Id; Navn; Beskrivelse; Stereotype; Versjon; Status; Pakke; NavPakke;
EAID_7AF3D60A_680D_4403_9C07_CDB25D2A1135;Context Diagram : NonDirectionalStructure;;diagram;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-CoreGeoSciML-Core
EAID_A2FA2A54_E0FC_4cae_9535_6532D3F75216;Context Diagram : ShearDisplacementStructure;;diagram;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-CoreGeoSciML-Core
EAID_919F820C_BECA_49c7_B9A6_034CA314FBBA;Context Diagram : Fold;;diagram;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-CoreGeoSciML-Core
EAID_452A6055_D060_4f9c_B49D_6C4F14F94FA6;Context Diagram : Lineation;;diagram;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-CoreGeoSciML-Core
EAID_2D40F0AB_D123_43d2_8B45_473AE50FB598;Context Diagram : Contact;;diagram;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-CoreGeoSciML-Core
EAID_B7B6C6AB_4292_4b52_9852_4E649A8B6E67;Summary Diagram : Geologic Structure;;diagram;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-CoreGeoSciML-Core
EAID_F49245C9_52F4_431e_AF93_00725A74330F;Context Diagram : DisplacementValue;;diagram;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-CoreGeoSciML-Core
EAID_E0476942_2916_43b8_90A8_13AD8C87115A;Context Diagram : FoldSystem;;diagram;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-CoreGeoSciML-Core
EAID_22B4F11A_1ECD_440d_A90C_6C7C00AB28A4;Context Diagram : Foliation;;diagram;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-CoreGeoSciML-Core
EAID_34A71D33_6B92_4a41_AA55_169A46BD35C5;Context Diagram : GeologicStructure;;diagram;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-CoreGeoSciML-Core
EAID_157A1DB7_EFD5_4a26_A9B7_E69262CE65BE;Context Diagram : BoundaryRelationship;;diagram;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-CoreGeoSciML-Core
EAID_68BC8AF3_B438_4c0a_A017_ADF485802B1A;Context Diagram : FaultSystem;;diagram;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-CoreGeoSciML-Core
EAID_891A8643_F3FF_481f_ADF7_68EADD815332;Context Diagram : Fracture;;diagram;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-CoreGeoSciML-Core
EAID_064E54EE_A29A_422f_85E3_7DA0EFD7D289;Context Diagram : Joint;;diagram;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-CoreGeoSciML-Core
EAID_8AB80B6F_2FB8_4b4d_9CDB_2DAB89FA8FDB;Context Diagram : Layering;;diagram;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-CoreGeoSciML-Core
EAID_429718A4_6349_4b27_AB17_5D708E5F8C9A;Context Diagram : NetSlipValue;;diagram;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-CoreGeoSciML-Core
EAID_CA04FE19_8F59_4ee3_866E_CE3BBD8E4C0D;Context Diagram : SeparationValue;;diagram;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-CoreGeoSciML-Core
EAID_4129F2C5_6231_43a4_A101_2A46FC9E1166;Context Diagram : SlipComponents;;diagram;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-CoreGeoSciML-Core
EAID_01D5DE98_7149_4e89_B7B4_168291739310;Layering;"Planar foliation defined by a tabular succession of layers > 5 mm thick. This definition is based on the proposed definition of gneiss by the NADM Science Language Technical Team, so that the GeologicStructure characteristic of gneiss is layering. The committee discussed the possibility that layering should be considered a kind of foliation, but the majority opinion was that it is a different kind of structure.  Kept so that instance documents have a ""Layering"" tag";objekttype;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure
EAID_02A16B97_C96E_4ab9_8AFA_6D2B5FE7EBA6;Foliation;"A planar arrangement of textural or structural features in any type of rock.  Includes any of a wide variety of penetrative planar geological structures that may be present in a rock.  Examples include schistosity, mylonitic foliation, penetrative bedding structure (lamination), and cleavage.  Following the proposed definition of gneiss by the NADM Science Language Technical Team, penetrative planar foliation defined by layers > 5 mm thick is considered Layering.  Bedding as a fabric representing the average orientation of paleodepositional surface should be encoded through the foliationType; might apply to bedding that is layering or a foliation without layering (e.g. clast alignment in amalgamated beds). ";objekttype;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure
EAID_07C5CFF1_EF8A_4308_9ABE_3F789DEB1FE3;BoundaryRelationship;Defines the two GeologicUnits that make up the relationship described by the Contact ;objekttype;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure
