This standard specifies the content of "ore deposits", including mineral resources, ore deposit genesis, ore deposit types, ore field structure, ore body shape, mineralization, wall rock alteration, ore structure, structure, metallogenic belt, etc. This standard is applicable to the construction of various geological and mineral information systems, and this standard should be used for information exchange and information sharing. GB/T 9649.16-1998 Classification code for geological and mineral terms Ore deposits GB/T9649.16-1998 Standard download decompression password: www.bzxz.net
This standard specifies the content of "ore deposits", including mineral resources, ore deposit genesis, ore deposit types, ore field structure, ore body shape, mineralization, wall rock alteration, ore structure, structure, metallogenic belt, etc. This standard is applicable to the construction of various geological and mineral information systems, and this standard should be used for information exchange and information sharing.

GB/T 9649.16-1998
GB/T9649-88. was formulated in 1985. It is the national standard for the Classification Code of Geological and Mineral Terminology, and consists of 35 parts: cosmic geology, geophysics, volcanic geology, geogeology, exodynamic geology, geomorphology, geotectonics, structural geology, crystallography and mineralogy, petrology, geochemistry, rock and mineral identification, chemical analysis, geohistory and stratigraphy, paleogeography, ore deposits, coal geology, petroleum and natural gas geology, marine geology, hydrogeology, engineering geology, geothermal geography, environmental geology, geoeconomics, remote sensing geology, mathematical geology, regional geological survey, geophysical exploration, geochemical exploration, mining geology and mining, ore dressing and metallurgy, solid mineral survey and exploration, prospecting engineering, paleontology, and surveying and mapping.
The content of GB/T9649-88 "Classification Code of Geological and Mineral Terminology" is mainly to combine geological and mineral production, scientific research and various geological phenomena, collect various types of related information involved in the attributes and the nouns and terms used for the text values ​​of the qualitative description of attribute characteristics. In order to facilitate application and division of labor in compilation, and avoid duplication and omission of content, subject classification is used for compilation. After consultation, appropriate division of labor is made for the overlapping parts of the content between subjects to ensure the overall systematicity, integrity and uniqueness. Character codes are given to terms used as data items (attributes), and a coding scheme combining surface classification and line classification is adopted, which can maintain uniqueness and have sufficient room for expansion. There will be no duplicate codes when supplementing with the needs of application. Terms used as text values ​​are generally coded with numbers, which is conducive to storage and retrieval, saves space and improves processing speed.
In order to maintain the stability and unity of GB/T9649-88 national standards during implementation, the national standard authority entrusts the National Geological Data Bureau (now merged into the China Institute of Geological and Mineral Information) to be responsible for maintenance and service. Users have no right to modify it at will when using it. If there is a request for supplementation and modification, they must contact the maintenance unit and obtain the approval of the maintenance unit before it can be included in the standard content for use. It will be formally listed in this standard when this standard is revised.
After five years of application, the national standard GB/T9649-88 was revised in 1993 according to the requirements of users. Due to actual needs, only some disciplines were revised this time, and a series of standards were adopted to facilitate user use and future revisions. The principle of revision is to make appropriate supplements and modifications under the premise of keeping the overall structure unchanged. The "Mineral Deposits" discipline in the national standard GB/T9649-88 "Geological and Mineral Terminology Classification Code" was compiled by Nanjing University, and the main drafter was Liu Xiaoshan. This standard is a revision standard of the "Mineral Deposits" part of the national standard GB/T9649-88 "Geological and Mineral Terminology Classification Code", and the standard code is GB/T9649.16. There are three main revisions: First, the word "ore" is removed from the original ore type, and only the metal element name is directly called, such as "iron ore" becomes "iron", in order to be consistent with the Mineral Resources Law; second, the original ore deposit genetic type is reclassified and coded separately from the industrial type. Because it is often mixed in actual application, in order to avoid duplicate codes when mixed, the genetic type coding is slightly changed; third, a small number of data items and text value terms are added.
This standard is proposed by the Ministry of Geology and Mineral Resources.
