Id; Navn; Beskrivelse; Stereotype; Versjon; Status; Pakke; NavPakke;
EAID_0D15D37C_98A1_4db8_8F07_041B5623F514;Context Diagram : AlterationDescription;;diagram;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-CoreGeoSciML-Core
EAID_5AB07B10_7571_4539_B31B_3816F90D11DE;Context Diagram : MetamorphicDescription;;diagram;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-CoreGeoSciML-Core
EAID_89DF4ED4_7563_46fd_AC3F_DD579905D1D7;Context diagram: CompoundMaterial;;diagram;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-CoreGeoSciML-Core
EAID_43274B1A_89A7_4f29_A616_206A94F9A565;Context diagram : EarthMaterial;;diagram;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-CoreGeoSciML-Core
EAID_AADEC3A2_3243_4715_A4A5_E4948137B615;Context diagram : OrganicMaterial;;diagram;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-CoreGeoSciML-Core
EAID_3CF8E487_B4B5_46f8_ADAF_3A40A6B6DE98;Context diagram : RockMaterial;;diagram;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-CoreGeoSciML-Core
EAID_3D41101C_FCC0_4aee_BBC9_80D7534C8105;Summary diagram : Earth Material;;diagram;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-CoreGeoSciML-Core
EAID_EA1BA5F4_3D13_4347_B18E_D3CD7973C04D;Context diagram : InorganicFluid;;diagram;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-CoreGeoSciML-Core
EAID_973E46DA_FA36_4616_B620_3C48D9D47C77;Context diagram : Mineral;;diagram;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-CoreGeoSciML-Core
EAID_32D2EEFF_FD36_48bd_ADAE_681CEA5F4278;Context Diagram : ConstituentPart;;diagram;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-CoreGeoSciML-Core
EAID_E29DEBA6_39CE_4ee0_B92C_3B5536B69757;Context Diagram : MaterialRelation;;diagram;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-CoreGeoSciML-Core
EAID_4DBE1031_6404_4048_955E_5DE32E76AD18;Context Diagram : ParticleGeometryDescription;;diagram;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-CoreGeoSciML-Core
EAID_237B1097_F86A_48b7_A9A8_3DF56B1FB007;Context Diagram : Chemical Composition;;diagram;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-CoreGeoSciML-Core
EAID_61E62BC2_0118_45a9_B7E6_36FC1168F7BA;Context Diagram : FabricDescription;;diagram;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-CoreGeoSciML-Core
EAID_038755DA_C5B6_4c44_B5FD_0FF9487F30A7;MetamorphicDescription;"MetamorphicDescription describes the character of metamorphism applied to a CompoundMaterial or GeologicUnit using one or more properties including estimated intensity (grade; eg high grade, low grade), characteristic metamorphic mineral assemblages (facies; eg, greenschist, amphibolite), peak P-T estimates, and protolith material if known.";datatype;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\EarthMaterial
EAID_0B0B1F78_C400_40f5_B143_9DA4B8617B94;FabricDescription;"The FabricDescription class describes all types of fabrics associated with a CompoundMaterial (ie, tectonic, metamorphic, sedimentary, igneous fabrics or textures).  It denotes a pattern, defined by one or more CompoundMaterial constituents, that is present throughout a rock body when considered at some scale.  FabricDescription is defined based on the average configuration of many constituents.  Penetrative fabric denotes that these constituents are distributed throughout the rock volume at the scale of observation [Passchier and Trouw, 1998], and are repeated at distances that are small relative to the scale of the whole, such that they can be considered to pervade the whole uniformly (Turner and Weiss [1963] p. 21-24; Hobbs and others [1976], p. 73; Jackson [1997]; Passchier and Trouw [1998]).   FabricDescription is distinguished from Particle Geometry based on the criteria that Particle Geometry is preserved if a CompoundMaterial is disaggregated, while FabricDescription is not defined if the material is disaggregated.  Use gml:description to capture any free text to indicate any specific or peculiar features of the described fabric in the CompoundMaterial.";datatype;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\EarthMaterial
