http://inspire.ec.europa.eu/codelist/LithologyValue/clasticSedimentaryMaterial
2015-08-18 17:31 PM CEST
clastic sedimentary material
clastic sedimentary material
Sedimentary material of unspecified consolidation state in which at least 50 percent of the constituent particles were derived from erosion, weathering, or mass-wasting of pre-existing earth materials, and transported to the place of deposition by mechanical agents such as water, wind, ice and gravity.
Sedimentary material of unspecified consolidation state in which at least 50 percent of the constituent particles were derived from erosion, weathering, or mass-wasting of pre-existing earth materials, and transported to the place of deposition by mechanical agents such as water, wind, ice and gravity.
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http://inspire.ec.europa.eu/codelist/LithologyValue/clasticSediment
2015-08-18 18:02 PM CEST
clastic sediment
clastic sediment
Sediment in which at least 50 percent of the constituent particles were derived from erosion, weathering, or mass-wasting of pre-existing earth materials, and transported to the place of deposition by mechanical agents such as water, wind, ice and gravity.
Sediment in which at least 50 percent of the constituent particles were derived from erosion, weathering, or mass-wasting of pre-existing earth materials, and transported to the place of deposition by mechanical agents such as water, wind, ice and gravity.
http://inspire.ec.europa.eu/codelist/LithologyValue/diamicton
2015-08-18 18:02 PM CEST
diamicton
diamicton
Unsorted or poorly sorted, clastic sediment with a wide range of particle sizes, including a muddy matrix. Biogenic materials that have such texture are excluded. Distinguished from conglomerate, sandstone, mudstone based on polymodality and lack of structures related to transport and deposition of sediment by moving air or water. Assignment to an other size class can be used in conjunction to indicate the dominant grain size.
Unsorted or poorly sorted, clastic sediment with a wide range of particle sizes, including a muddy matrix. Biogenic materials that have such texture are excluded. Distinguished from conglomerate, sandstone, mudstone based on polymodality and lack of structures related to transport and deposition of sediment by moving air or water. Assignment to an other size class can be used in conjunction to indicate the dominant grain size.
http://inspire.ec.europa.eu/codelist/LithologyValue/gravel
2015-08-18 18:03 PM CEST
gravel
gravel
Clastic sediment containing greater than 30 percent gravel-size particles (greater than 2.0 mm diameter). Gravel in which more than half of the particles are of epiclastic origin
Clastic sediment containing greater than 30 percent gravel-size particles (greater than 2.0 mm diameter). Gravel in which more than half of the particles are of epiclastic origin
http://inspire.ec.europa.eu/codelist/LithologyValue/mud
2015-08-18 18:04 PM CEST
mud
mud
Clastic sediment consisting of less than 30 percent gravel-size (2 mm) particles and with a mud-size to sand-size particle ratio greater than 1. More than half of the particles are of epiclastic origin.
Clastic sediment consisting of less than 30 percent gravel-size (2 mm) particles and with a mud-size to sand-size particle ratio greater than 1. More than half of the particles are of epiclastic origin.
http://inspire.ec.europa.eu/codelist/LithologyValue/silt
2015-08-18 18:05 PM CEST
silt
silt
Mud that consists of greater than 50 percent silt-size grains.
Mud that consists of greater than 50 percent silt-size grains.
http://inspire.ec.europa.eu/codelist/LithologyValue/clay
2015-08-18 18:02 PM CEST
clay
clay
Mud that consists of greater than 50 percent particles with grain size less than 0.004 mm
Mud that consists of greater than 50 percent particles with grain size less than 0.004 mm
http://inspire.ec.europa.eu/codelist/LithologyValue/sand
2015-08-18 18:05 PM CEST
sand
sand
Clastic sediment in which less than 30 percent of particles are gravel (greater than 2 mm in diameter) and the sand to mud ratio is at least 1. More than half of the particles are of epiclastic origin.
Clastic sediment in which less than 30 percent of particles are gravel (greater than 2 mm in diameter) and the sand to mud ratio is at least 1. More than half of the particles are of epiclastic origin.
http://inspire.ec.europa.eu/codelist/LithologyValue/clasticSedimentaryRock
2015-08-18 18:02 PM CEST
clastic sedimentary rock
clastic sedimentary rock
Sedimentary rock in which at least 50 percent of the constituent particles were derived from erosion, weathering, or mass-wasting of pre-existing earth materials, and transported to the place of deposition by mechanical agents such as water, wind, ice and gravity.
Sedimentary rock in which at least 50 percent of the constituent particles were derived from erosion, weathering, or mass-wasting of pre-existing earth materials, and transported to the place of deposition by mechanical agents such as water, wind, ice and gravity.
http://inspire.ec.europa.eu/codelist/LithologyValue/conglomerate
2015-08-18 18:02 PM CEST
conglomerate
conglomerate
Clastic sedimentary rock composed of at least 30 percent rounded to subangular fragments larger than 2 mm in diameter; typically contains finer grained material in interstices between larger fragments. If more than 15 percent of the fine grained matrix is of indeterminant clastic or diagenetic origin and the fabric is matrix supported, may also be categorized as wackestone. If rock has unsorted or poorly sorted texture with a wide range of particle sizes, may also be categorized as diamictite.