This standard is under the jurisdiction of the China Institute of Standardization and Information Classification and Coding. This standard is organized and drafted by the China Institute of Geological and Mineral Information. This standard is managed and maintained by the China Institute of Geological and Mineral Information. The main editors of this standard are: Fu Yikai, Zhao Jingman, Ma Deyao, and Fan Zhankui. GB/T9649-88 national standard was issued on July 8, 1988. 125
1 Scope
National Standard of the People's Republic of China
Terminology Classification Codes of Geology and Mineral Resources
Mineral Deposits
The terminology classification codesof geology and mineral resources--The study of ore deposits
GB/T 9649. 16--1998
Replaces GB9649-88
This standard specifies the contents of "Mineral Deposits", including mineral resources, ore deposit genesis, ore deposit type, ore field structure, ore body shape, mineralization, wall rock alteration, ore structure, structure, metallogenic belt, etc. This standard is applicable to the construction of various geological and mineral information systems, and should be used for information exchange and information sharing. 2 Definitions
This standard adopts the following definitions.
2.1 Data item: refers to the terminology that reflects the basic attributes of various geological entities and their upper-level concepts. 2.2 Text value: refers to the term used to make a specific qualitative description of the basic attributes of geological entities. 3 Classification principles
3.1 This standard adopts the surface classification method to divide geological science into 35 major disciplines in accordance with the principles of easy compilation and use, minimizing code holes while leaving room for expansion, and strictly divides the boundaries to maintain the overall systematicity and integrity and avoid duplication and overlap of content. 3.2 A three-level tree classification is adopted under the major categories, from medium categories, small categories to basic data item names. The content levels of each discipline are different, and can be less than three levels. Under the condition that the coding capacity allows, it can also be divided into four levels. 3.3 Classification at all levels is scientific, systematic and universal. 4 Principles of word selection
4.1 Objects of word selection: terms that may be used as data items of various geological and mineral databases (including the upper-level general inclusions of data items selected from the classification sense), as well as terms used to qualitatively describe the text values ​​of data items. The selected terms are consistent with the current relevant national standards, and refer to the current various geological work specifications as much as possible.
4.2 The terms used as data items are unique in this standard. Any synonyms shall be indicated in the remarks column for reference, but shall not be used when building a database.
4.3 The word selection should be simple, clear and unambiguous. The need to establish a database is fully considered. 4.4 In order to ensure the integrity and systematicness of the "geological and mineral terminology classification code" and avoid duplication, the content already included in the basic disciplines will no longer be selected in the applied disciplines, and only the unique content of emerging disciplines and marginal disciplines will be selected. For instructions on the scope of classification word selection, see Appendix A. 4.5 Appropriately select some terms that reflect the new direction and new level of discipline development. 4.6 For the convenience of use, individual data items with high frequency of use can appear repeatedly in different disciplines, but they must be encoded with a unified code to ensure the code. Approved by the State Administration of Quality and Technical Supervision on June 17, 1998 126
Implementation on January 1, 1999
GB/T 9649. 16- 1998
Uniqueness. There may be a small amount of duplication of text values ​​under different data items. 5 Coding method
5.1 Data items are coded with no more than six Latin letters (uppercase), and are generally divided into four levels. The structure is as follows: X
Medium category Subcategory
Data item
The major categories take the Chinese phonetic initials of two Chinese characters that can reflect the meaning of the category as the code, which has a certain readability. For example, "structural geology" takes "GZ" as the code. The following is a tree-shaped nested format. The middle category and subcategory each take AZ one letter sequence to arrange. The last two are basic data items, which are relatively large in number and are arranged in AA-ZZ sequence. If there is a need for classification and there is enough expansion margin, the last two digits can also be divided into two levels. 5.2 Text values ​​are generally coded with numbers. Their length is determined by the classification needs, the number of text values ​​and the expansion margin left. Try to shorten them as much as possible to reduce the hole surplus. When the text value is graded, the digital level nesting method is adopted, and the text value code under the same data item is the same length code. Some text values ​​(such as chemical elements, strata, etc.) continue to use the original international or domestic universal character codes. 6 Use and management
6.1. Usage method
This standard is provided in two forms: written and magnetic media. Users can select the required terms and their codes from various disciplines according to their own database construction purposes as the data dictionary of their own system. 6.2 If the content of the standard cannot meet a certain need, you can propose the content to be supplemented and report it to the standard promotion management unit for supplementation in the corresponding discipline, and give a code for use. Do not add words or codes on your own. Doing so can meet the needs and maintain the stability of the standard. New content will be added when the standard is revised. 7 Code table content settings
In order to meet the requirements of different models and different output forms, the classification and code table has four columns: code, Chinese name, English translation (Latin name for paleontology) and remarks.
