The chemical compositions,mineralogical characteristics,as well as dissemination of iron-and phosphorus-based minerals were studied for the E’xi oolitic hematite from western Hubei Province in China by using chemical...The chemical compositions,mineralogical characteristics,as well as dissemination of iron-and phosphorus-based minerals were studied for the E’xi oolitic hematite from western Hubei Province in China by using chemical analysis,optical microscope,electron probe micro-analyzer(EPMA)and energy dispersive spectroscopy(EDS).It is found that this kind of oolitic hematite ore contains 47.71%TFe,10.96%SiO_2,as well as 0.874%P,with hematite as the dominant Fe-bearing minerals,and quartz,chamosite,illite and cellophane as main gangue minerals.The microscope examination showed that the ore has an oolitic structure,with some ooids principally formed by a series of concentric layers of hematite collophanite around nucleus that is hematite in the association with collophanite.Based on the EPMA and EDS analysis,it can be known that some ooids are primarily composed of hematite and collophanite.The separation can be achieved through fine grinding for those collophanite laminae with a higher P content.However,the dissemination of two minerals at the interface will result in the difficulty in effective separation.Besides,some ooids are made of chamosite with some nucleus formed of quartz,which is principally finely disseminated with hematite.In view of the close association and dissemination of iron-and phosphorus-based minerals in the ooids,it is found that the process of stage-grindings and stage-separations can be adopted to effectively increase the iron recovery and decrease the P content in the concentrate to some extent.展开更多
Mineral contents and fractures of shale from well Yuye-1 and outcrops were examined mainly based on systematic description of the cores and outcrops, and data from experimental analyses. The data enabled us to thoroug...Mineral contents and fractures of shale from well Yuye-1 and outcrops were examined mainly based on systematic description of the cores and outcrops, and data from experimental analyses. The data enabled us to thoroughly explore the mineralogy and developmental features of shale of the Lower Silurian Longmaxi Formation in the study area. The results show that,the Lower Silurian Longmaxi Shale(SLS) in the southeastern margin of Sichuan Basin, China, is primarily characterized by a high content of brittle minerals and a relatively low content of clay minerals. The total content of brittle minerals is approximately 57%,including 27% quartz, 12.2% feldspar, 11.2% carbonate and 2.4% pyrite. The total content of clay minerals reaches 41.6%,composed of illite(23.8%), mixed-layer of illite and smectite(I/S)(10.8%) and chlorite(7.0%). The SLS accommodates the widespread development of various types of fractures, including tectonic fractures, diagenetic fractures, inter-layer fractures and slip fractures. The developmental level of the fracture in the SLS is mainly influenced by faults, lithology, mineral contents and total organic carbon content(TOC) in study area.展开更多
This paper presents a methodology for studying low grade lateritic nickel ore, which usually presents complex mineralogy, with widespread nickel in several mineral phases. The study is focused on determining the miner...This paper presents a methodology for studying low grade lateritic nickel ore, which usually presents complex mineralogy, with widespread nickel in several mineral phases. The study is focused on determining the mineralogy and the distribution of nickel in the bearing minerals. Laboratory assays comprise homogenization, sampling and particle size analysis. Chemical analyses by X-ray fluorescence are performed in all fractions sizes, while mineralogical assessments by X-ray diffraction are carried out for head sample. The mineralogical composition of the samples and the partition of main elements in the bearing minerals are assayed by size fraction through automated image analysis software (MLA) coupled to a scanning electron microscope (SEM). The chemical compositions of the several minerals identified in MLA are determined during systematic observations on SEM with energy dispersive spectrometer (EDS).展开更多
The effects of basicity and temperature on the reduction process of Hongge high-chromium vanadium-titanium magnetite(HCVTM)sinter were investigated in this work.The main characterization methods of X-ray fluorescence(...The effects of basicity and temperature on the reduction process of Hongge high-chromium vanadium-titanium magnetite(HCVTM)sinter were investigated in this work.The main characterization methods of X-ray fluorescence(XRF),X-ray diffraction(XRD),scanning electron microscope(SEM),and metallographic microscope were employed in this study.In this work,the reduction of HCVTM sinter with different temperature and basicity were experimented.The Fe,FeO,and TiO in reductive samples increase with increasing basicity and temperatures.The increase of basicity and temperature is favorable to the reduction of HCVTM sinter.The Fe phase has out-migration tendency to the surface of sinter while the perovskite and silicate phases have in-migration tendency to the inside of sinter.The reduction degradation index(RDI)decreases while the reduction index(RI)increases with increasing basicity.The RI increases from 67.14%to 82.09%with increasing temperature from 1073 K to 1373 K.展开更多