EAID_3CE3E953_2630_46d3_99FF_C2BD75FA3489;AlterationDescription;AlterationDescription decribes aspects of a geologic unit or earth material that are the result of bulk chemical, mineralogical or physical changes related to change in the physical or chemical environment. Includes weathering, supergene alteration, hydrothermal alteration and metasomatic effects not considered metamorphic.  A soil profile description would have to be constructed as a GeologicUnit with unit parts representing the various horizons in the profile.  Thickness of a weathering profile can be delivered as unitThickness of an AlterationUnit. ;datatype;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\EarthMaterial
EAID_6DB21756_EB7B_40f5_B24D_1D3692F3B467;MaterialRelation;The MaterialRelation class describes the relationships between constituent parts in an Earth Material (eg: A mineral overgrowth on a phenocryst within a granite).   Relationships are always binary and directional.  There is always a single source and a single target. The relationship is always defined from the perspective of the Source and is generally an active verb.  Example:  Consider an overgrowth of albite on plagioclase in a granite.  The  Source would originate with the albite constituentPart description.  In this case, the Target would point to the plagioclase constituentPart description and the relationship attribute would be 'overgrowth' and the sourceRole is 'overgrows'.  Other appropriate role attributes might include: crosscuts, replaces, etc. for crosscutting and replacement relationships.  Inverse relationships must be explicitly recorded as well or else they are invisible.;datatype;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\EarthMaterial
EAID_A242BAC8_A862_4fae_B42A_F720225E1212;ChemicalComposition;;datatype;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\EarthMaterial
EAID_ED53E456_2F3B_49e9_A327_E693EA5A6545;ParticleGeometryDescription;ParticleGeometryDescription describes particles in a CompoundMaterial independent of their relationship to each other or orientation. It is distinguished from Fabric in that the ParticleGeometryDescription remains constant if the material is disaggregated into its constituent particles, whereas Fabric is lost if the material is disaggregated.  Properties include the particle size (grainsize), particle sorting (size distribution, eg: well sorted, poorly sorted, bimodal sorting), particle shape (surface rounding or crystal face development, eg: well rounded, euhedral, anhedral), and particle aspectRatio (eg: elongated, platy, bladed, compact, acicular).;datatype;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\EarthMaterial
EAID_4A253631_B9AC_49b2_AED3_1F6E12DD1CD3;ConstituentPartRoleTerm;Refers to a vocabulary of terms describing the role played by a constituent part of a compound material (eg, matrix, phenocryst) ;kodeliste;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\EarthMaterial
EAID_5FD3D066_DB4A_44aa_B738_EB6778724F82;MaterialRelationSourceRoleTerm;Refers to a vocabulary of terms describing the role that the source material plays in a relationship between two constituent parts of a compound material (eg, quartz(source) overgrows plagioclase phenocrysts) ;kodeliste;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\EarthMaterial
EAID_6D925B55_0946_4d7f_A16D_7342B69DFED9;FabricTypeTerm;Refers to a vocabulary of terms describing the type of fabric present;kodeliste;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\EarthMaterial
EAID_9EECEA41_AEC0_4268_B7A1_8510593547F9;LithologyTerm;Refers to a vocabulary of terms describing the lithology of the compound earth material (eg, granite, sandstone, schist);kodeliste;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\EarthMaterial
EAID_A55B98CE_6914_4fff_8B1E_05124ECDD328;ParticleTypeTerm;Refers to a vocabulary of terms describing the type of particle in the compound earth material (eg, bioclast, phenocryst, pyroclast);kodeliste;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\EarthMaterial
EAID_B88B95D5_B32F_4765_AFE7_341E934CCA4F;MaterialRelationshipTypeTerm;Refers to a vocabulary of terms describing to type of relationship between two constituent parts of a compound material ;kodeliste;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\EarthMaterial
EAID_BDC1CDCE_4984_48a3_8EA3_FC841E7C8CA3;MineralNameTerm;Refers to a vocabulary of mineral names ;kodeliste;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\EarthMaterial