8 Code table for classification of mineral deposit terms
Chinese character name
Mineral deposit
Ore deposit genesis
Ore deposit type
Ore deposit genesis
General concept of mineral deposit
Mineralization
Mineralization formation
Mineralization model
Mineralization hypothesis
Source of ore-forming solution
Wall rock alteration
General transport form of ore-forming elements
Ore-forming elements Causes of precipitation
Zoning of ore deposits
Tectonic structure of ore fields
Regional metallogeny
Ore structure and texture
General concept of ore deposits
Ore minerals
Vein minerals
Ore formation
Associated minerals
Parallelized minerals
Host rock
Source layer
Mineralizer
Mineralization period
Mineralization stage
GB/T 9649.16—1998
Mineral deposit science
English translation
Genesis of mineral deposit
Types of mineral deposit
Kinds of commodities
General concept of mineral depositOre body
Ore-forming process
Metallogenic formation
Metallogenic model
Metallogenic hypothesis
Source of ore-forming solutionWallrock alteration
Transported form of ore-forming ele-ment
Precipitating cause of ore-forming ele-ment
Zonal distribution of mineral depositsStructure of orefield
Metallogeny
Texture and structure of ores Mineral deposit
Ore mineral.
Gangue
Gangue mineral
Ore formation
Associated ore
Paragenic ore
Mother rock
Country rock
Host rockbZxz.net
Protoliths
Source bed
Mineralizer
Qre magma||tt| |Mineralization epoch
Stage of mineralization
Mineralization period
Mineralization stage
DHACAQ
Chinese name
Mineralization components
Mineralizing elements
Mineral assemblage
Ore-forming fluid
Mineral assemblage
Single mineral
Main mineral
Symbiotic mineral
Associated mineral
In-penetration ore body
Blind ore body
Buried ore body
Concealed ore body
Coiled ore body
Chicken nest ore body|| tt||Lens-shaped ore body
Ring-shaped ore body
Sheet-shaped ore body
Vesicular ore body
Irregular ore body
Layered ore body
Plate-shaped ore body
Columnar ore body
Simple ore body
Saddle-shaped vein
Layer-shaped vein
Radial vein
Broom-shaped vein
Heavy film-shaped vein
Fissure vein
【Oblique vein
Imbriated vein
Chain-shaped vein
GB/T 9649. 16 -- 1998
Ore-forming fluid
Single commodity
Primary commodity
Ass associated commodity | body
Pockety ore body
Irregular ore body
Stratiform ore body
Stratoid ore body
Tabular ore body
Pipe ore body
Stockwork
Saddle reef
Ladder veins
Radiated veins
Broom-like veins
Sheeted-zone veins
Gash vein
Echelon-like veins
Imbricate veins
Chain-like veins
fracture veins
【Goose-shaped veins
Chinese name
「Alpine-type veins
1 Mineralization
Magmatic mineralization
Magmatic differentiation
Crystallization differentiation
Meltration
Residual melting
Pegmatite mineralization
Gasification hydrothermal mineralization
Activation transfer mineralization
Multi-cycle mineralization
Local enrichment
GB/T 9649.16-1998
Mineral deposit science
Alga translation
Alpine-type vein
Magmatic ore-forming processMagmatic differentiation
Fractional crystallization
Liquid immiscibility
Residual molten process
Pegmatitic ore-forming processPneumato-hydrothermal metallizationOre-forming process by mobilizationPolycyclic metallogenesis
Localization
Eastern Pacific Rise Seafloor Mineralization
Red Sea Seafloor Mineralization
High-temperature Metasomatism
Hydrothermal Effect
Deep high-temperature hydrothermal
Distant hydrothermal
Meso-deep hydrothermal
Shallow hydrothermal
Filling
Replacement
Percolation substitution Use
diffusion metasomatism
double metasomatism
selective metasomatism
alkaline metasomatism
potassium metasomatism
sodium metasomatism Effect
Alteration
Fading
Contact metasomatism mineralization
