| identifier: | http://resource.geosciml.org/classifierscheme/cgi/201012/lineationtype |
| title: | CGI lineation type categories |
| publisher: | Concept Definition Task Group of IUGS CGI Interoperability Working Group (http://www.cgi-iugs.org/tech_collaboration/interoperability_working_group.html) |
| creator: | Concept Definition Task Group of IUGS CGI Interoperability Working Group (http://www.cgi-iugs.org/tech_collaboration/interoperability_working_group.html) |
| format: | application/rdf+xml |
| language: | en |
| URI | http://resource.geosciml.org/classifier/cgi/lineationtype/0001 |
| Preferred label (en) | Augen lineation |
| Definition (en) | A shape lineation defined by elongate augen. |
| Source () | this vocabulary |
| Relationships: | |
| Broader | http://resource.geosciml.org/classifier/cgi/lineationtype/0015 |
| Broader | http://resource.geosciml.org/classifier/cgi/lineationtype/0022 |
| Notes: |
| URI | http://resource.geosciml.org/classifier/cgi/lineationtype/0002 |
| Preferred label (en) | Bedding cleavage intersection lineation |
| Definition (en) | Lineation defined by the intersection of bedding surfaces and cleavage surfaces. |
| Source () | this vocabulary |
| Relationships: | |
| Broader | http://resource.geosciml.org/classifier/cgi/lineationtype/0012 |
| Broader | http://resource.geosciml.org/classifier/cgi/lineationtype/0022 |
| Notes: |
| URI | http://resource.geosciml.org/classifier/cgi/lineationtype/0003 |
| Preferred label (en) | Biotite mineral lineation |
| Definition (en) | Mineral lineation defined by aligned elongate biotite aggregates in a foliation surface. Biotite does not have an elongate (prismatic, acicular) mineral habit, so production of lineation must reflect elongate aggregates of biotite crystals. |
| Source () | this vocabulary |
| Relationships: | |
| Broader | http://resource.geosciml.org/classifier/cgi/lineationtype/0014 |
| Notes: |
| URI | http://resource.geosciml.org/classifier/cgi/lineationtype/0004 |
| Preferred label (en) | Cleavage intersection lineation |
| Definition (en) | Lineation defined by the intersection of two cleavages. |
| Source () | this vocabulary |
| Relationships: | |
| Broader | http://resource.geosciml.org/classifier/cgi/lineationtype/0012 |
| Broader | http://resource.geosciml.org/classifier/cgi/lineationtype/0022 |
| Notes: |
| URI | http://resource.geosciml.org/classifier/cgi/lineationtype/0005 |
| Preferred label (en) | Crenulation lineation |
| Definition (en) | Lineation defined by small-scale wrinkles, typically of phylosillicate minerals, on another surface, typically a cleavage or schistosity. Use instead of intersection lineation if the wrinkles are the measured feature and the intersecting planar feature is not apparent. |
| Source () | this vocabulary |
| Relationships: | |
| Broader | http://resource.geosciml.org/classifier/cgi/lineationtype/0013 |
| Broader | http://resource.geosciml.org/classifier/cgi/lineationtype/0022 |
| Notes: |
| URI | http://resource.geosciml.org/classifier/cgi/lineationtype/0006 |
| Preferred label (en) | Flow lineation |
| Definition (en) | A linear alignment of fabric elements, especially elongate or rod-shaped minerals, interpreted to have been aligned by flow of magma, lava, pyroclastic material, or diapiric flow of sedimentary rock. |
| Source () | Geoscience Victoria, Australia |
| Relationships: | |
| Broader | http://resource.geosciml.org/classifier/cgi/lineationtype/0013 |
| Notes: |
| URI | http://resource.geosciml.org/classifier/cgi/lineationtype/0007 |
| Preferred label (en) | Hornblende mineral lineation |
| Definition (en) | Mineral lineation defined by aligned hornblende crystals. |
| Source () | this vocabulary |
| Relationships: | |
| Broader | http://resource.geosciml.org/classifier/cgi/lineationtype/0014 |
| Notes: |
| URI | http://resource.geosciml.org/classifier/cgi/lineationtype/0008 |
| Preferred label (en) | Igneous lineation |
| Definition (en) | Lineation defined by alignment of elongate fabric elements formed in lava or magma before complete crystallization. Some typical fabric elements are elongate phenocrysts and vesicles. |
| Source () | this vocabulary |
| Relationships: | |
| Broader | http://resource.geosciml.org/classifier/cgi/lineationtype/0013 |
| Narrower | http://resource.geosciml.org/classifier/cgi/lineationtype/0009 |
| Narrower | http://resource.geosciml.org/classifier/cgi/lineationtype/0010 |
| Narrower | http://resource.geosciml.org/classifier/cgi/lineationtype/0011 |
| Notes: |
| URI | http://resource.geosciml.org/classifier/cgi/lineationtype/0009 |
| Preferred label (en) | Igneous mineral lineation |