Using variety of modern testing methods, the processing mineralogical characteristics for a lead and zinc oxide ore in Sichuan were studied systematically. The chemical analysis result shows that the lead and zinc oxi...Using variety of modern testing methods, the processing mineralogical characteristics for a lead and zinc oxide ore in Sichuan were studied systematically. The chemical analysis result shows that the lead and zinc oxide content exceeding the minimum industrial grade and iron ore, total iron content reaches a minimum industrial grade and associated with gold and silver; The mineralogical analysis result shows that lead and zinc mineral composition and configuration are very complexity. The zinc minerals and zinciferous minerals are sphalerite, hemimorphite, Smithsonite, Hydrozincite, zinc chlorite, limonite, zinc dolomite and zincocalcite; lead minerals and plumbiferous minerals are mainly galena, cerussite, anglesite, limonite and Coronadite; The minerals disseminated grain size are very fine and mineral dissemination characteristics are very complex ; expected theoretical recoveries for lead and zinc were 72% and 67% respectively. The results of this study provide basic data and theoretical basis for ore dressing.展开更多
New attention has been given to the resources of rare earth minerals over the last years. The natural shortage of these elements in the Earth’s crust and trade restrictions recently imposed by China, motivated the Br...New attention has been given to the resources of rare earth minerals over the last years. The natural shortage of these elements in the Earth’s crust and trade restrictions recently imposed by China, motivated the Brazilian Government to encourage new projects by inserting the exploitation of rare earths in the National Mining Plan, which deals with industry strategic issues in the country, helping to reduce current importation. The incentives can be in the choice of future targets for mineral exploration and for the development of laboratory studies and pilot scale processing tests.展开更多
Sulfide oxidation by microbial activities play an important role in the release of heavy metals. An important source of contamination and formation of AMD is the heavy metals convey to soil, rivulet and groundwater. P...Sulfide oxidation by microbial activities play an important role in the release of heavy metals. An important source of contamination and formation of AMD is the heavy metals convey to soil, rivulet and groundwater. Pyrite is a commonly sulfide minerals in mine wastes, so it is vitally to prove up the microbial oxidation process.展开更多
The first International Conference on Modern Process Mineralogy and Mineral Processing, organized by the Nonferrous Metals Society of China and hosted by Beijing General Research Institute of Mining and Metallurgy,was...The first International Conference on Modern Process Mineralogy and Mineral Processing, organized by the Nonferrous Metals Society of China and hosted by Beijing General Research Institute of Mining and Metallurgy,was held on September 22-25,1992,in Beijing,China.About 350 scholars and experts from 25 countries and regions showed up at the conference and 130 papers were presented,among them 98 papers are of mineral processing.Some of the papers given in mineral processing are summed up as follows.展开更多
Genetically diverse lithologies, which include blueschist, greenschist, ultramafic, mafic plutonic, e.g. gabbros, and volcanic, e.g. pillowed basalts, and metasedimentary rocks, occur as a wedge\|shaped zone in the ar...Genetically diverse lithologies, which include blueschist, greenschist, ultramafic, mafic plutonic, e.g. gabbros, and volcanic, e.g. pillowed basalts, and metasedimentary rocks, occur as a wedge\|shaped zone in the area to the north of the Mingora town in Swat, NW Pakistan. This zone of fault\|bounded rock bodies and blocks is distinguished into three principal groups, each of which is itself a composite of lithologies, or a melange—the blueschist melange, greenschist melange and ophiolitic melange. All these lie along the Main Mantle Thrust (MMT)—the westward extension of the Indus\|Tsangbo suture zone and the locus of collision between the Indo\|Pakistan plate and the Kohistan island arc—and, are therefore, collectively termed as the Main Mantle Thrust Melange Group (MMTMG).The ultramafic rocks, locally containing chromite pods and constituting a part of the ophiolitic member of the MMTMG, occur as small to large lenticular bodies, distributed along the marginal part of the Indo\|Pakistan plate. They are invariably serpentinized to varying degrees and, therefore, consist of abundant, fine grained serpentine which is mostly accompanied by subordinate amounts of completely bastitised, medium to coarse grained orthopyroxene, trace to accessory amounts of commonly altered (zoned with ferritchromite and/or magnetite) chrome spinel, variable proportions of olivine, and accessory amounts of diopside. In other words, the ultramafic rocks are mostly harzburgitic in mineralogy and, therefore, the ophiolite as a whole can be classified as the harzburgite sub\|type..Detailed field and mineralogical studies show that the present petrographic ch aracteristics and mineral\|chemical composition of these dominantly harburgitic rocks are the result of a number of phenomena involving partial melting, serpentinization, metamorphism and talc\|carbonate alteration.展开更多