Hydrothermal metasomatism
Mineralization
Endogenous Mineralization
Volcanic mineralization
Eruption
submarine mineralization on the EastPacific Rise
Submarine mineralization in the RedSea
Pyrometasomatism
Hydrothermal process
Hypothermal process
Telethermal process
Mesothermal process
Epithermal process
Cavity filling
Metasomatism
Infiltration metasomatism
Diffusive metasomatism
Bimetasomatism
Selective metasomatism||tt ||Alkaline metasomatism
Potassium metasomatism
Sodium metasomatism
Alteration
Decolourization
Ore-forming process of contact metaso-matism
Hydrothermal metasomatism
Mineralization
Endogenic metallization
Volcanogenic ore-forming processEruptive process
Chinese name
Jet effect|| tt||Subvolcanic mineralization
Volcano hydrothermal mineralization
Weathering mineralization
Physical weathering
Chemical weathering
Difference Weathering
Laterization
GB/T 9649. 16 - 1998
Mineral Deposits
English Translation
Exhalative process
Subvolcanic ore-forming processVolcanic hydrothermal solution ore-forming process
Weathering ore-forming processPhysical weathering
Chemical weathering
Differential weathering
Iaterization
Secondary enrichment of sulfide deposits
Sedimentary mineralization
Colloid chemistry Sedimentary mineralization
Biological and chemical sedimentary mineralization
Saltification
Modern saltification
Exogenous mineralization
Upwelling current mineralization role
metamorphic mineralization
regional metamorphic mineralization
Contact metamorphic mineralization
Thermal metamorphic mineralization
Dynamic metamorphic mineralization
Ultrametamorphic mineralization
Metamorphic halogen mineralization||tt| |Stratabound mineralization
Syngenetic mineralization
Epigenetic mineralization
Hot brine mineralization
Regeneration
Selective mineralization| |tt||Mineralization Construction
Endogenous Mineralization Construction
Secondary enrichment of sulphide de-posit
Sedimentary ore-forming processSedimentary ore-forming process ofcolloidal chemistry
Biochemical-sedimentary ore-forming process
Salt precipitation
Present salt precipitation|| tt||Exogenic metallization
Ore-forming process of upwelling-curent
Metamorphic metallization
Regionally metamorphic metallizationContact metamorphic mineralizationThermally metamorphosed mineraliza-tion
Metallogenesis of dynamic metamor-phism
Ultrametamorphic ore-forming processOre-forming process of metamorphic secretion-brine
Strata-binding ore-froming processSyngenetic ore-forming processEpigenetic mineralization
Mineralization of thermal brinePalingenesis
Telescoping
Endogenetic metallogenic formationRemarks
Mechanical weathering
Aluminization
Chinese name
Endogenetic metallogenic formation Construction
Pre-geosyncline-type mineralization construction
Geosyncline-type mineralization construction
Platform-type mineralization construction
Dip-type mineralization construction||tt| |Mineralization model
Plate tectonic mineralization model
Groundwater circulation mineralization model
Sabha mineralization model
GB/T 9649.16-- 1998
Mineral Deposits
Exogenetic metallogenic formationMetallogenic formation of pregeocyn-cline type
Metallogenic formation of geosynclinetype
Metallogenic formation of plateformtype
Metallogenic formation of diwa-type(Geodeprassion)
Plate-tectonic model for metallogenesisGroundwater-circulation
metallogenic
Sabkha metallogenic model
Tungsten-tin-beryllium-niobium-molybdenum and rare earth deposit model
Porphyry copper deposit model
Porphyry molybdenum deposit model
Porphyry iron deposit model||tt| |Upwelling current mineralization model
Mineralization hypothesis
Magnetic hydrothermal mineralization theory
