This standard specifies the contents of crystallography and mineralogy, including the origin, morphology, physical properties (focusing on the identification of the naked eye), chemical composition, mineral classification and name, crystallography, and geometric crystallography. This standard is applicable to the construction of various geological and mineral information systems. This standard should be used when there is information exchange to achieve information sharing. GB/T 9649.9-1998 Classification code for geological and mineral terms Crystallography and Mineralogy GB/T9649.9-1998 Standard download decompression password: www.bzxz.net
This standard specifies the contents of crystallography and mineralogy, including the origin, morphology, physical properties (focusing on the identification of the naked eye), chemical composition, mineral classification and name, crystallography, and geometric crystallography. This standard is applicable to the construction of various geological and mineral information systems. This standard should be used when there is information exchange to achieve information sharing.

GB/T 9649.9—1998
Formulated in 1985, GB/T9649—88 is the national standard for the Classification Code of Geological and Mineral Terminology, which consists of 35 parts: cosmic geology, geophysics, volcanic geology, geogeology, exodynamic geology, geomorphology, tectonic geography, structural geology, crystallography and mineralogy, petrology, geochemistry, rock and mineral identification, chemical analysis, geohistory and stratigraphy, paleogeography, mineralognomy, coal geology, petroleum and natural gas geology, marine geology, hydrogeology, engineering geology, geothermal geography, environmental geology, geological economics, 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.
GB/T9649-88 "Classification Code of Geological and Mineral Terminology" is a national standard that mainly combines geological and mineral production and scientific research with various geological phenomena, collects various types of related information, and collects the names and terms used for the text values ​​used to qualitatively describe the characteristics of minerals. In order to facilitate application and cooperate in compilation, and avoid duplication and omission of content, it is compiled using subject classification. 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 the application. Terms used as text values ​​are generally coded with numbers, which is conducive to storage, retrieval, space saving and improved processing speed.
In order to maintain the stability and unity of GB/T9649-88 national standard during its implementation, the national standard authority has entrusted the National Geological Data Bureau (now merged into the China Institute of Geological and Mineral Resources Information) to be responsible for maintenance and services. Users have no right to modify it at will during use. When there are requirements for additions and modifications, they must contact the maintenance unit and obtain approval from the maintenance unit before it can be included in the standard content for use. When this standard is revised, it will be formally included in this standard.
After five years of application, GB/T9649-88 national standard was revised in 1993 according to user requirements. Due to actual needs, only some disciplines are revised this time, and a series of standards are adopted to facilitate user use and future revisions. The principle of static revision is to make appropriate additions and modifications while keeping the overall structure unchanged. The national standard GB/T9649-88 "Classification Code for Geological and Mineral Terms" "Crystallography and Mineralogy" was written by China University of Geosciences (Beijing), and the main drafters are Weng Lingbao, Wang Du, Chen Daizhang, Liu Zhen, and Zhu Baohua. This standard is a revised standard for the "Crystallography and Mineralogy" section of the national standard GB/T9649-88 "Classification Code for Geological and Mineral Terms", and the standard code is GB/T9649.9. There are two main revisions: one is to change the mineral code in the original standard from 8 digits to 4 digits, and the other is to add 298 new minerals and terms such as elongation coefficient. The more than 4,000 minerals contained in the standard were named by the New Minerals and Mineral Nomenclature Committee (CNMMN) of the International Mineralogical Association (IMA) before the end of 1991, and the 298 newly added minerals were provided by the New Minerals and Mineral Nomenclature Professional Committee under the Chinese Geological Society and the Chinese Society of Mineralogy, Petrology and Geochemistry.
This standard was proposed by the Ministry of Geology and Mineral Resources.