EAID_038755DA_C5B6_4c44_B5FD_0FF9487F30A7;metamorphicFacies;A description of characteristic mineral assemblages indicative of certain metamorphic P-T conditions. Examples include Barrovian metasedimentary zones (eg: biotite facies, kyanite facies) or assemblages developed in rocks of more mafic composition (eg: greenschist facies, amphibolite facies). ;egenskap;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\EarthMaterial\MetamorphicDescription
EAID_038755DA_C5B6_4c44_B5FD_0FF9487F30A7;metamorphicGrade;A term to indicate the intensity or rank of metamorphism applied to an EarthMaterial (eg: high metamorphic grade, low metamorphic grade) Indicates in a general way the P-T environment in which the metamorphism took place. Determination of metamorphic grade is based on mineral assemblages (ie, facies) present in a rock that are interpreted to have crystallized in equilibrium during a particular metamorphic event. ;egenskap;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\EarthMaterial\MetamorphicDescription
EAID_038755DA_C5B6_4c44_B5FD_0FF9487F30A7;peakPressureValue;A numerical value to indicate the estimated pressure at peak metamorphic conditions. ;egenskap;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\EarthMaterial\MetamorphicDescription
EAID_038755DA_C5B6_4c44_B5FD_0FF9487F30A7;peakTemperatureValue;A numerical value to indicate the estimated temperature at peak metamorphic conditions. ;egenskap;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\EarthMaterial\MetamorphicDescription
EAID_038755DA_C5B6_4c44_B5FD_0FF9487F30A7;protolithLithology;An interpretation of the EarthMaterial that constituted the pre-metamorphic lithology for this metamorphosed CompoundMaterial.;egenskap;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\EarthMaterial\MetamorphicDescription
EAID_0B0B1F78_C400_40f5_B143_9DA4B8617B94;fabricType;Attribute to denote the type of fabric in the CompoundMaterial (eg, rapikivi texture, autobrecciation, spaced cleavage, porphyroblastic, cross-bedding).  The fabricType describes a pattern, defined by one or more CompoundMaterial constituents, that is present throughout a rock body when considered at some scale. FabricDescription is defined based on the average configuration of many constituents. Penetrative fabric denotes that these constituents are distributed throughout the rock volume at the scale of observation [Passchier and Trouw, 1998], and are repeated at distances that are small relative to the scale of the whole, such that they can be considered to pervade the whole uniformly. ;egenskap;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\EarthMaterial\FabricDescription
EAID_3CE3E953_2630_46d3_99FF_C2BD75FA3489;alterationType;AlterationType is a general description of the dominant alteration mineralogy or alteration type, in common usage.  Examples include: argillic, phyllic, potassic, propylitic, calc-silicate, skarn, deuteric, greisen, serpenitisation,  weathering, etc. ;egenskap;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\EarthMaterial\AlterationDescription
EAID_3CE3E953_2630_46d3_99FF_C2BD75FA3489;alterationDegree;AlterationDegree is a term to specify degree of modification from original material.  eg: weak, moderate, strong, intense ;egenskap;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\EarthMaterial\AlterationDescription
EAID_3CE3E953_2630_46d3_99FF_C2BD75FA3489;alterationProduct;AlterationProduct is the material result of alteration processes, e.g. alteration minerals, saprolite, ferricrete, clay, calcrete, skarn, etc. Materials observed in a soil profile could be identified using this property. ;egenskap;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\EarthMaterial\AlterationDescription
EAID_3CE3E953_2630_46d3_99FF_C2BD75FA3489;alterationDistribution;AlterationDistribution describes the spatial distribution or geometry of alteration zones. eg: patchy, spotted, banded, viens, vein breccia, pervasive, disseminated, etc ;egenskap;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\EarthMaterial\AlterationDescription
EAID_6DB21756_EB7B_40f5_B24D_1D3692F3B467;materialRelationshipType;Describes the type of relationship between constituent parts in a compund material ;egenskap;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\EarthMaterial\MaterialRelation
