http://inspire.ec.europa.eu/codelist/LithologyValue/faultRelatedMaterial
2015-08-18 17:30 PM CEST
fault-related material
fault-related material
Material formed as a result of brittle faulting, composed of greater than 10 percent matrix; matrix is fine-grained material caused by tectonic grainsize reduction.
Material formed as a result of brittle faulting, composed of greater than 10 percent matrix; matrix is fine-grained material caused by tectonic grainsize reduction.
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http://inspire.ec.europa.eu/codelist/LithologyValue/brecciaGougeSeries
2015-08-18 18:02 PM CEST
breccia-gouge series
breccia-gouge series
Fault material with features such as void spaces (filled or unfilled), or unconsolidated matrix material between fragments, indicating loss of cohesion during deformation. Includes fault-related breccia and gouge.
Fault material with features such as void spaces (filled or unfilled), or unconsolidated matrix material between fragments, indicating loss of cohesion during deformation. Includes fault-related breccia and gouge.
http://inspire.ec.europa.eu/codelist/LithologyValue/myloniticRock
2015-08-18 18:04 PM CEST
mylonitic rock
mylonitic rock
Metamorphic rock characterised by a foliation resulting from tectonic grain size reduction, in which more than 10 percent of the rock volume has undergone grain size reduction. Includes protomylonite, mylonite, ultramylonite, and blastomylonite.
Metamorphic rock characterised by a foliation resulting from tectonic grain size reduction, in which more than 10 percent of the rock volume has undergone grain size reduction. Includes protomylonite, mylonite, ultramylonite, and blastomylonite.
http://inspire.ec.europa.eu/codelist/LithologyValue/phyllonite
2015-08-18 18:04 PM CEST
phyllonite
phyllonite
Mylonitic rock composed largely of fine-grained mica that imparts a sheen to foliation surfaces; may have flaser lamination, isoclinal folding, and deformed veins, which indicate significant shearing. Macroscopically resembles phyllite, but formed by mechanical degradation of initially coarser rock.
Mylonitic rock composed largely of fine-grained mica that imparts a sheen to foliation surfaces; may have flaser lamination, isoclinal folding, and deformed veins, which indicate significant shearing. Macroscopically resembles phyllite, but formed by mechanical degradation of initially coarser rock.