A severe Asian Dust Storm(ADS)event occurred on April 16-17th,2006 in northem China.Mineral components of dust samples were analyzed using X-ray diffraction(XRD).The result indicates that dust particles were dominated...A severe Asian Dust Storm(ADS)event occurred on April 16-17th,2006 in northem China.Mineral components of dust samples were analyzed using X-ray diffraction(XRD).The result indicates that dust particles were dominated by quartz(37.4%)and clay (32.9%),followed by plagioclase(13.7%),with small amounts of calcite,K-feldspar,dolomite,homblende, and gypsum(all【10%).The clay fractions with diameter less than 2μm were separated from the展开更多
In this paper we put forward a new concept——the ore of associated gain element. It is thought that the theoretical index forecast of dressing and smelting should be the component part of contents of technological mi...In this paper we put forward a new concept——the ore of associated gain element. It is thought that the theoretical index forecast of dressing and smelting should be the component part of contents of technological mineralogy study. The relative problems of the representativeness of ore sample, the handling of study sample and the choice of test means, and the examination of element existance form in the ore, etc., are discussed.展开更多
Located at the boundary of Chongli county, Chicheng county and Xuanhua county of Heibei province, the Dongping gold deposit is genetically affiliated to the late Jurassic- early Cretaceous volcanics and intrusives. Th...Located at the boundary of Chongli county, Chicheng county and Xuanhua county of Heibei province, the Dongping gold deposit is genetically affiliated to the late Jurassic- early Cretaceous volcanics and intrusives. The ore body is quartz vein- and alteration-type and pyrite and quartz are the dominant gold-bearing minerals.展开更多
It has been over 40 years since scientists and engineers attempted to automate optical microscope and scanning electron microscope (SEM) to measure the mineral liberation characteristics of ores in order to predict th...It has been over 40 years since scientists and engineers attempted to automate optical microscope and scanning electron microscope (SEM) to measure the mineral liberation characteristics of ores in order to predict their flotation responses. As early as 1963, the first optical instrument equipped with a video camera to analyse grain structure of a sample was produced by Metals Research Instrument Corporation (Image Analysis Company Ltd., 1970), which introduced Quantimet 720, a fully digital image analysis system, in 1969. Remarkably, Quantimet system is still widely used today.展开更多
Bolshetagninskoe deposit is one of the most important Russia niobium potential sources. It is confined to carbonatite complex of the same name that is situated in the Sayan Mountains, Eastern Siberia. In the result of...Bolshetagninskoe deposit is one of the most important Russia niobium potential sources. It is confined to carbonatite complex of the same name that is situated in the Sayan Mountains, Eastern Siberia. In the result of VIMS exploration niobium ores reserves have been applied by Russian State Reserve Committee in 2012 year. Ores contain about 1% Nb2O5 and are unique in that the economic pyrochlore mineralization is concentrated in alkaline metasomatic rocks but not in carbonatites[1]. During exploration 47 borehole samples and 6 bulk samples were collected and studied by process mineralogy techniques (optic mineralogical analyze, optic image analyzer system, XRD, EPMA). 26 borehole samples and 2 bulk samples were tested by rougher floatation to define geometallurgical items and to understand the ore’s behavior. Four volumetric samples have been tested by commissioned flowsheet (radiometric separation → impact milling → selective floatation → pyrochlore leaching → ferroniobium). There are three ore types in the Bolshetagninskoe deposit: microcline-pyrochlore (MP), biotite-columbite-pyrochlore (BCP) and carbonate-pyrochlore (CP). MP type is the most important one. MP ore consists of microcline (59wt%–70wt%) with minor carbonates, apatite, sulfides, goethite. Pyrochlore, the essential Nb mineral (94% of ore Nb content), occurs as fine grains (weighted average grain size is 57 μn). Since pyrochlore grains are fine and friable, the ore preparation size and method is a main problem of its treatment. While primary ore processing is effective to remove about 30% waste material it is important to evaluate its influence on floatation feed grade.展开更多
China produces much tungsten metal every year. The tungsten deposits in China usually are low-grade and have complex mineralogy composition as well as many associated valuable elements. The associated elements include...China produces much tungsten metal every year. The tungsten deposits in China usually are low-grade and have complex mineralogy composition as well as many associated valuable elements. The associated elements include Sn, Mo, Bi, Cu, Pb, Zn, Sb, Be, Co, Au, Ag, Nb, Ta, Re, Sc, REE, Li, As, S, P and the nonmetallic minerals such as quartz, fluorite, feldspar, etc. Therefore, only the tungsten ore dressing is done in accordance with the ore properties based on the detailed and full process mineralogy study can the valuable elements be reasonably and fully recovered and the maximization of resource utilization as well as environment-friendly is achieved eventually. This paper summarizes the status quo of process mineralogy of tungsten and its associated elements in China, focuses on the process mineralogy studies on major tungsten ore types including tungsten-molybdenum associated ore, tungsten-tin polymetallic ore and tungsten-copper polymetallic ore, suggests the future process mineralogy research on tungsten and its associated elements.展开更多