EAID_14D219F5_FAF6_436d_8070_C50D1881931F;Contact;"Very general concept representing any kind of surface separating two geologic units including primary boundaries such as depositional contacts, all kinds of unconformities, intrusive contacts, and gradational contacts, as well as faults that separate geologic units.  Permeability of contacts still needs to be modeled; considered out of scope for GeoSciML2.  Bedding measured as discrete surfaces in the case that those are the feature of interest (e.g. individual cross set surfaces for paleocurrent analysis) should be represented here.";objekttype;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure
EAID_65A73309_EB02_469d_8DA2_ACE79626A62A;NonDirectionalStructure;Structures present in geology that do not have a preferred orientation Includes small-scale structures that are characteristic of the geologic unit, e.g. herringbone crossbedding, mudcracks, graded bedding, planar lamination, miarolitic cavities, nebulitic structure, trace fossils, fossil molds;objekttype;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure
EAID_75E0E4D9_79B2_4711_A42D_8D9B5F9C7C63;Fold;One or more systematically curved layers, surfaces, or lines in a rock body. Fold denotes a structure formed by the deformation of a GeologicStructure to form a structure that may be described by the translation of an abstract line (the fold axis) parallel to itself along some curvilinear path (the fold profile). Folds have a hinge zone (zone of maximum curvature along the surface) and limbs (parts of the deformed surface not in the hinge zone).  Folds are described by an axial surface, hinge line , profile geometry, the solid angle between the limbs, and the relationships between adjacent folded surfaces if the folded structure is a Layering fabric (similar, parallel).   ;objekttype;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure
EAID_808BCC3C_73E7_4a94_98AF_AC5DAF5CD074;ShearDisplacementStructure;A shear displacement structure includes all brittle to ductile style structures along which displacement has occurred, from a simple, single 'planar' brittle or ductile surface to a fault system comprised of 10's of strands of both brittle and ductile nature. This structure may have some significant thickness (a deformation zone) and have an associated body of deformed rock that may be considered a DeformationUnit ;objekttype;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure
EAID_94E28F8D_9573_4f6b_BB8F_20E580A78F32;GeologicStructure;"A configuration of matter in the Earth based on describable inhomogeneity, pattern, or fracture in an EarthMaterial.  The identity of a GeologicStructure is independent of the material that is the substrate for the structure.  Properties like ""clast-supported"",  ""matrix-supported"", and ""graded bed"" that do not involve orientation are considered kinds of GeologicStructure  because they depend on the configuration of parts of a rock body. Includes sedimentary structures. The general GeologicRelation is used to associate penetrative GeologicStructures with GeologicUnits.";objekttype;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure
EAID_98C1CC85_FFE3_49de_80A0_A921FB354D74;FaultSystem;A composite structure that is an aggregation of genetically related instances of Faults and/or DuctileShearStructures. A FaultSystem is composed of individually identified and mapped Faults and/or DuctileShearStructures that are considered distinct ShearDisplacementStructures, that generally form overlapping, anastomosing patterns in which, at any point along the fault system, multiple fault strands are identified and each considered important at the scale of description. Displacement and other descriptive data may be assigned at the 'fault segment', 'fault', or 'fault system level'. ;objekttype;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure
EAID_CE96AB19_C851_4ebb_8D2E_BFF3D0C0D43C;FoldSystem;"A collection of congruent folds  (axis and axial surface are parallel) produced by the same tectonic event. Sometimes referred to as a ""Fold Train"".";objekttype;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure
EAID_D1FCC703_3E95_4208_8F40_55894578D446;Fracture;Fractures are cracks in the earth surface. If there is no displacement it is a joint. If there is displacement and you are in the brittle zone it is a fault. In the ductile zone, a fracture with displacement with fracture is called a shear.  FaultSurface as a separate class is not considered necessary for GeoSciML 2. Recording observations on FaultSurface should be in observation and measurement. The observation needs to be able to distinguish the type of measurement made (PropertyType) ;objekttype;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure
EAID_D4A5A711_9AE1_4521_B291_880E575A36BB;Lineation;GeologicStructure defined by aligned elongate elements. Lineation connotes a pervasive linear structure. Includes: flow lines, scratches, striae, slickenlines, linear arrangements of elongate components in sediments, fold hinges (when abundant and closely spaced), elongate minerals, crinkles, and lines of intersection between penetrative planar structures.  Class also includes discrete linear structures like boudin, channel axis, tool marks. ;objekttype;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure
EAID_F4593A8A_16F3_4c90_BEED_44BEEA834367;Joint;Fracture across which there is no displacement at the scale of interest.  ;objekttype;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure
EAID_3D89EEAC_2032_4831_A3A2_E2513CDB184D;SlipComponents;representation of slip as vector resolved into components resolved into reference frame in which horizontal axes are parallel and perpendicular to the strike of the fault. ;datatype;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure
EAID_57F62C93_1331_4ec9_A9D5_13B12801FE16;DisplacementValue;Trying to express the displacement on a fault with respect to a planar approximation of its shape ;datatype;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure
EAID_60FEA7EE_3491_4283_8FEF_74211DBD6855;SeparationValue;The amount of separation displacement;datatype;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure
EAID_BB2F0A66_9B63_439d_94D4_8D0B161CA69F;NetSlipValue;The total amount of slip displacement;datatype;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure
EAID_011A9F20_72DE_4719_B244_0607AA01EA57;ContactTypeTerm;Refers to a vocabulary of terms describing types of geological contacts ;kodeliste;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure
EAID_027E0FE0_96FC_4930_901A_A1C055456B2C;NonDirectionalStructureTypeTerm;Refers to a vocabulary of terms describing types of non-directional structures (eg, miarolitic cavity, flame structure, load cast, shatter cone, trace fossil, fossil mold, etc);kodeliste;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure
EAID_12195470_4925_45d4_A536_60CA5E9BE96B;FoliationTypeTerm;Refers to a vocabular of terms defining the type of foliation (eg, crenulation cleavage, gneissic layering, slaty cleavage, schistosity, etc) ;kodeliste;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure
EAID_2F279F9A_44FA_49ca_A8C0_EF0F2562F50C;DeformationStyleTerm;A vocabulary of terms to describe the style of deformation, ie brittle (fault, breccia), ductile (shear), brittle-ductile, unknown.;kodeliste;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure
EAID_43451644_E9F7_4751_A5B9_2944B92A73AA;FaultTypeTerm;"A vocabulary of terms describing the type of shear displacement structure (eg; thrust fault, normal fault, wrench fault)";kodeliste;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure
EAID_B3A317F8_523C_48d1_B6DF_5CE801B7B5F2;FoldProfileTypeTerm;Refers to a vocabulary of terms specifying concave/convex geometry of fold relative to earth surface, and relationship to younging direction in folded strata if known. antiform, synform, neutral, anticline, syncline, monocline, ptygmatic ;kodeliste;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure
EAID_C620AC1F_F98C_4f47_B926_A1FDADD04870;MovementSenseTerm;Refers to a vocabulary of terms describing the sense of movement on a shear displacement structure ;kodeliste;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure
EAID_F6889114_2CAE_4745_ADFF_1C8F6EB240AE;LineationTypeTerm;Refers to a vocabulary of terms describing the type of lineation.  Examples include: flow lines, scratches, striae, slickenlines, linear arrangements of elongate components in sediments, elongate minerals, crinkles, and lines of intersection between penetrative planar structures. ;kodeliste;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure
EAID_FACBB382_EF7B_476d_8346_69ADBA483817;MovementTypeTerm;Refers to a vocabulary of terms describing the type of movement  (eg, dip-slip, strike-slip) ;kodeliste;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure
EAID_02A16B97_C96E_4ab9_8AFA_6D2B5FE7EBA6;foliationType;Specifies the type of foliation.  Examples include crenulation cleavage, slaty cleavage, schistosity ;egenskap;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure\Foliation
EAID_02A16B97_C96E_4ab9_8AFA_6D2B5FE7EBA6;definingElement;Kinds of describable inhomogeneity in a rock body that may define a GeologicStructure.   Examples include Discontinuity, Shaped Surface, Oriented Particle, Material Boundary, and Layer.   ;egenskap;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure\Foliation
EAID_02A16B97_C96E_4ab9_8AFA_6D2B5FE7EBA6;continuity;terms to distinguish continuous vs. disjunct cleavages ;egenskap;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure\Foliation