| Definition (en) | Lineation in igneous rock defined by aligned crystals where there is evidence that the crystal alignment is related to process occurring before the rock was solidified. |
| Source () | this vocabulary |
| Relationships: | |
| Broader | http://resource.geosciml.org/classifier/cgi/lineationtype/0008 |
| Broader | http://resource.geosciml.org/classifier/cgi/lineationtype/0014 |
| Notes: |
| URI | http://resource.geosciml.org/classifier/cgi/lineationtype/0010 |
| Preferred label (en) | Igneous particle shape lineation |
| Definition (en) | Lineation in an igneous rock, usually welded tuff, defined by elongate objects in the rock (usually pumice pads, also elongate crystals). Descriptive--elogation may be due to deformation or to rotation/alignment of originally elongate (prolate ellipsoid) objects in the rock. |
| Source () | this vocabulary |
| Relationships: | |
| Broader | http://resource.geosciml.org/classifier/cgi/lineationtype/0008 |
| Broader | http://resource.geosciml.org/classifier/cgi/lineationtype/0015 |
| Notes: |
| URI | http://resource.geosciml.org/classifier/cgi/lineationtype/0011 |
| Preferred label (en) | Igneous vesicle lineation |
| Definition (en) | lineation defined in a volcanic rock by aligned elongation direction of vesicles. |
| Source () | this vocabulary |
| Relationships: | |
| Broader | http://resource.geosciml.org/classifier/cgi/lineationtype/0008 |
| Notes: |
| URI | http://resource.geosciml.org/classifier/cgi/lineationtype/0012 |
| Preferred label (en) | Intersection lineation |
| Definition (en) | A lineation produced by the intersection of two planar fabrics. |
| Source () | Neuendorf et al 2005; this vocabulary |
| Relationships: | |
| Broader | http://resource.geosciml.org/classifier/cgi/lineationtype/0013 |
| Narrower | http://resource.geosciml.org/classifier/cgi/lineationtype/0002 |
| Narrower | http://resource.geosciml.org/classifier/cgi/lineationtype/0004 |
| Notes: |
| URI | http://resource.geosciml.org/classifier/cgi/lineationtype/0013 |
| Preferred label (en) | Lineation |
| Definition (en) | Nongenetic term for a penetrative linear structure. |
| Source () | Neuendorf et al 2005; this vocabulary |
| Relationships: | |
| Narrower | http://resource.geosciml.org/classifier/cgi/lineationtype/0005 |
| Narrower | http://resource.geosciml.org/classifier/cgi/lineationtype/0006 |
| Narrower | http://resource.geosciml.org/classifier/cgi/lineationtype/0008 |
| Narrower | http://resource.geosciml.org/classifier/cgi/lineationtype/0012 |
| Narrower | http://resource.geosciml.org/classifier/cgi/lineationtype/0015 |
| Narrower | http://resource.geosciml.org/classifier/cgi/lineationtype/0016 |
| Narrower | http://resource.geosciml.org/classifier/cgi/lineationtype/0018 |
| Narrower | http://resource.geosciml.org/classifier/cgi/lineationtype/0020 |
| Narrower | http://resource.geosciml.org/classifier/cgi/lineationtype/0022 |
| Notes: |
| URI | http://resource.geosciml.org/classifier/cgi/lineationtype/0014 |
| Preferred label (en) | Mineral lineation |
| Definition (en) | Lineation defined by alignment of elongate crystals that have a prismatic crystal habit or of monomineralic grain aggregates. |
| Source () | Neuendorf et al 2005; this vocabulary |
| Relationships: | |
| Broader | http://resource.geosciml.org/classifier/cgi/lineationtype/0015 |
| Narrower | http://resource.geosciml.org/classifier/cgi/lineationtype/0003 |
| Narrower | http://resource.geosciml.org/classifier/cgi/lineationtype/0007 |
| Narrower | http://resource.geosciml.org/classifier/cgi/lineationtype/0009 |
| Narrower | http://resource.geosciml.org/classifier/cgi/lineationtype/0019 |
| Notes: |
| URI | http://resource.geosciml.org/classifier/cgi/lineationtype/0015 |
| Preferred label (en) | Particle shape lineation |
| Definition (en) | Lineation defined by alignment of long axes of prolate-shaped particles such as clasts, fossils, crystals, or phenocrysts. Particles may be polycrystalline aggregates formed by deformation of pre-existing particles. General category does not specify genesis of particles or their alignment. |
| Source () | this vocabulary |
| Relationships: | |
| Broader | http://resource.geosciml.org/classifier/cgi/lineationtype/0013 |
| Narrower | http://resource.geosciml.org/classifier/cgi/lineationtype/0001 |
| Narrower | http://resource.geosciml.org/classifier/cgi/lineationtype/0010 |
| Narrower | http://resource.geosciml.org/classifier/cgi/lineationtype/0014 |
| Narrower | http://resource.geosciml.org/classifier/cgi/lineationtype/0017 |
| Narrower | http://resource.geosciml.org/classifier/cgi/lineationtype/0021 |
| Notes: |
| URI | http://resource.geosciml.org/classifier/cgi/lineationtype/0016 |
| Preferred label (en) | Pencil lineation |