Process mineralogy of low-grade laterite nickel ore in Indonesia was systematically characterized and the beneficiation process of mineral components such as limonite,serpentine and chromite was studied on the basis o...Process mineralogy of low-grade laterite nickel ore in Indonesia was systematically characterized and the beneficiation process of mineral components such as limonite,serpentine and chromite was studied on the basis of process mineralogy.The results show that the low-grade laterite nickel ore is a typical weathering sedimentary metamorphic oxidized ore,with the main valuable elements of Ni,Co and Cr and the main mineral components of limonite,serpentine,chromite,etc.There is no independent carrier mineral of Ni and Co in the raw ore,and the occurrence states of Ni and Co are relatively dispersed.For the limonite in laterite nickel mine,the nickel bearing magnetite concentrate with nickel grade of 1.98%and recovery rate of 88.42%can be obtained by reduction roasting magnetic separation process.For the serpentine in laterite nickel mine,the cobalt bearing concentrate with Co grade of 0.17%and recovery rate of 23.17%can be obtained by positive and reverse flotation process.A chromium concentrate containing 35.17%Cr_(2)O_(3) and a recovery of 33.42%can be obtained by using the combined process of coarse and fine classification and gravity and magnetic.展开更多
Mineralization in tumours is a complex dynamic process regulated by cancerization process, organic matter, mineral crystal growth mechanism, external environment, human body environment and other aspects. Differences ...Mineralization in tumours is a complex dynamic process regulated by cancerization process, organic matter, mineral crystal growth mechanism, external environment, human body environment and other aspects. Differences between mineral crystals may imply different cancerization process and tumorous types. Therefore, the study on mineralization progress in human tumours can help to provide some important information on the occurrence and development of the diseases.展开更多
Burnt lime and serpentine were incorporated into the sinter mix to improve high iron and low silica sinte-ring. Optimization of how to use burnt lime including dosage of burnt lime, moisture of sinter mix, hydrating a...Burnt lime and serpentine were incorporated into the sinter mix to improve high iron and low silica sinte-ring. Optimization of how to use burnt lime including dosage of burnt lime, moisture of sinter mix, hydrating andgranulation time was performed. Evaluations of sinter characteristics including sinter mineralogy, reducibility, lowtemperature reduction degradation, softening and melting down properties were carried out. Compared with the re-sults of traditional process in base case, the tumbling index (TI) is increased by 1.53%-2.33% through proportio-ning high ratio of burnt lime or adding serpentine in the sinter mix. It is shown that effective granulation, better per-meability and improved high temperature reactivity in the sinter bed are achieved, resulting in an increase in 3.13 %- 5.10% calcium ferrite occurring in acicular and columnar shape and decrease in glass phase, and with the reduc-ibility index(RI) being increased by 1.65%- 3.25%.展开更多
Large plutons and dyke networks of Miocene leucogranite, magnificently exposed in Makalu, Nuptse and Cho Oyu, occur in the Cho—Oyu—Everest—Makalu Range at the top of the Higher Himalayan Crystalline (HHC) nappe and...Large plutons and dyke networks of Miocene leucogranite, magnificently exposed in Makalu, Nuptse and Cho Oyu, occur in the Cho—Oyu—Everest—Makalu Range at the top of the Higher Himalayan Crystalline (HHC) nappe and along the South Tibetan Detachment (STD). In the Kharta\|Dzakar Chu area, in the western limb of the Arun transverse anticline, discordant leucogranite dykes were found in the Precambrian—Cambrian (?) sediments of the Tibetan Series just above the STD (North Col Formation), throughout the HHC nappe, in the thrust sheets of the MCT zone (Main Central Thrust II sensu Arita, 1983) and in the underlying granite gneisses of the Lesser Himalayan Crystallines (LHC) which crop out in the Ama Drime —Nyonno Ri Range. While Miocene leucogranites in the HHC and in the Tibetan Series are known from end to end of the Himalaya, Miocene leucogranites in the MCT zone and in the Lesser Himalaya have not been frequently described.展开更多
Qara-aghaj and Skandian as hard rock titanium deposit and Kahnooj one as a placer deposit were investigated from applied mineralogical point of view. The mineralogical studies were carried out using XRD, XRF, optical ...Qara-aghaj and Skandian as hard rock titanium deposit and Kahnooj one as a placer deposit were investigated from applied mineralogical point of view. The mineralogical studies were carried out using XRD, XRF, optical microscopy, scanning electron microscopy and microprobe analysis. These studies indicated that ilmenite and magnetite are main valuable minerals in the studied ores. Pyroxene, olivine and plagioclase are the main gangue minerals in Qara-aghaj ore while chlorite and plagioclase are the major gangue minerals in Skandian ore. Plagioclase, clinopyroxene, amphibole, feldspate and some quartz are the important gangue minerals in kahnooj deposit. In all three