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.
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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. 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