Vocabularies — view dictionary terms
DIC_ROCK_NAMEV3 (3025 rows)
Dictionary table which is part of version 3 of the BGS Rock Classification Scheme. The main part of the RCS - it contains only single lithologies.
Displaying rows 601 to 620 of 3025
| Row | CODE | DESCRIPTION | RCS_STATUS | TRANSLATION | Q1 | Q2 | Q3 | Q4 | USER_ENTERED | DATE_ENTERED | USER_UPDATED | DATE_UPDATED | TRANSFER | DEFINITION_BKING | STATUS |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 601 | FELRB | Felsite, riebeckite | U | Riebeckite felsite | riebeckite | AWEL | 30-JUN-03 | TMCM | 31-AUG-18 | Generally light coloured fine-grained, aphanitic (>75% crystals <0.25mm) normal crystalline rock; quartz <60% or feldspathoids <10% QAPF, remainder dominantly feldspar; with 5-20% riebeckite. | C | ||||
| 602 | FELS | Felsite - A type of fine-grained normal crystalline rock. It is a general term used for light-coloured aphanitic rocks. In the Rock Classification Scheme, the class includes rhyolitic-rock, dacitic-rock, and trachytic-rock. British Geological Survey Research Report RR/99/06, section 5.2 and fig. 17. | A | Felsite | GRBA | 24-FEB-00 | TMCM | 22-FEB-19 | Generally light coloured fine-grained, aphanitic (>75% crystals <0.25mm) normal crystalline rock; quartz <60% or feldspathoids <10% QAPF, remainder dominantly feldspar; rhyodacite is a felsite | C | |||||
| 603 | FELSAB | Felsite, albitised | U | Albitised felsite | albitised | AWEL | 07-OCT-03 | TMCM | 31-AUG-18 | Generally light coloured fine-grained, aphanitic (>75% crystals <0.25mm) normal crystalline rock; quartz <60% or feldspathoids <10% QAPF, remainder dominantly feldspar. Metamorphosed by introduction/altertion of other minerals to albite, degree undefined. | C | ||||
| 604 | FELSFO | Felsite, foliated | U | Foliated felsite | foliated | GRBA | 24-FEB-00 | TMCM | 31-AUG-18 | Fine-grained, av. <0.25mm generally light coloured aphanitic (>75% crystals <0.25mm) normal crystalline rock, preferred planar orientation of inequidiamensional minerals; quartz <60% or felspathoids <10% of QAPF, remainder dominantly feldspar | C | ||||
| 605 | FELSH | Felsite, sheared | U | Sheared felsite | sheared | AWEL | 15-FEB-01 | TMCM | 31-AUG-18 | Generally leucocratic fine-grained, aphanitic (>75% crystals <0.25mm) normal crystalline rock; quartz <60% or feldspathoid <10% QAPF, remainder dominantly feldspar. Relative movement of contiguous parts parallel to their plane of contact, cleavage. | C | ||||
| 606 | FELSP | Felsite, porphyritic | U | Porphyritic felsite | porphyritic | AWEL | 13-MAR-01 | TMCM | 31-AUG-18 | Generally light coloured fine-grained, aphanitic (>75% crystals <0.25mm) normal crystalline rock; quartz <60% or feldspathoids <10% QAPF, remainder dominantly feldspar.Contains undefined phenocrysts, larger crystals in finer matrix. | C | ||||
| 607 | FELSPF | Felsite, foliated-porphyritic | U | Foliated-porphyritic felsite | foliated | porphyritic | AWEL | 14-FEB-01 | TMCM | 31-AUG-18 | Usually light coloured fine-grained, aphanitic (>75% crystals <0.25mm) norm crystalline rock; qtz <60% or foid <10% QAPF, remainder mainly feldspar. Larger crystals in finer matrix. <5mm planar structure, preferred orientation of platy/prismatic minerals. | C | |||
| 608 | FELSQP | Felsite, quartz-phyric | U | Quartz-phyric felsite | quartz-phyric | AWEL | 01-SEP-03 | TMCM | 31-AUG-18 | Generally light coloured fine-grained, aphanitic (>75% crystals <0.25mm) normal crystalline rock; quartz <60% or feldspathoids <10% QAPF, remainder dominantly feldspar. Quartz 5-20% as phenocrysts, larger crystals in finer matrix. | C | ||||
| 609 | FELSR | Felsic-rock | N | Felsic-rock | AWEL | 23-JAN-02 | TMCM | 31-AUG-18 | Normal igneous rock grain-size undefined consisting dominantly of felsic minerals; quartz or feldspathoid, (nephelene/leucite/sodalite/nosean/analcime etc) alkali feldspar, (orthoclase/microcline/anorthoclase/sodic albite etc), plagioclase & scapolite. | C | |||||
| 610 | FEMDST | Iron-mudstone - A type of ironstone, classified on the basis of its depositional texture. In the Rock Classification Scheme, it is a matrix-supported ironstone composed of greater than 75% matrix (mud-grade material smaller than 32 µm). British Geological Survey Research Report RR/99/03, section 5.2, table 14 and fig. 9. | R | Iron-mudstone | GRBA | 24-FEB-00 | TMCM | 08-MAR-19 | Sedimentary rock (>15wt % iron), with particles >50% iron-bearing minerals (15wt% iron). Particles >50% or predominantly mud-grade, <0.032mm. | C | |||||
| 611 | FEMG | Ironstone, manganiferous | U | Manganiferous ironstone | manganiferous | AWEL | 26-JUL-04 | TMCM | 31-AUG-18 | Sedimentary rock (>15wt% iron), no recognisable depositional texture with particles >50% iron-bearing minerals (15wt% iron). Particle size not defined. 5-20% manganese minerals. | C | ||||