ores ilmenite is mainly in the form of ilmenite grains but some lamellae of ilmenite with thickness between 0.1 to 20 μm have been occurred as exsolution textures inside magnetite grains, where the magnetite here can be referred to as ilmenomagnetite. In the hard rock ores some fine ilmenites have been disseminated in silicate minerals. The liberation degree of granular ilmenite was determined 150, 140 and 200 μm for Qara-aghaj, Skandian and Kahnooj, respectively. So, only the granular form of ilmenite is recoverable by physical methods. Some sphene and rutile as titanium containing minerals were observed mainly inside ilmenite phase in kahnooj ore. Some fine rutile was also found inside Skandian ilmenite while there were not any other titanium minerals inside Qara-aghaj ilmenite. Apatite is another valuable mineral which was found only in Qara-aghaj ore. Using SEM and microprobe analysis it was found that there are different amounts of exsolved fine lamellae of hematite inside ilmenite in Qara-aghaj and Kahnooj ores while it was not observed in Sckandian one. The average contents of TiO2 in the lattice of Qara-aghaj, Skandian and Kahnooj ilmenite were determined 51.13, 50.9% and 52.02%, respectively. FeO content of ilmenite lattice for all three samples is clearly lower than the theoretical content. This is due to the substitution of Mg and Mn for some Fe2+ ions in the ilmenite lattice. V2O3 content of magnetite lattice is up to 1%. So, magnetite can be a suitable source for production of vanadium as a by-product in all three deposits.展开更多
基金Project(51474161)supported by the National Natural Science Foundation of China
文摘The chemical compositions,mineralogical characteristics,as well as dissemination of iron-and phosphorus-based minerals were studied for the E’xi oolitic hematite from western Hubei Province in China by using chemical analysis,optical microscope,electron probe micro-analyzer(EPMA)and energy dispersive spectroscopy(EDS).It is found that this kind of oolitic hematite ore contains 47.71%TFe,10.96%SiO_2,as well as 0.874%P,with hematite as the dominant Fe-bearing minerals,and quartz,chamosite,illite and cellophane as main gangue minerals.The microscope examination showed that the ore has an oolitic structure,with some ooids principally formed by a series of concentric layers of hematite collophanite around nucleus that is hematite in the association with collophanite.Based on the EPMA and EDS analysis,it can be known that some ooids are primarily composed of hematite and collophanite.The separation can be achieved through fine grinding for those collophanite laminae with a higher P content.However,the dissemination of two minerals at the interface will result in the difficulty in effective separation.Besides,some ooids are made of chamosite with some nucleus formed of quartz,which is principally finely disseminated with hematite.In view of the close association and dissemination of iron-and phosphorus-based minerals in the ooids,it is found that the process of stage-grindings and stage-separations can be adopted to effectively increase the iron recovery and decrease the P content in the concentrate to some extent.
基金Project(41302076)supported by the National Natural Science Foundation of ChinaProject(BJ14266)supported by Special Fund of Ministry of Science and Technology from the State Key Laboratory of Continental Dynamics(Northwest University),China
文摘Mineral contents and fractures of shale from well Yuye-1 and outcrops were examined mainly based on systematic description of the cores and outcrops, and data from experimental analyses. The data enabled us to thoroughly explore the mineralogy and developmental features of shale of the Lower Silurian Longmaxi Formation in the study area. The results show that,the Lower Silurian Longmaxi Shale(SLS) in the southeastern margin of Sichuan Basin, China, is primarily characterized by a high content of brittle minerals and a relatively low content of clay minerals. The total content of brittle minerals is approximately 57%,including 27% quartz, 12.2% feldspar, 11.2% carbonate and 2.4% pyrite. The total content of clay minerals reaches 41.6%,composed of illite(23.8%), mixed-layer of illite and smectite(I/S)(10.8%) and chlorite(7.0%). The SLS accommodates the widespread development of various types of fractures, including tectonic fractures, diagenetic fractures, inter-layer fractures and slip fractures. The developmental level of the fracture in the SLS is mainly influenced by faults, lithology, mineral contents and total organic carbon content(TOC) in study area.
文摘This paper presents a methodology for studying low grade lateritic nickel ore, which usually presents complex mineralogy, with widespread nickel in several mineral phases. The study is focused on determining the mineralogy and the distribution of nickel in the bearing minerals. Laboratory assays comprise homogenization, sampling and particle size analysis. Chemical analyses by X-ray fluorescence are performed in all fractions sizes, while mineralogical assessments by X-ray diffraction are carried out for head sample. The mineralogical composition of the samples and the partition of main elements in the bearing minerals are assayed by size fraction through automated image analysis software (MLA) coupled to a scanning electron microscope (SEM). The chemical compositions of the several minerals identified in MLA are determined during systematic observations on SEM with energy dispersive spectrometer (EDS).