EAID_02A16B97_C96E_4ab9_8AFA_6D2B5FE7EBA6;intensity;How well the foliation is developed. Terms such as weak, moderate, strong. ;egenskap;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure\Foliation
EAID_02A16B97_C96E_4ab9_8AFA_6D2B5FE7EBA6;mineralElement;The mineral that defines the foliation;egenskap;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure\Foliation
EAID_02A16B97_C96E_4ab9_8AFA_6D2B5FE7EBA6;orientation;The planar orientation of the foliation;egenskap;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure\Foliation
EAID_02A16B97_C96E_4ab9_8AFA_6D2B5FE7EBA6;spacing;linear dimension representing the thickness of foliation domains. Also use for thickness of layers of a given composition ;egenskap;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure\Foliation
EAID_14D219F5_FAF6_436d_8070_C50D1881931F;contactType;Classifies the contact (eg intrusive, unconformity, bedding surface, lithologic boundary, phase boundary) ;egenskap;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure\Contact
EAID_14D219F5_FAF6_436d_8070_C50D1881931F;contactCharacter;The character of the boundary, as opposed to its type. e.g.  abrupt, gradational  ;egenskap;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure\Contact
EAID_14D219F5_FAF6_436d_8070_C50D1881931F;orientation;orientation of the contact surface;egenskap;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure\Contact
EAID_3D89EEAC_2032_4831_A3A2_E2513CDB184D;heave;component of slip in the horizontal, and perpendicular to the strike of the fault;egenskap;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure\SlipComponents
EAID_3D89EEAC_2032_4831_A3A2_E2513CDB184D;horizontalSlip;slip component that is horizontal and parallel to strike of the fault;egenskap;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure\SlipComponents
EAID_3D89EEAC_2032_4831_A3A2_E2513CDB184D;throw;vertical component of slip;egenskap;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure\SlipComponents
EAID_57F62C93_1331_4ec9_A9D5_13B12801FE16;hangingWallDirection;Normally the compass quadrant indicating the hangingwall side of the fault-system for faults that are steep enough to define a hanging-wall on the map trace;egenskap;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure\DisplacementValue
EAID_57F62C93_1331_4ec9_A9D5_13B12801FE16;movementSense;eg, dextral, sinistral ;egenskap;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure\DisplacementValue
EAID_57F62C93_1331_4ec9_A9D5_13B12801FE16;movementType;Defines the type of movement  (eg dip-slip, strike-slip) ;egenskap;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure\DisplacementValue
EAID_60FEA7EE_3491_4283_8FEF_74211DBD6855;separation;Reported apparent offset of planar feature, report as vector.  ;egenskap;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure\SeparationValue
EAID_65A73309_EB02_469d_8DA2_ACE79626A62A;structureType;The type of non oriented structure.  Examples include miarolitic cavity, flame structure, load cast, shatter cone, trace fossil, fossil mold;egenskap;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure\NonDirectionalStructure
EAID_75E0E4D9_79B2_4711_A42D_8D9B5F9C7C63;amplitude;length from line segment connecting inflection points on adjacent fold limbs to the intervening fold hinge  ;egenskap;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure\Fold
EAID_75E0E4D9_79B2_4711_A42D_8D9B5F9C7C63;axialSurfaceOrientation;This is used to characterize the geometry of a fold. The axial surface of a particular fold may be located based on observations of the folded geologic structure, but in general it has no direct physical manifestions. As a geologic surface, it has geometric properties, including orientation, which may be specified by observations at one or more locations, or generalized using terminology (upright, inclined, reclined, recumbent, overturned). Dip and Dip Direction are one approach to specifying the value.;egenskap;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure\Fold
EAID_75E0E4D9_79B2_4711_A42D_8D9B5F9C7C63;geneticModel;Specification of genetic model for fold, e.g. flexural slip, parallel ;egenskap;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure\Fold
EAID_75E0E4D9_79B2_4711_A42D_8D9B5F9C7C63;hingeLineCurvature;variation in orientation of fold hinge along trend of fold, distinguish sheath from cylindrical folds. Specify with terminology eg sheath, dome, basin, cylindrical. ;egenskap;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure\Fold