Side secretion theory
Down secretion theory
Regeneration mineralization theory
Thermal brine mineralization theory
Soil-based mineralization theory||tt ||Pyroclastic clock mineralization theory
Syngenetic mineralization theory
Granitic mineralization theory
Deep tectonic line mineralization theory
Mineralization concentration (metal) zone theory| |tt||Trough-platform mineralization theory
Cosmic source mineralization theory
Progressive mineralization theory
Source of mineralization solution
Supergene descending solution||tt ||「Metamorphic hydrothermal
Granitic hydrothermal
Model of tungsten-tin-beryllium-niobi-um-tantalumand rare earth depositModel of porphyry copper depositModel of porphyry molybdenum deposit
Model of porphyrite iron depositUpwelling-current metallogenic model Magmatic-hydrothermal theoryIateral secretion theory
Descending secretion theory
Palingenetic ore-forming theory Hot brine ore-forming theory Batholith hypothesis of mineralizationCupola hypothesis of mineralizationSyngenetic ore-forming theoryGranitization theory of netallizationMetallogeny of deep lineamentsTheory of concentration of metallogen-esis
Geosyncline-platform theory for metal- logenesis
Cozmogenic hypothesis of mineraliza-tion
Progressive metallogenesis
Supergene solution
Metamorphic-hydrothermal solutionGranitizational-hydrothermal solutionRemarks
KCAJAA
KCAJAB
KCAJAC
KCAJAD
KCAJAE
KCAJAF
KCAJAG||tt ||KCAJAH
KCAJAI
KCAJAJ
Chinese character name
magma hydrothermal
groundwater hydrothermal
deep circulation hydrothermal||tt ||Supercritical ore-bearing fluid
Ore-bearing hot aqueous solution
Rising solution
Descending solution
Wall rock alteration
Alteration type||tt ||Alteration zone shape
Alteration zone direction,
Alteration length||tt ||Alteration width
Alteration depth
Alteration zone name
Relationship between alteration zones
Alteration intensity
Alteration Variation zone width
Wall rock alteration
Skarnization
Potassium feldsparization
Microcline feldsparization
Orthositeization||tt ||Tianhe Petrochemical
Crystalline Chemical|| tt||Albiteization
Parasiteization
Albiteization
Alkaline pyroxeneization
Alkaline hornblendeization
Anemoniteization|| tt||nepheline
greisen
electrification
benzite
biotite
actinolite
fiber Amphibole
GB/T 9649.16-1998
矿床学
英译名
Magmatic hydrothermal solutionGroundwater hydrothermal solutionDeep circulating hydrothermal solutionSupracritical ore fluid
Ore-bearing hydrothermal solutionAscending solution
Decending solution
Types of alteration
Shape of alteration zone
Strike of alteration zone
Altered length
Altered width
Altered depth
Zonal name of alteration zoningBetween-zone relations of alterationzoning
Intensity of alteration
Width of alteration zoning
Skarnization
Potash feldspathization
Microclinization
Orthoclasization
Amazonitization
Adularization
Albitization
Scapolitization
Marialitization
Alkaline pyroxenization
Alkaline amphibolization
Aegirinization
Nephelinization
Greisenization
Tourmalinization
Axinitization
Biotitization
Actinolitization
Uralitization
汉字名
绿帘石化
钠鹦帘石化
黄铁矿化
绢云母化
石英化
玉髓化
蛋白石化
黄铁绢英岩化
赤铁矿化
绿泥石化
碳酸盐化
白云石化
方解石化
青盘岩化
蛇纹石化
粘土化
高岭石化
明矾石化
石膏化
沸石化
重晶石化
似碧玉化
绢英岩化
绢云岩化
水云母化
铁白云石化
白铁矿化
胶黄铁矿化
角岩化
透辉石化
透闪石化
蓝闪石化
白云母化
金云母化
滑石化
蓝晶石化
GB/T 9649. 16—-1998
矿床学
英译名
Epidotization
Saussuritization
Pyritization
Sericitization
Sil cification
Quartzification
: Chalcedonization
Opalization
Beresitization
Hematitization
Chloritization
Carbonatization
Dolomitization
Calcitization
Propylitization
Serpentinization
Clayization
Argillization
Kaolinization
Alunitization
Gypsification
Zeolitization
Baritization
Jasperoidization
Sericite quartzitization