基金Project(2013CB632603)supported by the National Basic Research Program of ChinaProject(2015BAB19B02)supported by the National Key Technology R&D Program of ChinaProjects(51674084,51174051,51574082)supported by National Natural Science Foundation of China
文摘The effects of basicity and temperature on the reduction process of Hongge high-chromium vanadium-titanium magnetite(HCVTM)sinter were investigated in this work.The main characterization methods of X-ray fluorescence(XRF),X-ray diffraction(XRD),scanning electron microscope(SEM),and metallographic microscope were employed in this study.In this work,the reduction of HCVTM sinter with different temperature and basicity were experimented.The Fe,FeO,and TiO in reductive samples increase with increasing basicity and temperatures.The increase of basicity and temperature is favorable to the reduction of HCVTM sinter.The Fe phase has out-migration tendency to the surface of sinter while the perovskite and silicate phases have in-migration tendency to the inside of sinter.The reduction degradation index(RDI)decreases while the reduction index(RI)increases with increasing basicity.The RI increases from 67.14%to 82.09%with increasing temperature from 1073 K to 1373 K.
文摘Using variety of modern testing methods, the processing mineralogical characteristics for a lead and zinc oxide ore in Sichuan were studied systematically. The chemical analysis result shows that the lead and zinc oxide content exceeding the minimum industrial grade and iron ore, total iron content reaches a minimum industrial grade and associated with gold and silver; The mineralogical analysis result shows that lead and zinc mineral composition and configuration are very complexity. The zinc minerals and zinciferous minerals are sphalerite, hemimorphite, Smithsonite, Hydrozincite, zinc chlorite, limonite, zinc dolomite and zincocalcite; lead minerals and plumbiferous minerals are mainly galena, cerussite, anglesite, limonite and Coronadite; The minerals disseminated grain size are very fine and mineral dissemination characteristics are very complex ; expected theoretical recoveries for lead and zinc were 72% and 67% respectively. The results of this study provide basic data and theoretical basis for ore dressing.
文摘New attention has been given to the resources of rare earth minerals over the last years. The natural shortage of these elements in the Earth’s crust and trade restrictions recently imposed by China, motivated the Brazilian Government to encourage new projects by inserting the exploitation of rare earths in the National Mining Plan, which deals with industry strategic issues in the country, helping to reduce current importation. The incentives can be in the choice of future targets for mineral exploration and for the development of laboratory studies and pilot scale processing tests.
文摘Sulfide oxidation by microbial activities play an important role in the release of heavy metals. An important source of contamination and formation of AMD is the heavy metals convey to soil, rivulet and groundwater. Pyrite is a commonly sulfide minerals in mine wastes, so it is vitally to prove up the microbial oxidation process.
文摘The first International Conference on Modern Process Mineralogy and Mineral Processing, organized by the Nonferrous Metals Society of China and hosted by Beijing General Research Institute of Mining and Metallurgy,was held on September 22-25,1992,in Beijing,China.About 350 scholars and experts from 25 countries and regions showed up at the conference and 130 papers were presented,among them 98 papers are of mineral processing.Some of the papers given in mineral processing are summed up as follows.
文摘Genetically diverse lithologies, which include blueschist, greenschist, ultramafic, mafic plutonic, e.g. gabbros, and volcanic, e.g. pillowed basalts, and metasedimentary rocks, occur as a wedge\|shaped zone in the area to the north of the Mingora town in Swat, NW Pakistan. This zone of fault\|bounded rock bodies and blocks is distinguished into three principal groups, each of which is itself a composite of lithologies, or a melange—the blueschist melange, greenschist melange and ophiolitic melange. All these lie along the Main Mantle Thrust (MMT)—the westward extension of the Indus\|Tsangbo suture zone and the locus of collision between the Indo\|Pakistan plate and the Kohistan island arc—and, are therefore, collectively termed as the Main Mantle Thrust Melange Group (MMTMG).The ultramafic rocks, locally containing chromite pods and constituting a part of the ophiolitic member of the MMTMG, occur as small to large lenticular bodies, distributed along the marginal part of the Indo\|Pakistan plate. They are invariably serpentinized to varying degrees and, therefore, consist of abundant, fine grained serpentine which is mostly accompanied by subordinate amounts of completely bastitised, medium to coarse grained orthopyroxene, trace to accessory amounts of commonly altered (zoned with ferritchromite and/or magnetite) chrome spinel, variable proportions of olivine, and accessory amounts of diopside. In other words, the ultramafic rocks are mostly harzburgitic in mineralogy and, therefore, the ophiolite as a whole can be classified as the harzburgite sub\|type..Detailed field and mineralogical studies show that the present petrographic ch aracteristics and mineral\|chemical composition of these dominantly harburgitic rocks are the result of a number of phenomena involving partial melting, serpentinization, metamorphism and talc\|carbonate alteration.