EAID_6DB21756_EB7B_40f5_B24D_1D3692F3B467;sourceRole;Describes the role that the source material plays in a relationship between two constituent parts of a compound material (eg, quartz(source) overgrows plagioclase phenocrysts) ;egenskap;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\EarthMaterial\MaterialRelation
EAID_88D7E594_0B57_4cf2_AC19_D07B5FB76992;color;Terms to specify color of the earth material.  Color schemes such as the Munsell rock and soil color schemes could be used. ;egenskap;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\EarthMaterial\EarthMaterial
EAID_88D7E594_0B57_4cf2_AC19_D07B5FB76992;purpose;Specification of the intended purpose/level of abstraction for the given EarthMaterial. Scoped name because intention is asserted by author of the data instance.  Values: Instance, TypicalNorm, IdentifyingNorm.;egenskap;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\EarthMaterial\EarthMaterial
EAID_9C4A4EC3_7473_4940_9F77_D171AA984BE0;mineralName;Name of the mineral (eg: orthoclase) or mineral family (eg: feldspar), approved by the International Mineralogical Association. (eg: http://www.mindat.org/mineralindex.php) ;egenskap;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\EarthMaterial\Mineral
EAID_A242BAC8_A862_4fae_B42A_F720225E1212;chemicalAnalysis;This element delivers a swe:DataRecord of analyte concentrations (ie, swe:Quantity elements) which describe the chemical composition of an earth material or geologic unit;egenskap;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\EarthMaterial\ChemicalComposition
EAID_B23FACED_7E92_4614_80EA_3E6C8CD162DE;consolidationDegree;A property that specifies the degree to which an aggregation of EarthMaterial particles is a distinct solid material. Consolidation and induration are related concepts specified by this property. They define a continuum from unconsolidated material to very hard rock. Induration is the degree to which a consolidated material is made hard, operationally determined by how difficult it is to break a piece of the material. Consolidated materials may have varying degrees of induration (NADMSC, 2004) ;egenskap;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\EarthMaterial\RockMaterial
EAID_B23FACED_7E92_4614_80EA_3E6C8CD162DE;lithology;A controlled concept indicating the name of the RockMaterial type (eg, quartz sandstone, basalt, muscovite schist, sand, mud, soil, saprolite). Igneous rock definitions are governed by IUGS agreed vocabulary;egenskap;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\EarthMaterial\RockMaterial
EAID_D12BF66B_EE48_4f4f_B7E0_30F00F89C040;role;The role a ConstituentPart plays in a CompoundMaterial aggregation. The same EarthMaterial may occur as different ConstituentParts playing different roles within the same CompoundMaterial.  For example, feldspar may be present as groundmass (a ConstituentPart::role) and as phenocrysts (an ConstituentPart::role) within a single igneous rock. ;egenskap;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\EarthMaterial\ConstituentPart
EAID_D12BF66B_EE48_4f4f_B7E0_30F00F89C040;proportion;The fraction of the whole that is formed by a ConstituentPart in a part/whole relationship.  Used for the ConstituentPart portion in a CompoundMaterial.   Quantity that specifies the fraction of the Earth Material formed by the part (eg: 20%, minor, dominant) ;egenskap;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\EarthMaterial\ConstituentPart
EAID_ED53E456_2F3B_49e9_A327_E693EA5A6545;particleType;Terms to specify the nature of individual particles of each constituent in an Earth Material aggregation, based mostly on their genesis.  If applied on ParticleDescription for CompoundMaterial, then would characterize all particles in aggregate. Use this property on CompoundMaterial to distinguish rocks composed of crystals (crystalline rocks) from rocks composed of granular particles (clasts, fragments). Examples include oolith, crystals, pore space. Constituent type is determined based on the nature of the particles, and ideally is independent of the relationship between particles in a compound material aggregation. See discussion of particleType vs ConstituentPart.role in the scope notes for ConstituentPart. ;egenskap;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\EarthMaterial\ParticleGeometryDescription