| Definition (en) | Lineation defined by tendency of rock to break into long, slender pieces resembling pencils. Typically produced by intesection of bedding and cleavage or intersection of two cleavages. Fabric is generally only observed in weakly metamorphosed rocks. |
| Source () | based on Neuendorf et al 2005 |
| Relationships: | |
| Broader | http://resource.geosciml.org/classifier/cgi/lineationtype/0013 |
| Notes: |
| URI | http://resource.geosciml.org/classifier/cgi/lineationtype/0017 |
| Preferred label (en) | Quartz fibre lineation |
| Definition (en) | Aligned quartz fibres that define a measurable lineation |
| Source () | this vocabulary |
| Relationships: | |
| Broader | http://resource.geosciml.org/classifier/cgi/lineationtype/0015 |
| Notes: |
| URI | http://resource.geosciml.org/classifier/cgi/lineationtype/0018 |
| Preferred label (en) | Rodding lineation |
| Definition (en) | Linear structure in metamorphic rocks in which the stronger parts have been shaped into parallel rods (eg. vein quartz) |
| Source () | Jackson 1997 |
| Relationships: | |
| Broader | http://resource.geosciml.org/classifier/cgi/lineationtype/0013 |
| Broader | http://resource.geosciml.org/classifier/cgi/lineationtype/0022 |
| Notes: |
| URI | http://resource.geosciml.org/classifier/cgi/lineationtype/0019 |
| Preferred label (en) | Sillimanite mineral lineation |
| Definition (en) | Mineral lineation defined by aligned sillimanite crystals. |
| Source () | this vocabulary |
| Relationships: | |
| Broader | http://resource.geosciml.org/classifier/cgi/lineationtype/0014 |
| Notes: |
| URI | http://resource.geosciml.org/classifier/cgi/lineationtype/0020 |
| Preferred label (en) | Slickenline |
| Definition (en) | Lineation on a brittle slip surface defined by grooves, ridges, or striations |
| Source () | based on Neuendorf et al 2005 |
| Relationships: | |
| Broader | http://resource.geosciml.org/classifier/cgi/lineationtype/0013 |
| Broader | http://resource.geosciml.org/classifier/cgi/lineationtype/0022 |
| Notes: |
| URI | http://resource.geosciml.org/classifier/cgi/lineationtype/0021 |
| Preferred label (en) | Stretching lineation |
| Definition (en) | Lineation defined by elongate (prolate) fabric elements in which the alignment of the fabric elements, and the formation of prolate fabric elements is interpreted to be the product of crystal plastic deformation processes. Associated with mylontic foliation. |
| Source () | this vocabulary |
| Relationships: | |
| Broader | http://resource.geosciml.org/classifier/cgi/lineationtype/0015 |
| Broader | http://resource.geosciml.org/classifier/cgi/lineationtype/0022 |
| Notes: |
| URI | http://resource.geosciml.org/classifier/cgi/lineationtype/0022 |
| Preferred label (en) | Tectonic lineation |
| Definition (en) | Penetrative linear structure in a rock body defined by fabric elements that are the product of tectonic processes. Linear is used in the sense that the orientation of the structure can be represented as a line in some sufficiently small neighborhood of any point in the material containig the fabric. Penetrative denotes that the fabric elements defining the structure are repeated at distances so small, compared with the scale of the whole…that they can be considered to pervade it uniformly and be present at every point (paraphrase of Turner and Weiss, 1963, p. 21). |
| Source () | this vocabulary |
| Relationships: | |
| Broader | http://resource.geosciml.org/classifier/cgi/lineationtype/0013 |
| Narrower | http://resource.geosciml.org/classifier/cgi/lineationtype/0001 |
| Narrower | http://resource.geosciml.org/classifier/cgi/lineationtype/0002 |
| Narrower | http://resource.geosciml.org/classifier/cgi/lineationtype/0004 |
| Narrower | http://resource.geosciml.org/classifier/cgi/lineationtype/0005 |
| Narrower | http://resource.geosciml.org/classifier/cgi/lineationtype/0018 |
| Narrower | http://resource.geosciml.org/classifier/cgi/lineationtype/0020 |
| Narrower | http://resource.geosciml.org/classifier/cgi/lineationtype/0021 |
| Notes: |
| URI | |
| Preferred label (en) | CGI Lineation type categories |
| Definition (en) | This file contains the CGI Lineation Type vocabulary. Vocabulary for populating Lineation Type properties in GeoSciML GeologicStructure/Lineation elements. |
| Relationships: | |
| Notes: | |
| History note (en) | 2010-02-11 Add narrower relationship links by adding skos:narrower link in Protege, defining skos:narrower as inverse of skos:broader, calculating with Pellet reasoner to add inferred axioms, and using 'file/Export inferred axioms as ontology' in Protege. |
| History note (en) | 2010-11-28 SMR Replace URN with http URI according to CGI URI scheme (see https://www.seegrid.csiro.au/wiki/bin/view/CGIModel/PersistentIdentifiersInGeoSciMLServices) |