Sericitolitization
Hydromicazation
Ankeritization
Marcasitization
Melnikovitization
Homfielsization
Diopsidization
Tremolitization
Glaucophanization
Muscovitization
Phlogopitization
Talcization
Kyanitization
黄铁细晶岩化
红色蚀变
变安山岩化
绿盘岩化
高岭土化
KCAJAH
KCAIAI
汉字名
蓝线石化
石墨矿化
大理石化
萤石化
叶腊石化
磁铁矿化
褐铁矿化
菱铁矿化
黄铜矿化
磁黄铁矿化
毒矿矿化
雄黄矿化
雌黄砂化
铀矿化
生石英岩化
蚀变分带带间关系
不明显
蚀变强度
「成矿元素搬运形式
」呈胶体熔液搬运
呈真熔液搬运
呈络合物搬运
呈卤化物搬运
成矿元素沉淀原因
置换反应
渗滤效应
吸收作用
胶体凝结
自然电场作用
热液系统温度变化
热液系统压力变化
矿床分带
地热分带
GB/T 9649.16-1998
矿床学
英译名
Kganitization
Graphite mineralization
Marblization
Fluoritization
Pyrophyllitization
Magnetitization
Limonitization
Sideritization
Chalcopyritization
Pyrrhotinization
Dalarnite mineralization
Eolite mineralization
Auripigment mineraliztion
Uraninite mineralization
Scondary quartzitization
Conspicuous
Transitional
I Inconspicuous
Intense
Medium
Transport by colloidal solutionTransport by true solution
Transport by complex
Transport by haloids
Substitutional reaction
Infiltrating effect
Absorption
Colloidal agglutination
Action of natural-electric fieldTemperature change of hydrothermalsystem
Pressure change of hydrothermal sys-tem
Geothermal zoning
KCAOAA
KCAOAB
KCAOAC
KCAOAD
KCAOAE
KCAOAF
KCAOAG
KCAOAH
KCAOAI
汉字名　
沉淀分带
脉动分带
顺向分带
逆向分带
水平分带
垂直分带
氧化带
还原带
矿田构造
矿床构造
成矿控制因素
成矿控制
矿床构造
导矿构造
布矿构造
储矿构造
成矿控制
构造控制
地层控制
岩性控制
古地理控制
水文地质控制
区域成矿学
成矿区域
成矿区
成矿时代
成矿区域
成矿带
成矿亚带
全球性巨成矿带
亚全球性巨成矿带
三级成矿带
四级成矿带
矿带赋存位置
矿带名称
矿带号
GB/T 9649. 16 -1998
矿床学
Precipitation zoning
Pulsative zoning
Normal zoning
Reverse zoning
Horizontal zoning
Vertical zoning
Oxidized zone
Reducing zone
Ore field
Ore district
Ore zone
Structure of mineral depositFactor of mineralizing controlMineralized control
Ore-conduit structure
Ore-distributing structure
Ore-containing structure
Structure control
Stratigraphic control
Lithologic contro!
Palaeogeographic control
Hydrogeological control
Metallogenetic region
Metallogenetic province
Metallogenetic eppch
Metallogenic belt
Sub-metallogenic belt
Global metallogenic belt
Sub-global metallogenic beltMetallogenic belt of third gradeMetallogenic belt of fourth gradeLodging position of ore zoneOre zone name
Ore zone number
！间歌分带
配矿构造
容矿构造
成矿省
金属成矿带
Palaeogeographic control
Hydrogeological control
Metallogenetic region
Metallogenetic province
Metallogenetic eppch
Metallogenic belt
Sub-metallogenic belt
Global metallogenic belt
Sub-global metallogenic beltMetallogenic belt of third gradeMetallogenic belt of fourth gradeLodging position of ore zoneOre zone name
Ore zone number
！间歌分带
配矿构造
容矿构造
成矿省
金属成矿带
Palaeogeographic control
Hydrogeological control
Metallogenetic region
Metallogenetic province
Metallogenetic eppch
Metallogenic belt
Sub-metallogenic belt
Global metallogenic belt
Sub-global metallogenic beltMetallogenic belt of third gradeMetallogenic belt of fourth gradeLodging position of ore zoneOre zone name
Ore zone number
！间歌分带
配矿构造
容矿构造
成矿省
金属成矿带
Palaeogeographic control
Hydrogeological control
Metallogenetic region
Metallogenetic province
Metallogenetic eppch
Metallogenic belt
Sub-metallogenic belt
Global metallogenic belt
Sub-global metallogenic beltMetallogenic belt of third gradeMetallogenic belt of fourth gradeLodging position of ore zoneOre zone name
Ore zone number
！间歌分带
配矿构造
容矿构造
成矿省
金属成矿带
Palaeogeographic control
Hydrogeological control
Metallogenetic region
Metallogenetic province
Metallogenetic eppch
Metallogenic belt
Sub-metallogenic belt
Global metallogenic belt
Sub-global metallogenic beltMetallogenic belt of third gradeMetallogenic belt of fourth gradeLodging position of ore zoneOre zone name
Ore zone number
！间歌分带
配矿构造
容矿构造
成矿省
金属成矿带
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