EAID_ED53E456_2F3B_49e9_A327_E693EA5A6545;aspectRatio;"AspectRatio describes the geometry of particles based on the ratios of lengths of long, intermediate and short axes of grains. Equates to sphericity in sedimentary rocks (ie: the degree to which the shape of a particle approximates a sphere).  A quantitative specification based on the ratio of lengths of long, intermediate and short axes of grain shape (Sneed and Folk, 1958; Zingg, 1935). (eg: prolate, slightly flattened, very bladed, equant, acicular, tabular) ";egenskap;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\EarthMaterial\ParticleGeometryDescription
EAID_ED53E456_2F3B_49e9_A327_E693EA5A6545;shape;"The Shape attribute describes, a) the development of crystal faces bounding particles in crystalline compond materials, and b) surface rounding of grains in sedimentary rocks.  Roundness is a measure of the sharpness of the edges between surfaces bounding a particle (see Jackson, 1997; Wadell, 1932). Terms should be appropriate for the kind of compound material (eg: for crystalline rocks- euhedral, ideoblastic, subhedral, anhedral, xenoblastic; for sedimentary rocks - angular, rounded) ";egenskap;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\EarthMaterial\ParticleGeometryDescription
EAID_ED53E456_2F3B_49e9_A327_E693EA5A6545;size;"The Size attribute specifies particle grainsize.  Values may be reported using absolute measurements (eg: range, mean, median, mode, maximum) or as descriptive terms from a schema appropriate to the type of Compound Material (eg: the Udden-Wentworth sheme for clastic sedimentary rocks - silt, sand, gravel; volcaniclastic rocks - ash, lapilli, bomb; crystalline rocks - fine, medium, coarse, cryptocrystalline) ";egenskap;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\EarthMaterial\ParticleGeometryDescription
EAID_ED53E456_2F3B_49e9_A327_E693EA5A6545;sorting;The Sorting attribute holds text terms to specify size distribution of particles in a CompoundMaterial. Terminology for sorting in sedimentary rocks is based on the quantitative Graphic Standard Deviation (IGSD) scheme proposed by Folk (1968, 1974).  Example terms for this attribute may include sedimentary terms such as well sorted and poorly sorted, or igneous terms such as porphyritic, equigranuilar, seriate. ;egenskap;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\EarthMaterial\ParticleGeometryDescription
EAID_EEA1EA12_5ACD_4758_9C7E_EE7545949007;compositionCategory;Term to specify the gross compositional character of a compound material. Composition as used here is loosely construed to include both chemical composition and petrograpic composition, thus multiple values may be applied to a single rock, e.g. metaluminous and alkalic, undersaturated and basic, etc. Terms would typically include broad chemical classifications such as silicate, carbonate, ferromagnesian, oxide.  However, this attribute may have different terminology for different kinds of rocks - for example sandstone petrographic classification terms (e.g. feldspathic) might be placed here. ;egenskap;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\EarthMaterial\CompoundMaterial
EAID_EEA1EA12_5ACD_4758_9C7E_EE7545949007;geneticCategory;A term that represents a summary geologic history of the material. (ie, a genetic process classifier term) Examples include igneous, sedimentary, metamorphic, shock metamorphic, volcanic, pyroclastic. ;egenskap;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\EarthMaterial\CompoundMaterial
EAID_25EFF7C2_AE52_4bcb_A56F_3B125742437F;OrganicMaterial;An EarthMaterial that belongs to the class of chemical compounds having a reduced carbon basis (as distinct from carbonates), and derived from living organisms.  Includes high-carbon EarthMaterials such as bitumen, peat, and coal.  ;type;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\EarthMaterial
EAID_3CCDFFC6_7C25_431f_B219_32E554F8EEAF;InorganicFluid;An inorganic, non-crystalline EarthMaterial (solid, liquid, or gas) that tends to flow or conform to the shape of its container.  Includes glass.  By convention liquid mercury is considered a mineral (examples: water, brine, glass);type;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\EarthMaterial