This standard is under the jurisdiction of China Institute of Standardization and Information Classification and Coding. This standard was drafted by China Institute of Geology and Mineral Resources Information. The main drafters of this standard are Ma Deyao, Zhao Jingman, Fan Zhankui, Boyikai and Cao Yawen. 1
National Standard of the People's Republic of China
Terminology Classification Codes of Geology and Mineral Resources
Crystallography and Mineral Resources
The terminology classification codes of geology and mineral resourcesThe crystallography and mineralogy1Scope
GB/T 9649. 9 --- 1998
Partially replaces B964988
This standard specifies the contents of crystallography and mineralogy, including the origin, morphology, physical properties (focusing on naked eye identification), chemical composition, mineral classification and name, crystallography, and geometric crystallography of minerals. This standard is applicable to the construction of various geological and mineral information systems. All information exchanges and information sharing should use this standard. 2 Definitions
This standard adopts the following definitions.
2.1 Data item: refers to the term that reflects the basic attributes of various geological entities and their upper-level concepts. 2.2 Text value refers to the term used to describe the basic and specific qualitative description of geological entities. 3 Classification principles
3.1 This standard adopts the face classification method according to the principles of easy compilation and use and minimizing code redundancy while leaving room for expansion. It divides geological science into 35 major disciplines and strictly divides the boundaries to maintain the overall systematicity and integrity and avoid duplication and overlap of content. 3.2 Three-level tree classification is adopted under the major categories, including medium category, small category and basic data item name. The content levels of each discipline are different, which can be less than three or even four levels under the condition that the coding capacity allows. 3.3 Classification at all levels is scientific, systematic and universal. 4.1 Objects of word selection: terms that may be used as data items in various geological and mineral databases (including upper-level concepts of data items selected from the classification sense), as well as terms used to qualitatively describe the text value of data items. The selected terms are consistent with the current relevant national standards, and various current geological work specifications are referred to as much as possible.
4.2, the terms used as data items are unique in this standard. All synonyms are marked in the remarks column for reference, but they shall not be used when building the database.
4.3 The selection is simple, clear and unambiguous. The needs of establishing a database are fully considered. 4.4 In order to ensure the integrity and systematicness of the "geological and mineral term classification code" and avoid duplication, no more content is selected from the content already included in the basic disciplines and applied disciplines, and only the unique content of emerging disciplines and marginal disciplines is selected. For instructions on the scope of classification word selection, please refer to Appendix A. 4.5 Some terms that reflect the new direction and new level of discipline development are appropriately selected. 4.6 For the convenience of use, individual frequently used data items may be repeated in different disciplines, but they must be encoded in a unified way to ensure the uniqueness of the code. The text values ​​under different data items may be repeated at least. The State Administration of Quality and Technical Supervision approved 199806-17 12
1999-01-01 implementation
5 Coding method
GB/T 9649. 9—1998
5.1 Data items are coded with Latin letters (uppercase) of no more than six digits, and are generally divided into four levels, as follows: x
Category Subcategory
Data Item
The major categories use the Chinese phonetic initials of two Chinese characters that can reflect the meaning of the category as the code, which has a certain readability, such as "Geology" takes \GZ\ as the code. The following is a tree-shaped nested format, with the middle category and subcategory arranged in alphabetical order of AZ digits respectively. The last two digits are basic data items, which are relatively large in number and are arranged in the order of AA-ZZ. If there is a need for classification and there is enough expansion margin, the last two digits can also be divided into two 5.2 Text values ​​are generally coded digitally, and their length is determined by the level, the number of text values, and the margin left for expansion. They should be as short as possible to reduce the margin. When text values ​​are graded, digital hierarchical embedding is used, and the text value codes under the same data item are equal-length codes. Some text values ​​(such as chemical elements, strata, etc.) continue to use the original international or domestic common character codes. 6 Use and management
6.1 How to use
This standard is provided in both written and magnetic media forms. Users can select the required terms and codes from various disciplines according to their own database construction purposes as the data dictionary of their own systems. 6.2 If the content of the standard does not meet a certain requirement, you can propose the content to be supplemented and report it to the standard management unit for supplementation in the corresponding subject, 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.
