This standard specifies the data items and text values ​​of the "Petrology" discipline, including the names, structures, textures, and components of three major types of rocks, various lithofacies, occurrence of igneous rocks, magmatism, rock combinations, sedimentary patterns, sedimentary environments, sedimentary facies, and types, methods, and metamorphic structures of metamorphism. This standard is applicable to the construction of various geological and mineral information systems, determines the database standard system and data dictionary, is the basic standard for formulating various data file format standards, and provides a technical basis for information exchange and sharing. GB/T 9649.10-2001 Geological and Mineral Terminology Classification Code Petrology GB/T9649.10-2001 Standard Download Decompression Password: www.bzxz.net
This standard specifies the data items and text values ​​of the "Petrology" discipline, including the names, structures, textures, and components of three major types of rocks, various lithofacies, occurrence of igneous rocks, magmatism, rock combinations, sedimentary patterns, sedimentary environments, sedimentary facies, and types, methods, and metamorphic structures of metamorphism. This standard is applicable to the construction of various geological and mineral information systems, determines the database standard system and data dictionary, is the basic standard for formulating various data file format standards, and provides a technical basis for information exchange and sharing.

ICS35.040
National Standard of the People's Republic of China
GB/T9649.10—2001
The terminology classification codes ofgeology and mineral resources--Petrology2001-04-29 Issued
People's Republic of China
General Administration of Quality Supervision, Inspection and Quarantine
2001-12-01 Implementation
GB/T9649.10—2001
Classification principles
Word selection principles
Coding methods
Use and management
Code table content settings
8 Petrology term classification code table
Appendix A (Standard Appendix) Explanation on the scope of classification word selection
GB/T9649.10--2001
Informatization in the field of geology and mineral resources has emerged in countries around the world. my country should catch up with the world's advanced level, introduce modern information technology, and develop my country's information resources to ensure the realization of information sharing between various information systems to be built. In 1985, the national standardization department approved the establishment of the project to formulate the national standard "Geological and Mineral Terminology Classification Code", which was approved and issued in 1988. The content of GB/T9649-1988 "Geological and Mineral Terminology Classification Code" is mainly the terms used to collect the attributes involved in various types of relevant information and the text values ​​used to qualitatively describe the attribute characteristics in combination with various geological phenomena in geological and mineral production and scientific research. 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 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 supplemented as needed by the application. Terms used as text values ​​are generally coded with numbers, which is conducive to storage and retrieval, saving space and improving processing speed.
After five years of application, GB/T9649-1988 was revised in 1993 according to user requirements. 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. In order to maintain the stability of the standard, the principle of this revision is to keep the overall structure, word selection scope, classification principles, word selection principles and coding methods unchanged, and the original term code remains unchanged as much as possible, and its content is appropriately supplemented and modified. The 10th discipline "Petrology" of GB/T9649-1988 "Geological and Mineral Terminology Classification Code" was drafted by Chen Kerong, Han Tongrong, Tang Junzai and others. This standard is a revision of GB/T9649-1988 "Geological and Mineral Terminology Classification Code" Part 10 "Petrology". This revision is mainly based on the needs of building a database and the latest research results. More than 20 new terms for rock structure and structure are added; more than 300 new rock names are added, including more than 120 igneous rocks, about 10 sedimentary rocks, and more than 200 metamorphic rocks. This revision adds, deletes, and modifies more than 390 items, including more than 350 new terms.
Appendix A of this standard is the appendix of the standard.
This standard is proposed by the Ministry of Land and Resources.
This standard is sponsored by the China Standardization and Information Technology Commission. This standard is drafted by the China Institute of Geology and Mineral Resources Information. This standard is managed and maintained by the China Institute of Geology and Mineral Resources Information. The main drafters of this standard are Fu Yikai, Chen Kerong, Chen Chunzi, Zhao Jingman, Ma Deyao, Wu Zhongyu and Fan Zhankui. GB/T9649-1988 was issued on July 8, 1988. Part 10 of GB/T9649-1988 was revised for the first time on April 29, 2001. 1 Scope
National Standard of the People's Republic of China
Ma Petrology
The terminology classification codes ofgeologyand mineral resourcesPetrologyGB/T9649.10—2001
Partially replaces GB/T9649—1988
This standard specifies the data items and text values ​​of the "Petrology" discipline, including the names, structures, textures, and compositions of three major types of rocks, various lithofacies, occurrence of igneous rocks, magmatic activities, rock combinations, sedimentary patterns, sedimentary environments, sedimentary phases, types and modes of metamorphism, and metamorphic structures.