文摘A severe Asian Dust Storm(ADS)event occurred on April 16-17th,2006 in northem China.Mineral components of dust samples were analyzed using X-ray diffraction(XRD).The result indicates that dust particles were dominated by quartz(37.4%)and clay (32.9%),followed by plagioclase(13.7%),with small amounts of calcite,K-feldspar,dolomite,homblende, and gypsum(all【10%).The clay fractions with diameter less than 2μm were separated from the
文摘In this paper we put forward a new concept——the ore of associated gain element. It is thought that the theoretical index forecast of dressing and smelting should be the component part of contents of technological mineralogy study. The relative problems of the representativeness of ore sample, the handling of study sample and the choice of test means, and the examination of element existance form in the ore, etc., are discussed.
文摘Located at the boundary of Chongli county, Chicheng county and Xuanhua county of Heibei province, the Dongping gold deposit is genetically affiliated to the late Jurassic- early Cretaceous volcanics and intrusives. The ore body is quartz vein- and alteration-type and pyrite and quartz are the dominant gold-bearing minerals.
文摘It has been over 40 years since scientists and engineers attempted to automate optical microscope and scanning electron microscope (SEM) to measure the mineral liberation characteristics of ores in order to predict their flotation responses. As early as 1963, the first optical instrument equipped with a video camera to analyse grain structure of a sample was produced by Metals Research Instrument Corporation (Image Analysis Company Ltd., 1970), which introduced Quantimet 720, a fully digital image analysis system, in 1969. Remarkably, Quantimet system is still widely used today.
文摘Bolshetagninskoe deposit is one of the most important Russia niobium potential sources. It is confined to carbonatite complex of the same name that is situated in the Sayan Mountains, Eastern Siberia. In the result of VIMS exploration niobium ores reserves have been applied by Russian State Reserve Committee in 2012 year. Ores contain about 1% Nb2O5 and are unique in that the economic pyrochlore mineralization is concentrated in alkaline metasomatic rocks but not in carbonatites[1]. During exploration 47 borehole samples and 6 bulk samples were collected and studied by process mineralogy techniques (optic mineralogical analyze, optic image analyzer system, XRD, EPMA). 26 borehole samples and 2 bulk samples were tested by rougher floatation to define geometallurgical items and to understand the ore’s behavior. Four volumetric samples have been tested by commissioned flowsheet (radiometric separation → impact milling → selective floatation → pyrochlore leaching → ferroniobium). There are three ore types in the Bolshetagninskoe deposit: microcline-pyrochlore (MP), biotite-columbite-pyrochlore (BCP) and carbonate-pyrochlore (CP). MP type is the most important one. MP ore consists of microcline (59wt%–70wt%) with minor carbonates, apatite, sulfides, goethite. Pyrochlore, the essential Nb mineral (94% of ore Nb content), occurs as fine grains (weighted average grain size is 57 μn). Since pyrochlore grains are fine and friable, the ore preparation size and method is a main problem of its treatment. While primary ore processing is effective to remove about 30% waste material it is important to evaluate its influence on floatation feed grade.
文摘China produces much tungsten metal every year. The tungsten deposits in China usually are low-grade and have complex mineralogy composition as well as many associated valuable elements. The associated elements include Sn, Mo, Bi, Cu, Pb, Zn, Sb, Be, Co, Au, Ag, Nb, Ta, Re, Sc, REE, Li, As, S, P and the nonmetallic minerals such as quartz, fluorite, feldspar, etc. Therefore, only the tungsten ore dressing is done in accordance with the ore properties based on the detailed and full process mineralogy study can the valuable elements be reasonably and fully recovered and the maximization of resource utilization as well as environment-friendly is achieved eventually. This paper summarizes the status quo of process mineralogy of tungsten and its associated elements in China, focuses on the process mineralogy studies on major tungsten ore types including tungsten-molybdenum associated ore, tungsten-tin polymetallic ore and tungsten-copper polymetallic ore, suggests the future process mineralogy research on tungsten and its associated elements.
基金Project(2019M653082)supported by the China Postdoctoral Science FoundationProject(BGRIMM-KJSKL-2020-02)supported by the Found of State Key Laboratory of Mineral Processing,China。
文摘Process mineralogy of low-grade laterite nickel ore in Indonesia was systematically characterized and the beneficiation process of mineral components such as limonite,serpentine and chromite was studied on the basis of process mineralogy.The results show that the low-grade laterite nickel ore is a typical weathering sedimentary metamorphic oxidized ore,with the main valuable elements of Ni,Co and Cr and the main mineral components of limonite,serpentine,chromite,etc.There is no independent carrier mineral of Ni and Co in the raw ore,and the occurrence states of Ni and Co are relatively dispersed.For the limonite in laterite nickel mine,the nickel bearing magnetite concentrate with nickel grade of 1.98%and recovery rate of 88.42%can be obtained by reduction roasting magnetic separation process.For the serpentine in laterite nickel mine,the cobalt bearing concentrate with Co grade of 0.17%and recovery rate of 23.17%can be obtained by positive and reverse flotation process.A chromium concentrate containing 35.17%Cr_(2)O_(3) and a recovery of 33.42%can be obtained by using the combined process of coarse and fine classification and gravity and magnetic.