B Code table for classification of mineralogy and mineralogy terms 13
IKWAAE
Chinese character name
Crystallography and mineralogy
Crystallography
Mineralogy
Crystallography
Crystallogenesis
Ji Ke crystallography
Structural crystallography
Crystallization chemistry
Crystallogenesis
Type of crystallization
Heat of crystallization
Crystallization pressure
Crystallization temperature
Nucleation
Nucleation rate
Nucleation time
Nucleation energy| |tt||Crystal Growth Factors
Crystal Growth Conditions
Crystal Imperfection
Nucleation Rate
Crystalization Type
Melt Crystallization
Liquid Crystallization
Gas Crystallization
Quarterly Crystallization
Nucleation
Nucleation Center
Spontaneous Nucleation
Crystal Nucleus Growth
Crystal Growth Factors
Growth Plane
Growth Step
Growth Stripe
Growth Layer
Growth Zone
GB/T 9649. 91998
Crystallography and Mineralogy
English Translation
Crystallography
Mineralogy
Crystallogeny
I Geometrical crystallographyStructural crystallography
Crystal chemistry
t||Crystallization pressure
Crystallization temperature
Nucleation
Nucleation Tate
Nucleation time
Nucleation energy
Element of erystal growth
I Condition of crystal growthCrystal imperfection
Nucleation frequency
[ Crystallization from melt
Crystallizatisn from solutionI Crystallizetion Irom vapaurCrystallization by cooling
Crystal nucleus
I Nucleating center
Spontaneous rucleation
I Nucleus growth
Crystallite
Cluster
I Growth surlace
Grawth step||t t||Growth striation
Growth lamellae
Grawth zoning
DWHAAE
DWHABA
KWAAJC
KWAAJD
SYEFAE
KWAAJF
KWAAJG
KWAAKA
KWAAKB
KWAAKA
KWAAKB
Chinese character name
Growth line
Growth direction
Growth interface
Growth characteristics
Growth rate
Growth rhythm
Growth process
Crystal growth conditions||tt| |Media pH
Redox potential
Crystal imperfection
Defect structure
Defect structure
Point defect
Misplacement defect
Vacancy defect
Impurity defect
Linear defect
Surface defect
Row and column dislocation
Screw pin
Stacking fault
Growth defect
Mosaic structure
Positive thread
Negative thread
Geometric crystallography
Geometric elements of crystal
Degree of crystallinity
Basic properties of crystal
GB/T 9649. 9 1998
Crystallography and mineralogy
English translation
Growth line
Growth velocity
Grnwth inierface
Growth habit
Growth rate
Growth rhythm
Process of growth
Temperature
:Pressure
Concentration
Impurity
Viscosity
Acid-base degree of media
Redox potential
Defect structure
Spiral striation
Dislocation
Point defect
Mislocation defect (Frenkel defect)Vacency defect(Schottky defect)[mpurity defect (Interstitial defect)Line defect(Dislocation)
Plane defect
Edge dislocation(Row dislocation)Screw dislocation
Stacking feult
Growth defect
Domain
Mosaic structure
Positive spiral striation|| tt||Negative spiral striation
Geometric element of crystalGrystallinity af erystal
I Basic property pf crystal
reverse thread
KWARBDA
KWABDB
KWABDC
KWABDD
KWARDE|| tt||KWABEA
KWABEB
Hanning name
Crystal symmetry key points
Classification of body symmetry
Crystal morphology
Crystal orientation| |tt||Geometric elements of crystals
Degree of crystallinity of crystals
Crystallinity
Microcrystalline
Amorphous||t t||cryptocrystalline
liquid crystal
amorphous
transformed into amorphous
1 basic properties of crystal
"self-limiting| |tt||Homogeneity
Anisotropy
Symmetry
Stability
Crystal symmetry requirements
Symmetry plane
Symmetry Center
Symmetry axis
Rotation reflection axis
Translation anti-extension axis
Type of crystal system
Monoclinic
Crystal symmetry Classification
『Types of crystal systems
GB/T 9649.91998 ||tt || Crystal face
Crystal edgr
I Crystalline
iMicrocrystalline
' Phaneric
Cryptocrystalline
:Liquid crystal
iAmotphous| |tt||:Metarnict
Property of self-confinementEniformity
Anisotopy
Symmetry
Stability
Symmeiry plane
Symmetry center
Symmetry axis
Rotoreflection axis
, Rotoinversion axis
Isometric
Hexagonal
Trigonal|| tt||Tetragonal
Crthorhombie
Monoclinic
Triclinic
Kind of crystal system
Crystal category
Personality
KWABEC
KWABEE
KWABED
KWABFA
KWABFB
KWARFC
KWABFD
KWABFA
Chinese name