This standard is applicable to the construction of various geological and mineral information systems, determines the database standard system and data dictionary, and is the basic standard for formulating various geological data file format standards, providing a technical basis for information exchange and 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 redundancy 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 concepts of data items selected from the classification sense), as well as terms used to describe the text values ​​of data items in qualitative terms. 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 needs of establishing a database should be 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 and applied disciplines will no longer be selected, and only the unique content of emerging disciplines and marginal disciplines will be selected. For instructions on the scope of classification word selection, please see Appendix A (Appendix to the standard).
4.5 Appropriately select some terms that reflect the new direction and new level of discipline development. 4.6 For the convenience of use, some frequently used data items can be repeated in different disciplines, but they must be coded uniformly to ensure the uniqueness of the code. Approved by the General Administration of Quality Supervision, Inspection and Quarantine of the People's Republic of China on April 29, 2001 and implemented on December 1, 2001
GB/T9649.10—2001
2001-04-29. Text values ​​under different data items may be repeated in small amounts. 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:XX
Major categoryMiddle categorySmall categoryData item
Major categories take the Chinese phonetic initials of two Chinese characters that can reflect the meaning of the category as codes, which have a certain degree of readability. For example, "structural geology" takes "GZ" as the code. The following is a tree-like nested format, with the middle category and small category each taking the order of letters A to Z, and the last two are basic data items, which are relatively large in number and are arranged in the order of AA to ZZ. If there is a need for grading and there is enough margin for expansion, the last two digits can also be used in two levels.
5.2 Text values ​​are generally coded digitally. The length is determined by the need for grading, the number of text values ​​and the margin for expansion. Try to shorten it to reduce the margin. When text values ​​are graded, a digital hierarchical nesting method is used. 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 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 management unit for supplementation in the corresponding discipline, and give a code for use. You are not allowed to add words or codes on your own. In this way, you can meet the needs and maintain the stability of the standard. 7 Code table content setting
In order to meet the needs of database construction and international communication, the classification and code table has four columns: code, Chinese name, English translation (Latin name for paleontology) and remarks.
8 Petrology terminology classification code table
Petrology
Petrology
Petrology Introduction
Rock composition
Rock structure
Rock structure
Chinese name
Classification and name of rocks
Petrology diagrams
English translation
Introduction of petrology
Composition of rocks
Texture of rocks
Structure of rocks
Classification and name of rocksDiagrams of petrology
Petrological indexes (coefficients, parameters, formulas, ratios)
Colour of rocks
Petrologic phase equilibrium
Colour of rocks
Petrologic phase equilibrium igneous rock occurrence and facies of igneous rock magmatism rock assembly and genetic type of rocks genetic type
sediment
environment and sedimentation
sedimentary assemblage
Chinese character name
vertical change of sedimentation
metamorphic type and metamorphic mode
metamorphic rock isophysical series