文摘Mineralization in tumours is a complex dynamic process regulated by cancerization process, organic matter, mineral crystal growth mechanism, external environment, human body environment and other aspects. Differences between mineral crystals may imply different cancerization process and tumorous types. Therefore, the study on mineralization progress in human tumours can help to provide some important information on the occurrence and development of the diseases.
基金Project(2000-26) supported by the Foundation for the Teaching and Research Program for Outstanding Young Teachers in Higher Education Institutions of Education Ministry, China
文摘Burnt lime and serpentine were incorporated into the sinter mix to improve high iron and low silica sinte-ring. Optimization of how to use burnt lime including dosage of burnt lime, moisture of sinter mix, hydrating andgranulation time was performed. Evaluations of sinter characteristics including sinter mineralogy, reducibility, lowtemperature reduction degradation, softening and melting down properties were carried out. Compared with the re-sults of traditional process in base case, the tumbling index (TI) is increased by 1.53%-2.33% through proportio-ning high ratio of burnt lime or adding serpentine in the sinter mix. It is shown that effective granulation, better per-meability and improved high temperature reactivity in the sinter bed are achieved, resulting in an increase in 3.13 %- 5.10% calcium ferrite occurring in acicular and columnar shape and decrease in glass phase, and with the reduc-ibility index(RI) being increased by 1.65%- 3.25%.
文摘Large plutons and dyke networks of Miocene leucogranite, magnificently exposed in Makalu, Nuptse and Cho Oyu, occur in the Cho—Oyu—Everest—Makalu Range at the top of the Higher Himalayan Crystalline (HHC) nappe and along the South Tibetan Detachment (STD). In the Kharta\|Dzakar Chu area, in the western limb of the Arun transverse anticline, discordant leucogranite dykes were found in the Precambrian—Cambrian (?) sediments of the Tibetan Series just above the STD (North Col Formation), throughout the HHC nappe, in the thrust sheets of the MCT zone (Main Central Thrust II sensu Arita, 1983) and in the underlying granite gneisses of the Lesser Himalayan Crystallines (LHC) which crop out in the Ama Drime —Nyonno Ri Range. While Miocene leucogranites in the HHC and in the Tibetan Series are known from end to end of the Himalaya, Miocene leucogranites in the MCT zone and in the Lesser Himalaya have not been frequently described.
文摘Qara-aghaj and Skandian as hard rock titanium deposit and Kahnooj one as a placer deposit were investigated from applied mineralogical point of view. The mineralogical studies were carried out using XRD, XRF, optical microscopy, scanning electron microscopy and microprobe analysis. These studies indicated that ilmenite and magnetite are main valuable minerals in the studied ores. Pyroxene, olivine and plagioclase are the main gangue minerals in Qara-aghaj ore while chlorite and plagioclase are the major gangue minerals in Skandian ore. Plagioclase, clinopyroxene, amphibole, feldspate and some quartz are the important gangue minerals in kahnooj deposit. In all three ores ilmenite is mainly in the form of ilmenite grains but some lamellae of ilmenite with thickness between 0.1 to 20 μm have been occurred as exsolution textures inside magnetite grains, where the magnetite here can be referred to as ilmenomagnetite. In the hard rock ores some fine ilmenites have been disseminated in silicate minerals. The liberation degree of granular ilmenite was determined 150, 140 and 200 μm for Qara-aghaj, Skandian and Kahnooj, respectively. So, only the granular form of ilmenite is recoverable by physical methods. Some sphene and rutile as titanium containing minerals were observed mainly inside ilmenite phase in kahnooj ore. Some fine rutile was also found inside Skandian ilmenite while there were not any other titanium minerals inside Qara-aghaj ilmenite. Apatite is another valuable mineral which was found only in Qara-aghaj ore. Using SEM and microprobe analysis it was found that there are different amounts of exsolved fine lamellae of hematite inside ilmenite in Qara-aghaj and Kahnooj ores while it was not observed in Sckandian one. The average contents of TiO2 in the lattice of Qara-aghaj, Skandian and Kahnooj ilmenite were determined 51.13, 50.9% and 52.02%, respectively. FeO content of ilmenite lattice for all three samples is clearly lower than the theoretical content. This is due to the substitution of Mg and Mn for some Fe2+ ions in the ilmenite lattice. V2O3 content of magnetite lattice is up to 1%. So, magnetite can be a suitable source for production of vanadium as a by-product in all three deposits.