EAID_88D7E594_0B57_4cf2_AC19_D07B5FB76992;EarthMaterial;The Earth Material class holds a description of a naturally occurring substance in the Earth.  Earth Material represents material composition or substance, and is thus independent of quantity or location. Ideally, Earth Materials are defined strictly based on physical properties, but because of standard geological usage, genetic interpretations may enter into the description as well. ;type;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\EarthMaterial
EAID_9C4A4EC3_7473_4940_9F77_D171AA984BE0;Mineral;A naturally occurring inorganic element or compound having a periodically repeating arrangement of atoms and a characteristic chemical composition or range of compositions, resulting in distinctive physical properties.  Includes mercury as a general exception to the requirement of crystallinity.  Also includes crypto-crystalline materials such as chalcedony and amorphous silica.;type;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\EarthMaterial
EAID_B23FACED_7E92_4614_80EA_3E6C8CD162DE;RockMaterial;A specialized CompoundMaterial that includes consolidated and unconsolidated materials as well as mixtures of consolidated and unconsolidated materials. ;type;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\EarthMaterial
EAID_D12BF66B_EE48_4f4f_B7E0_30F00F89C040;ConstituentPart;"The Constituent Part class describes how Earth Materials may be made up of other Earth Materials, including the proportion of the constituent part in the whole (eg: 20%, minor, dominant); the role that the constituent plays in the whole (eg: matrix, groundmass, framework, phenocryst, xenolith, vein). The particleType property that specifies type of particle (eg: grain, clast, crystal, fossil, oolite) has been moved to the ParticleGeometryDescription data type, associated with both ConstituentPart and CompoundMaterial (GeoSciMLv2, RC3, Uppsala, Sweden).  The distinction between ""role"" and ""particleType"" is subtle.  An operational test is that constituentType may be determined independent of relationship between particles in the aggregation, whereas role requires consideration of the relationship to other particles. A particle may be identified as clast, independent of its material composition, and independent of its relationship to other grains in a rock. The term 'floating clast' is a role, because it is dependent on the relationship 'not in contact with other clasts'. Consider Dunham's textural classification of carbonate rocks (wackestone, packstone, grainstone...) in the description of carbonate rocks. The description is predicated on identification of two kinds of intraclasts (grains) and matrix (carbonate mud), and then uses this distinction to establish relationships--mud supported vs. grain supported -- that define roles for the two types of constituents (framework, matrix...).  examples of type vs. role: Particle type: clast. Role: framework, floating particle  particle type: crystal. Role: matrix, pseudomatrix (in case that matrix is interpreted as recrystallized material)  particle type: clast. Role: matrix (in case that matrix is interpreted as very-fine grained detrital fraction)  particle type: crystal. Role: cement (in case that material insterstitial to particles is crystalline material introduced during diagenesis)  particle type: crystal. Role: phenocryst (in igneous rock)  particle type: microlite Role: groundmass (in porphyrytic igneous rock)  particle type: crystal. Role: framework (in igneous rock)  particle type: pyroclast. role: framework (in tuff)  particle type: crystal Role: oikocryst  particle type: crystal Role: overgrowth  particle type: biogenic particle Role: floating particle  particle type: ooid Role: framework  ";type;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\EarthMaterial
EAID_EEA1EA12_5ACD_4758_9C7E_EE7545949007;CompoundMaterial;"An EarthMaterial composed of particles composed of EarthMaterials, possibly including other CompoundMaterials.   This class is provided primarily as an extensibility point for related domain models that wish to import and build on GeoSciML, and wish to define material types that are compound but are not rock or rock-like material. For most users of GeoSciML ""RockMaterial"" should be used. ";type;;Gyldig;EarthMaterial;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\EarthMaterial