metamorphic formation
preface to petrology
petrological classification
rock genetic theory
rock genetic classification
diagenetic mechanism
other petrological concepts
petrological classification
igneous petrology
sedimentary petrology
metamorphic petrology
compositional petrology
genetic petrology
descriptive petrology
rock morphology
rock physics
chemical petrology|| tt||Rock Tectonics
Rock Chemistry
Petrogeology
Lithology
Facies Petrology
Tectonic Petrology
Rheology
Technical Petrology
Regional Petrology
Chemical Petrology
Experimental Petrology
Sedimentary Petrology
Theory of Rock Genesis
Igneous On
Water Formation
Metamorphosis
Rock Genesis Classification
Igneous Rock
Sedimentary Rock
Metamorphic Rock
Rocks of Unknown Origin
GB/T9649.10—2001
Petrology
English Translation
Sediments
Environment and sedimentationSedimentary accosiation
Vertical variation of sedimentationMetamorphic type and genesis of tnetamorphismIsophysical series of metamorphic rocksMetamorphic formation
Classification of petrology
Doctrines of petrogenesis
Petrogenic classification
Deformation
Mechanism of rock-forming
Otherpetrologic conception
Igneous petrology
Sedimentary petrology
Metamorphic petrology
Compositional petrology
Petrogenesis
Petroography
Petromorphology
Petrophysics
Chemical petrology | Experimental petrology
Sedimentology
Plutonism
Neptunism
Transformism
Igneousrocks
Sedimentary rocks
Metamorphic rocks
Agnostogenic rocks
Igneous petrology
Rock composition
Petrology
Petrology
Igneous rocks
Postdiagenetic rocks
Secondary rocks
Crystalline rocks
Aphanitic rocks
Granular rocks
Phaneritic rocks
Glassy rocks
Semicrystalline rocks
Extrusive rocks
Intrusive rocks
Eruptural rocks
Extrusive rocks
Plutonic rocks
Semi-deep diagenetic rocks
Hypodermic rocks
Subvolcanic rocks
Volcanic rock
Isomorphic rock
Isophase rock
Single mineral rock
Multiple mineral rock
Mixed rock
Saturated rock
Unsaturated rock
Supersaturated rock
Light-colored rock
Medium-colored rock
Dark-colored rock
Mantle rock
Uniform strain
Non-uniform strain
Rotational deformation
Non-rotational deformation
Plane deformation
Pure strain
Strain ellipsoid
Chinese name
GB/T9649.10—2001
Petrology
English translation name
Bedrock
Primaryrock
Deuterogenous rock
Secondary rock
Countryrock| |tt||Mother rock
Crystalline rock
Cryptocrystalline rock
Kokkite
Phanerocrystalline rock
Vitreous rock
Hemicrystalline rock||tt ||Extrusive rock
Intrusive tock
Explosive rock
Extruded rock
Plutonic rock
Hypabyssal rock
Epizonal rock||tt| |Subvolcanic rock
Volcanic rock
Isograde rock
Isofacial rock
Monomineralic rock
Polymineralie rock
Hybrid rock
Saturated rock
Unsaturated rock
Oversaturated rock
Leucocratic rock
Mesocratic rock
Melanocratic rock
Pyrolite
Homogeneous deformation
Heterogeneous deformation|| tt||Plastic deformation
Rotational deformation
Irrotational deformation
Plane deformation
Purestrain
Deformation ellipsoid
extruded rock
subvolcanic rock
graded rock
light-colored rock
dark-colored
slip flow
Pressure lens
Viscous fluid
Snowball tectonics
Spiral tectonics
Direct sliding
Diagenesis
Magmatism||tt ||Pegmatism
Sedimentation
Metamorphism
Volcanism
Chinese character name
Other petrological concepts
Magmatic genesis type
Sediment zoning
Traction flow
Fluid dynamics Classification
Density flow type
Magma genesis type
Residual magma
Synmolten magma
Anatectic magma
Slow-source magma|| tt||Crust-derived magma
Sediment zoning
Source area
Land-derived area
Sedimentary area
Traction flow
Bed sand load
Push load
Suspended load
Dissolution load
Suspended colloid load
Suspended colloid dissolution load
Fluid dynamic classification|| tt||Newtonian fluid
Non-Newtonian fluid
Upper water flow dynamics
GB/T 9649.10-2001
Petrology
English translation
Dilation
Glidingflow
Pressure lenses
Snowball structure
Spiral structure
Strike
Translation gliding
Magmatism
Pegmatitization
Sedimentation
Metamorphism
Volcanism
Genetic type of magma
Sediment division