Class of the type
Type of symmetry
Laue symmetry
Heteropolar Symmetry type
Enantiosymmetry type
Crystal form
Types of single form
General form
Types of special form
Single form Types
Parallel effective surface
Reflection double surface
Axis double surface
Rhombic prism
Rhombic tetrahedron|| tt||Omnidirectional single cone
Omnidirectional double cone
Triangular prism
Compound triangular prism
Quadrangular prism
Compound quadrangular prism||tt| |Hexagonal column
Compound hexagonal house
Trigonal single cone
Compound trigonal single cone
Quadrilateral sheep shop
Compound quadratic single cone
Hexagonal simple pyramid·
Compound hexagonal simple pyramid||t t||Trigonal bipyramid
Compound bipyramid
Tetragonal bipyramid
Compound tetragonal bipyramid
Hexagonal bipyramid
Compound hexagonal bipyramid
Tetragonal tetrahedron
CB/T9649.9—1998
Crystallography and mineralogy
English translation
Crystalclass
Kind of Symrnetry type
Laueclass
Heteropola:class
Enantiomorphous class
Kind of sinple forn
General form
Kind of special forrm
i Combined form
Pedion||tt ||Pinacoid
Sphenoid
Rhombic prism
Rhombic disphenoid
Rhombic Pyramid
Rhombic dipyramid
Trigonal prism
Ditrigonal pristn
Tetragonal prism
Ditetragonal prism
Hexagonal prisn
Dihexagonal prism
Trigonal pyramid
Ditrigonal pyramid
Tetragonal pyramid
Ditetragonal pyramid
Hexagonal pyramid
Dihexagonal pyramid
Trigonal dipyramid
Ditrigonal dipyramid
Teiragonal dipyramid
Ditetragonal dipyramid
Hexagonal dipyramid
Dihexagonal dipyramid
Tetragonal disphenoid
KWABFC
KWAPGA
KWABGB
KWABGC
KWABGD
KWABGE
KWABGF
KWABGG| |tt||KWABGH
KWAEGI
Chinese character name
Rhombohedron
Tetragonal trigonal body
Compound digonal scalenohedron
Trigonal Trapezohedron
Tetragonal Trapezohedron
Hexagonal Ublique
Tetrahedron
Triangular Trihedron
Angular Tritetrahedron|| tt||Five corners tri-tetrahedron
hexa-tetrahedron
octahedron
triangular trioctahedron
tetragonal trioctahedron
pentagonal trioctahedron||tt ||Hexahedron
: Cube
Tetrahexahedron
Rhombic dodecahedron
Pentadecahedron
Triangular compound dodecahedron||tt ||Special shape types
Heteropolar shape
Crystal orientation
Crystal coordinate axis
Crystal plane index
Crystal plane symbol||tt ||Single shape symbol
Zone symbol
Axis unit
Structural crystallography
Space lattice element
GB/T 9649. 9—1998
Crystallography and Mineralogy
English Translation
Rhombohedron
Tetragonal scnlenohedren
Trigonal scalenohedron
Trigonal trapezohedron| |tt||Tetragonal trapezohedron
I Hexagonal trapezohedron
Teirahedron
Tristerrahedron
Deltohedron
Tetartoid
Hextetrahedron
Octehedron
Trisoctahedran
Trapezohedron
Gyroid
Hexuctahedron
Tetrahexahedron
Dodecahedron
Pyritohedron
Diploid
Hemimorphic form
I.eft-handed form
Right- handed farm
Positive form
Negative form
Crystel coordinate axis
Axial ratio
Indices of crystal face
Symbol of crystal face| |tt||Crystal axis
: Symbol ol sirmple form
Symbol of crystal zone
Axial unit distance
I Interaxial angle
Element of space lattice
axis unit ratio
lattice symbol
KWACCA
KWABG1
KWACCC
KWACCD
YKBGBO||tt ||KWACCF
YKRGBN
KWACCH
KWACCI
KWACCJ
KWACCK
KWACCL
KWACCM
KWACCF
KWACDA
KWACDB
KWACDC
Chinese character name
Space grid type
Unit cell parameters
Crystal structure arrest Symmetry elements
Equivalent point system
Space group symbol
Coordination structure
Space lattice elements
Space lattice type
Primitive lattice
Body-centered lattice
Face-centered lattice
Bottom-centered lattice
Heterohedral lattice
Cell parameters
Unit of measurement|| tt|| Surface density
Surface spacing
Node spacing
Unit cell volume
Atomic valence
Surface mesh symbol
Degree of Unit
Hihui meter
KX unit
Symmetry element of crystal structure
Translation axis
Slip plane
Symmetry axis of spiral family
GB/T 9649. 9—1998
Crystallography and Mineralogy
English translation
Type of space lattice
Unit cell parameter
Symmetry element of crystal structureEquivalent point system
Symbol of space group
Coordination structure
Unit cell
Primitive lattice
Body-centered laltice
Face-centered lattice| |tt||Base-centered lattice
Rhombohedral lattice.