EAID_75E0E4D9_79B2_4711_A42D_8D9B5F9C7C63;hingeLineOrientation;Specification of hinge line orientation for fold.  CGI_LinearOrientation allows for a term value specification or a numeric specification of either or both the trend and plunge of hinge line. kHinge plunge term examples: sub-vertical, steeply plunging, ... sub-horizontal, reclined and vertical for special cases in which hinge plunge is close to axial surface dip. 0..* cardinality allows for both a numeric specification a term specification.;egenskap;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure\Fold
EAID_75E0E4D9_79B2_4711_A42D_8D9B5F9C7C63;hingeShape;"rounded vs. angular hinge zones; has to do with proprotion of wavelength that is considered part of hinge ";egenskap;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure\Fold
EAID_75E0E4D9_79B2_4711_A42D_8D9B5F9C7C63;interLimbAngle;Specify using a tightness term (gentle (120-180), open (70-120), close (30-70), tight (10-30), isoclinal (0-10));egenskap;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure\Fold
EAID_75E0E4D9_79B2_4711_A42D_8D9B5F9C7C63;limbShape;straight vs curved limbs, eg kink, chevron, sinusoidal, box ;egenskap;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure\Fold
EAID_75E0E4D9_79B2_4711_A42D_8D9B5F9C7C63;profileType;"Terminology specifying concave/convex geometry of fold relative to earth surface, and relationship to younging direction in folded strata if known. (eg; antiform, synform, neutral, anticline, syncline, monocline, ptygmatic)";egenskap;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure\Fold
EAID_75E0E4D9_79B2_4711_A42D_8D9B5F9C7C63;span;linear distance between inflection points in a single fold  ;egenskap;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure\Fold
EAID_75E0E4D9_79B2_4711_A42D_8D9B5F9C7C63;symmetry;concordance or discordance of bisecting surface and axial surface, or ratio of length of limbs. Folded surface may have asymmetry defined by limb length ratio if inflection points are defined. Defintion based on bisecting surface/axial surface angle depends on having multiple surfaces defined such that the axial surface may be identified. (symmetric, assymetric) ;egenskap;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure\Fold
EAID_808BCC3C_73E7_4a94_98AF_AC5DAF5CD074;faultType;"Refers to a vocabulary of terms describing the type of shear displacement structure (eg; thrust fault, normal fault, wrench fault).";egenskap;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure\ShearDisplacementStructure
EAID_808BCC3C_73E7_4a94_98AF_AC5DAF5CD074;deformationStyle;A mandatory element referring to a vocabulary of terms to describe the style of deformation, ie brittle (fault, breccia), ductile (shear), brittle-ductile, unknown.;egenskap;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure\ShearDisplacementStructure
EAID_808BCC3C_73E7_4a94_98AF_AC5DAF5CD074;planeOrientation;Allows capturing the orientation of the plane of the structure;egenskap;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure\ShearDisplacementStructure
EAID_BB2F0A66_9B63_439d_94D4_8D0B161CA69F;netSlip;The value of the net slip;egenskap;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure\NetSlipValue
EAID_CE96AB19_C851_4ebb_8D2E_BFF3D0C0D43C;periodic;True if fold hinges in train are regularly spaced.;egenskap;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure\FoldSystem
EAID_CE96AB19_C851_4ebb_8D2E_BFF3D0C0D43C;wavelength;Quantitative specification of length between adjacent antiforms (or synforms) in a fold train. ;egenskap;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure\FoldSystem
EAID_D4A5A711_9AE1_4521_B291_880E575A36BB;lineationType;Type of lineation. Examples include: flow lines, scratches, striae, slickenlines, linear arrangements of elongate components in sediments, elongate minerals, crinkles, and lines of intersection between penetrative planar structures. ;egenskap;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure\Lineation
EAID_D4A5A711_9AE1_4521_B291_880E575A36BB;definingElement;Kinds of describable inhomogeneity in a rock body that may define a GeologicStructure.   Examples include Oriented Particle.   ;egenskap;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure\Lineation
EAID_D4A5A711_9AE1_4521_B291_880E575A36BB;intensity;How well the lineation is developed. Terms such as weak, moderate, strong. ;egenskap;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure\Lineation
EAID_D4A5A711_9AE1_4521_B291_880E575A36BB;mineralElement;Mineral that defines the lineation;egenskap;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure\Lineation
EAID_D4A5A711_9AE1_4521_B291_880E575A36BB;orientation;Orientation of the lineation;egenskap;;Gyldig;GeologicStructure;Inspire Consolidated UML Model\Foundation Schemas\GeoSciML\GeoSciML-Core\GeologicStructure\Lineation