Tractive current
Flow regime classification
Type of density current
Besidualmagma
Syntectic magma||tt| |Anatectic magma
Mantle-derived magma
Crust-derived magma
Source area
Terrigenous province
Sedimentary province
Bed sediment||tt ||Bed load
Tractionload
Suspension loed
Dissolved load
Suspensoid load
Suspensoid-dissolved load
Newtonian fluid||tt ||Non-newtonian fluid
Laminer flow
Turbulent flow
Rapidflow
Tranguil flow
Upper flow regime
Rheological regime, soft flow
Bedload
Traction load
Suspended load
High flow regime
YSBBAA|| tt||YSBBAB
YSBBAC
YSBBAD
YSBBAE
YSBBAF
YSBBAG
YSBBAH
YSBBAI||tt| |YSBBAJ
YSBBAK||tt ||YSBBAL
YSBBAM
YSBBAN
YSBBAO
YSBBAP
YSBBAQ
YSBBAR
YSBBBA
YSBBBB
YSBBBC
YSBBBD
YSBBBE
YSBBBF
Chinese character name
Lower water flow dynamics
Transition water flow dynamics|| tt||Secret Flow type
Sediment gravity flow
Granular flow
Liquid sediment flow
Debris flow
Fluid gravity flow
Debris flow| |tt||Fluidized flow
Underwater landslide
Underwater debris flow
Rock composition
Mineral composition of rocks
Other material components of rocks
Textural components of sedimentary rocks
Chemical components
Biological components
Grain size components
Other substances in rocks Component
Isolated body
Residual body
Afterimage body
Xenosome
Charin body
Vigna body| |tt||Meteorite material
Matrix minerals
Volatile matter
Other crystals
Rock inclusions
Rock cavities
Rock Chip composition
Rock content
Crystal content
Crystal content
Agglomerate compositionWww.bzxZ.net
Agglomerate content
GB/T9649 .10—2001
Petrology
English translation name
Lower flow regime
Transition regime
Sediment gravity flows
Turbidity current||tt ||Grainflow
Liquefied flow
Debrisflow
Fluid gravity flow
Debris flow
Mudflow
Fluidingflow
Subaqueous slump
Subaqueous debris flow
Petrologic mineral compositionOther petrologic material componentTextural component of sedimentary rocksChemical composition
Organic composition
Grainic composition
Schlieren
Relict
Skialith
Xenolith
Amygdale
Metasome
Palasome
Phacoids| |tt||Colloid
Meteoric matter
Matrix mineral
Volatile component
Phenocryst
Other erystal
Peterologic enclave||tt| |Fragments
Peterologic cavity
Detritic composition
Detritic content
Crystal fragment compositionCrystal fragment content
Agglomerated composition
Agglomerated content
Low flow
Dark residual rock
Lens
YSBBBG
YSBBBH
YSBBBI
YSBBBJ|| tt||YSBBBK
YSBBBL
YSBBAL
YSBBAN
YSBBAO
YSBBAP
YSBBAQ
brecciated component|| tt||breccia content
tuff content
terrestrial component
terrestrial content
cloud glass
extreme Black glass
Dissolution phenocryst
Broken phenocryst (crystal)
Self-broken phenocryst||t t||Phenocryst
Rotational phenocryst
Other bodies
Captured crystal
Dissolved crystal
Endometrastic crystal||tt| |Metamorphosis
Rock inclusions
Xuolite inclusions
Homologous inclusions
Heterogeneous inclusions
Chinese name|| tt||Homologous inclusions
Heterogeneous inclusions||tt ||Multi-source inclusions
Inclusion groups
Anatectic dark inclusions
Volcanic debris
Plastic rock debris
Pumice-like debris
Plastic glass fragments
Rate broken glass fragments
Volcanic blocks
GB/T9649.102001
Petrology
English translation| |tt||Breccia composition
Breccia content
Tuff composition
Tuff content
Terrigenous composition
Terrigenous content
Sideromelane
Palagonite|| tt||Corrosivephenocryst
Clastic phenocryst
Autoclastic phenocryst
Metacrystal
Helicitic porphyroblast
Xenocryst
Corroded crystal
Blast crystal
Endoblast
Inclosing crystal
Host-crystal
Guest-crystal
Poikilocrystal
Poikiloblast
Dendrite
Xenolithic enclave
Enclave homoeogene| |tt||Enclave enallogene
Enclave allomorphe
Enclave antilogue
Enclave polygene
Enclave swarm
Mianthite
Pyroclast||tt| |Detritus
Plastic-detritus
Pumiceous fragment
Crystal fragment
Vitreous fragment
Plastic-vitreous fragment
Hyaloclastic vitreous fragmentVolcanicblock
Residual porphyroblast
Eyeball
Filling crystal
Dendrite
Exogenous inclusion
Pyrogenic fragment debris
flame stone, pulp debris
glassy debris