Clastic sedimentary rock composed of at least 30 percent rounded to subangular fragments larger than 2 mm in diameter; typically contains finer grained material in interstices between larger fragments. If more than 15 percent of the fine grained matrix is of indeterminant clastic or diagenetic origin and the fabric is matrix supported, may also be categorized as wackestone. If rock has unsorted or poorly sorted texture with a wide range of particle sizes, may also be categorized as diamictite.
http://inspire.ec.europa.eu/codelist/LithologyValue/diamictite
2015-08-18 18:02 PM CEST
diamictite
diamictite
Unsorted or poorly sorted, clastic sedimentary rock with a wide range of particle sizes including a muddy matrix. Biogenic materials that have such texture are excluded. Distinguished from conglomerate, sandstone, mudstone based on polymodality and lack of structures related to transport and deposition of sediment by moving air or water. If more than 10 percent of the fine grained matrix is of indeterminant clastic or diagenetic origin and the fabric is matrix supported, may also be categorized as wacke.
Unsorted or poorly sorted, clastic sedimentary rock with a wide range of particle sizes including a muddy matrix. Biogenic materials that have such texture are excluded. Distinguished from conglomerate, sandstone, mudstone based on polymodality and lack of structures related to transport and deposition of sediment by moving air or water. If more than 10 percent of the fine grained matrix is of indeterminant clastic or diagenetic origin and the fabric is matrix supported, may also be categorized as wacke.
http://inspire.ec.europa.eu/codelist/LithologyValue/mudstone
2015-08-18 18:04 PM CEST
mudstone
mudstone
Clastic sedimentary rock consisting of less than 30 percent gravel-size (2 mm) particles and with a mud to sand ratio greater than 1.
Clastic sedimentary rock consisting of less than 30 percent gravel-size (2 mm) particles and with a mud to sand ratio greater than 1.
http://inspire.ec.europa.eu/codelist/LithologyValue/shale
2015-08-18 18:05 PM CEST
shale
shale
Laminated mudstone that will part or break along thin, closely spaced layers parallel to stratification.
Laminated mudstone that will part or break along thin, closely spaced layers parallel to stratification.
http://inspire.ec.europa.eu/codelist/LithologyValue/siltstone
2015-08-18 18:05 PM CEST
siltstone
siltstone
Mudstone that contains detectable silt. (see comments)
Mudstone that contains detectable silt. (see comments)
http://inspire.ec.europa.eu/codelist/LithologyValue/claystone
2015-08-18 18:02 PM CEST
claystone
claystone
Mudstone that contains no detectable silt, inferred to consist virtually entirely of clay-size particles.
Mudstone that contains no detectable silt, inferred to consist virtually entirely of clay-size particles.
http://inspire.ec.europa.eu/codelist/LithologyValue/sandstone
2015-08-18 18:05 PM CEST
sandstone
sandstone
Clastic sedimentary rock in which less than 30 percent of particles are greater than 2 mm in diameter (gravel) and the sand to mud ratio is at least 1.
Clastic sedimentary rock in which less than 30 percent of particles are greater than 2 mm in diameter (gravel) and the sand to mud ratio is at least 1.
http://inspire.ec.europa.eu/codelist/LithologyValue/wacke
2015-08-18 18:05 PM CEST
wacke
wacke
Clastic sandstone with more than 10 percent matrix of indeterminate detrital or diagenetic nature. Matrix is mud size silicate minerals (clay, feldspar, quartz, rock fragments, and alteration products).
Clastic sandstone with more than 10 percent matrix of indeterminate detrital or diagenetic nature. Matrix is mud size silicate minerals (clay, feldspar, quartz, rock fragments, and alteration products).
http://inspire.ec.europa.eu/codelist/LithologyValue/arenit
2015-08-18 18:01 PM CEST
2016-06-07 09:21 AM CEST
arenit
arenit
Clastic sandstone that contains less than 10 percent matrix. Matrix is mud-size silicate minerals (clay, feldspar, quartz, rock fragments, and alteration products) of detrital or diagenetic nature.
Clastic sandstone that contains less than 10 percent matrix. Matrix is mud-size silicate minerals (clay, feldspar, quartz, rock fragments, and alteration products) of detrital or diagenetic nature.
http://inspire.ec.europa.eu/codelist/LithologyValue/arenite
2016-06-07 09:21 AM CEST
arenite
arenite
Clastic sandstone that contains less than 10 percent matrix. Matrix is mud-size silicate minerals (clay, feldspar, quartz, rock fragments, and alteration products) of detrital or diagenetic nature.
Clastic sandstone that contains less than 10 percent matrix. Matrix is mud-size silicate minerals (clay, feldspar, quartz, rock fragments, and alteration products) of detrital or diagenetic nature.