Axial length
Interaxial angle
[ Bond number
Bond order
Bond length
Measurement unit
Bond angle
Planar net density
Interplanar spacing
Distance of lattice point
Volume of anit cell
Valence state
Symbol of net|| tt||Angstrom
Milli-rnicron
Kilo-X unit
Translation axis
:Glideplane
Serew axis
KWACDD
KWACPE
KWACEA
KWACEB
KWACEC
KWACED
KWACEE
KWACEF| |tt||KWACFA
KWACFB
KWACFC
KWACFD
KWACGA
KWACGB
KWACGC
KWAC GD
KWACGE
KWACGF
KWACGG
KWACGH
KWACGB
KWACGD
KWACGE
KWACGF| |tt||Chinese character name
Antisymmetric
Polychromatic symmetry
Equivalent point system
General equivalent point system
Special equivalent point system
Equivalent position group
Number of repeated points in equivalent point system
G#/r 9649. 91998
Crystallography and mineralogy
English translation
Antisymmetry
Color symmetry
General equivalent point systemSpecial equivalent point systemFquiyalent positiongroup||tt| |Repeat point number af eguivalentPoint
Equivalent position group repeat position number
Equivalent point coordinate value
Space group symbol
International symbol
Crystal International symbol for cell orientation
Sanforis symbol
1Sanforis-International symbol
Coordination structure.
Coordination polyhedron type||tt ||Cation radius ratio
Coordination polyhedron connection mode
Close packing mode||tt ||Empty type
Crystal structure basis
Ligand
Coordination polyhedron type
Triangle
Tetrahedron
Octahedron
Cube
Branched octahedron
Coordination polyhedron connection mode
Co-preparation
Close packing mode
Cubic close packing| |tt||Hexagonal Close Packing
Empty Type
Tetrahedron
Repeat position unmber of eyuivalentposition
Coordinate value of equivalent poinInternational symbol
International symbol of other orientatipSchoenflies symbol
Schoenflies-international symbolCoprdination number
Type of coordination polyhedronCation-anion radius ratio| |tt||Connection type of coordination poly-hedron
Type of close packing
Holetype
I Motif of crystal structureLigand
Trigonal
Tetrahedral|| tt||jOctahedral
Cuboctahedral
Share apex
Share edge
Share plane
Cubic close packing
Hexagonal close paeking
Tetrahedral
Two-color symmetry
KWACGG
KWADAB
KWADAC
KWADAD
KWADAE
KWADAF
KWADAG
KWADAH
KWADAA
Chinese character name
Octahedron
Crystal structure basis type
Coordination basis type
Frame-like base type
Ring-like base type
Island-like base type
Chain-like base type
Layer-like base type
Crystal chemistry
isotope Image
Homogeneous polymorphism
Types of ordered structures
Disordered structures
Completely disordered
Degree of order
Three Slope
Superstructure
Superpoint group
Subcell
Crystal field stabilization energy
Octahedral selective position energy
Isomorphism
Isomorphism replaces species
Isomorphism series
Isomorphism mixed characters
Guzuolirong
Isomorphic mixture
interstitial solid bath
substitutional solid solution
lacunarity solid solution
isomorphic substitution type
no Completely
GB/T 9649.9 -1988 |Ring molif (paitern)
Insular motif (pattern)
Chain motif (pattern)
Layer motif (pattern)
Iaomorphous
Palymorph|| tt||Palytype
Morphotropy
Order structure type
Disorder structure
