and tendency of magnetic body
(2) instruments and technical parameters
Nanfang Lingrui S80 al frequency GPS receiver is used for survey network layout and survey point positioning, with nominal RTK plane accuracy of 1cm + 1ppm and elevation accuracy of 2cm + 1ppm. Quality inspection observation accuracy of measuring points: plane mean square error ± 17m, mean square error of elevation ± 11m, which meets the technical requirements of the code for engineering survey of geophysical and geochemical exploration
The measurement parameters are total field t, the resolution of the instrument is 1nt, the capacity is 5000nt, and the observation accuracy is ≤ 5nt. The mean square error of quality inspection in each stage ring the working period is less than 0 ±( 97) nt, meeting the technical requirements of DZ / t0071-93(3) interpretation inference and achievements
anomaly interpretation is mainly based on the geological and physical characteristics of the mining area, from known to unknown
from the region Δ It can be seen from the T isoline plan (Fig. 2-5-4) that the magnetic anomaly in the area is mainly composed of Δ T = - 100nt is closed, and the trend of magnetic anomaly is ne, narrower in the West and wider in the East