| 612 | FEMONC | Microoncoid-ironstone - A type of ironstone composed dominantly of microoncoids. British Geological Survey Research Report RR/99/03, section 5.2, table 15 and fig. 9. Synonym: iron-microoncolite. | R | Microoncoid-ironstone | GRBA | 24-FEB-00 | TMCM | 08-MAR-19 | Sedimentary rock (>15wt% iron), with particles >50% iron-bearing minerals (15wt% iron). Allochem dominantly as micro-oncoids, <2mm coated grains with irregular partially overlapping laminae, biogenic structures may be present. Particle size not defined. | C | |||||
| 613 | FEMUD | Iron-mud - A type of iron-sediment. In the Rock Classification Scheme, it is one in which over 75% of the clasts are smaller than 32 µm. The grain size classes are defined in the same way as the siliciclastic sediments. British Geological Survey Research Report RR/99/03, section 5.1, table 13 and fig. 9. See also: silicate-mud. | R | Iron-mud | GRBA | 24-FEB-00 | TMCM | 08-MAR-19 | Sediment (>15wt % iron) with particles >50% iron-bearing minerals (15wt% iron). Particles >50% or predominantly mud-grade, <0.032mm. | C | |||||
| 614 | FENITE | Fenite - A type of metasomatic-rock. Fenites are desilicated crustal rocks formed by reaction with Na- and K-rich fluids expelled during the emplacement of carbonatite or undersaturated alkaline magmas. British Geological Survey Research Report RR/99/02, section 8. | R | Fenite | GRBA | 24-FEB-00 | TMCM | 22-FEB-19 | Metamorphic rock (grain size & protolith undefined) with significant chemical/mineralogical alteration, desilicated due to reaction with Na/K-rich fluids derived from carbonatite/unsaturated alkaline magmas; a metasomatic rock | C | |||||
| 615 | FEOCBT | Ferrocarbonatite - A type of carbonatite. In the Rock Classification Scheme, this term may be used when a chemical classification is necessary because the rock is too fine grained for an accurate mode to be determined, or if the carbonate minerals are complex Ca-Mg-Fe solid solutions. The definition of ferrocarbonatite is as shown in British Geological Survey Research Report RR/99/06, section 6.1 and figs. 25, 26. See also: ferroan-carbonatite. | R | Ferrocarbonatite | GRBA | 24-FEB-00 | TMCM | 22-FEB-19 | Fine grained, av. between 0.032-0.25mm exotic crystalline intrusive/extrusive rock >50% modal primary carbonates or complex Ca-Mg-Fe carbonates; CaO <90wt%, Fe-Mn oxides >10wt%, MgO <50wt% of Ca+Mg+Fe+Mn oxides; chemical wt% oxide classification | C | |||||
| 616 | FEONC | Oncoid-ironstone - A type of ironstone composed dominantly of oncoids. British Geological Survey Research Report RR/99/03, section 5.2, table 15 and fig. 9. Synonym: iron-oncolite. | R | Oncoid-ironstone | GRBA | 24-FEB-00 | TMCM | 08-MAR-19 | Sediment (>15wt% iron), with particles >50% iron-bearing minerals (15wt% iron). Allochem dominantly as oncoids, >2mm coated grains with irregular partially overlapping laminae, biogenic structures may be present. Particle size not defined. | C | |||||
| 617 | FEOOL | Ooid-ironstone - A type of ironstone composed dominantly of ooids. British Geological Survey Research Report RR/99/03, section 5.2, table 15 and fig. 9. Synonyms: ooidal ironstone; ironstone, ooidal. | R | Ooid-ironstone | AWEL | 24-FEB-00 | TMCM | 08-MAR-19 | Sediment (>15wt% iron), with particles >50% iron-bearing minerals (15wt% iron). Ooids dominant allochem, <2mm coated grains with smooth regular laminae, usually spherical/ellipsoidal no obvious biogenic structures.Particle size not defined. | C | |||||
| 618 | FEPEL | Peloid-ironstone - A type of ironstone composed dominantly of peloids. British Geological Survey Research Report RR/99/03, section 5.2, table 15 and fig. 9. Synonym: iron-peloidite. | R | Peloid-ironstone | GRBA | 24-FEB-00 | TMCM | 08-MAR-19 | Sediment (>15wt% iron), with particles >50% iron-bearing minerals (15wt% iron). Peloids dominant allochem, 0.01 to 0.5mm spherical/ellipsoidal microcrystalline carbonate grains, internally structureless. If faecal origin, pellet. | C | |||||
| 619 | FEPIS | Pisoid-ironstone - A type of ironstone composed dominantly of pisoids. British Geological Survey Research Report RR/99/03, section 5.2, table 15 and fig. 9. Synonym: iron-pisolite. | R | Pisoid-ironstone | GRBA | 24-FEB-00 | TMCM | 08-MAR-19 | Sediment (>15wt% iron), with particles >50% iron-bearing minerals (15wt% iron). Pisoids dominant allochem, >2mm coated grains with smooth regular laminae, usually spherical/ellipsoidal no obvious biogenic structures.Particle size not defined. | C | |||||
| 620 | FEPST | Iron-packstone - A type of ironstone, classified on the basis of its depositional texture. It is a grain-supported ironstone with intergranular spaces filled by matrix (mud-grade material smaller than 32 µm). British Geological Survey Research Report RR/99/03, section 5.2, table 14 and fig. 9. | R | Iron-packstone | GRBA | 24-FEB-00 | TMCM | 08-MAR-19 | Grain-supported sedimentary rock (>15wt % iron) with grains >50% iron-bearing minerals (15wt% iron). Matrix (grains<0.032mm) fills intergranular spaces. Non-matrix grain size not defined. | C |
Displaying rows 601 to 620 of 3025