Complete disorder
Degree of order
Trielinicity||tt| |Super-structure
Super-lattice
Suhcell
Isotype
Homotype
Heterotype
Crystal field stabilization
energy
(CFSE)
eenergy
Octahedral site preference
(OSPE)
Type of isomorphous substitutionIsomorphous series
Isomorphous addition
Exsolution of aolid-solutionIsomorphous mixture
Interstitial solid solutian||tt ||Substitutional solid solutionOmission solid solution
Perfect
Imperfect
KWADAR
KWADBA
KWADBB
KWADBC
KWADBA| tt|多像变性情度
同贝多像变体
同贝多像变态引语
位秘是
可变性变体
双变性是|| tt||单变性这些
有序有序学么
长程有序
短程有序
完全有序
小有序|| tt||局域有序
红物学
红物学图像
红物物手机
红物北京可以
红物移动国院||tt| |水物成因成因
水物成因公司
线物手机学学
线物所物学教公园
水物学学学
经经物物学
北京约吻学
结果约物学
手机约物学
成固硬物学
迷变约物学
约床约物学||tt ||找约约物学
结果约物学
GB/T 9649. 91998
kristalsis学及约物学
Equal valent
Unequal valent| |tt||Continuous
Discontinuous
Type of polymorphic transitionPolymorphic transition temperaturePolymorphic modification
Displacive irversion
Reconstructive inversion
Enantiotropic inversion
Monotropy inversian
Long-range order
Short-range order
Perfect order
Part order
Local order
Classification of mineralogyMorphology of mincrals
Chemical composition of mineralsPhysical properties of mineralsGenesis of minerals
Genetic classification of mineralsApplied classification of mineralsCrystallochemical classification of mine Physical mineralogy
Chemical mineralogy
Structure mineralogy
Morphological mineralogy
Genetic mineralogy
Alterrealion mineralogy
Mineralogy of ore-deposits
(Ore-finding mineralogy
Experimental mineralogy.91998
结晶学及矿物学
Equal valent
Unequal valent
Continuous
Discontinuous
Type of polymorphic transitionPolymorphic transition temperaturePolymarphic modification
Displacive irversion
Reconstructive inversion
Enantiotropic inversion
Monotropie inversian
Long-range order
Short-range orderbzxz.net
Perfect order
Part order
Local order
Classification of mineralogyMorphology of mincrals
Chemical composition of mineralsPhysical properties of mineralsGenesis of minerals
Genetic classification of mineralsApplied classification of mineralsCrystallochemical classification of mine Physical mineralogy
Chemical mineralogy
Structure mineralogy
Morphological mineralogy
Genetic mineralogy
Alterealion mineralogy
Mineralogy of ore-deposits
(Ore-finding mineralogy
Experimental mineralogy.91998
结晶学及矿物学
Equal valent
Unequal valent
Continuous
Discontinuous
Type of polymorphic transitionPolymorphic transition temperaturePolymarphic modification
Displacive irversion
Reconstructive inversion
Enantiotropic inversion
Monotropie inversian
Long-range order
Short-range order
Perfect order
Part order
Local order
Classification of mineralogyMorphology of mincrals
Chemical composition of mineralsPhysical properties of mineralsGenesis of minerals
Genetic classification of mineralsApplied classification of mineralsCrystallochemical classification of mine Physical mineralogy
Chemical mineralogy
Structure mineralogy
Morphological mineralogy
Genetic mineralogy
Alterealion mineralogy
Mineralogy of ore-deposits
(Ore-finding mineralogy
Experimental mineralogy.
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