plastic glass debris
YSBBAR
volcanic slag
volcanic bomb| |tt||Splashing lava
Volcanic breccia
Volcanic breccia
Volcanic sand
Volcanic ash
Volcanic dust
Volcanic mud balls| |tt||Volcano hair
Chinese character name||t t||Volcanic exogenous debris
Non-volcanic exogenous debris
Volcanic heterogeneous debris
Organic debris
Voids in rocks||tt ||Amygdalmond hole
Dissolution hole
Texture components of sedimentary rocks
Clastic particles
Carbonate heterogeneous particles
Clastic rock matrix| |tt||Clastic rock cement
Carbonate rock matrix and cement
Clastic particles
Extremely coarse sand
Extremely fine sand||tt| |Coarse silt sand
Medium silt sand
Fine silt sand
Extremely fine silt sand
GB/T9649.10—2001
Petrology
English translation
Volcanic cinder
Volcanicbomb
Spatter
Volcanicrubble
Volcanic gravel| |tt||Voleanic sand
Volcanic ash
Volcanic dust
Volcanic mud ball
Volcanichair
Volcanic exogenic fragment
Un-volcanic exogenic fragmentVolcano-allothigenous fragmentOrganic fragment
Amygdule
Corrosion cavity
Dissolution cavity
Miarolitic cavity
Vesicle
Fumarole
Clastic grain
Carbonate allochems
Matrix of clastic rocks
Cements of clastic rocks
Matrix and cements of carbonate rocksBreccia
Gravel
Boulder
Cobble
Pebble
Granule
Very coarse sand
Coarse sand
Medium sand
Fine sand
Very fine sand
Coarse silt
Medium silt
Fine silt
Very fine silt
magma mass
ash ball
amydrange
fumarole
colossal sand
YSBCBA
YSBCBB
YSBCBC
YSBCBD
YSBCBE
YSBCBA
YSBCBB
YSBCBC
YSBCBD
Chinese character name
Carbonate heterogeneous particles
Internal debris
Bioclasts
Internal debris
Coarse sand debris
Medium sand debris
Fine sand chips||t t||Silty sand
Coarse silty sand
Fine silty sand
Compound pellet
Fecal pellet
Algae pellet|| tt||Pellets
Algae clots
Glass stone clumps
Moor clots
Biological encapsulated particles
Seepage beans||tt ||Thin-skinned porgy
Deformed porgy
Crystal paving
Metamorphic crystal song
Nuclear stone
GB/T9649.102001
Petrology
English translation
Intraclasts
Pellets
Coated grain
Bioclast
Gravel clast
Sandy clast
Coarse sandy clast
Medium sandy clast
Fine sandy clast
Silty clast
Coarse silty clast
Fine silty clast
Microclast
Mud elast
Compound pellet
Faecal pellet
Algalpellet
Pelletoid
Oolite pellet
Algal lump
Catagraph
Grapestone lump
Grumeaux
Calcispheres
Biocoatedgrain
Pisolite
Vadose pisolite
Normal ooid
Superficial ooid||tt| |Compositeooid
Eccentric ooid
Algal ooid
Deformation ooid
Crystalline ooid
Crystalloblastic ooid
Minusooid
Pseudo- ooid
Oncolites
Algalbiscuit
aggregated particles
drug clumps
algae nodules102001
Petrology
English translation
Intraclasts
Pellets
Coated grain
Bioclast
Gravel clast||tt ||Sandy clast
Coarse sandy clast
Medium sandy clast
Fine sandy clast
Silty clast
Coarse silty clast
Fine silty clast
Microclast
Mud elast
Compound pellet
Faecal pellet
Algalpellet
Pelletoid
Oolite pellet||tt ||Algal lump
Catagraph
Grapestone lump
Grumeaux
Calcispheres
Biocoatedgrain
Pisolite
Vadose pisolite
Normal ooid
Superficial ooid
Compositeooid
Eccentric ooid
Algal ooid
Deformation ooid
Crystalline ooid
Crystalloblastic ooid
Minusooid
Pseudo-ooid
Oncolites
Algalbiscuit
aggregated particles
drug clumps
102001
Petrology
English translation
Intraclasts
Pellets
Coated grain
Bioclast
Gravel clast||tt ||Sandy clast
Coarse sandy clast
Medium sandy clast
Fine sandy clast
Silty clast
Coarse silty clast
Fine silty clast
Microclast
Mud elast
Compound pellet
Faecal pellet
Algalpellet
Pelletoid
Oolite pellet||tt ||Algal lump
Catagraph
Grapestone lump
Grumeaux
Calcispheres
Biocoatedgrain
Pisolite
Vadose pisolite
Normal ooid
Superficial ooid
Compositeooid
Eccentric ooid
Algal ooid
Deformation ooid
Crystalline ooid
Crystalloblastic ooid
Minusooid
Pseudo-ooid
Oncolites
Algalbiscuit
aggregated particles
drug clumps
Tip: This standard content only shows part of the intercepted content of the complete standard. If you need the complete standard, please go to the top to download the complete standard document for free.