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 246 to 265 of 3025
| Row | CODE | DESCRIPTION | RCS_STATUS | TRANSLATION | Q1 | Q2 | Q3 | Q4 | USER_ENTERED | DATE_ENTERED | USER_UPDATED | DATE_UPDATED | TRANSFER | DEFINITION_BKING | STATUS |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 246 | BRCQ | Breccia, quartzite | U | Quartzite breccia | quartzite | AWEL | 08-JUN-04 | TMCM | 31-AUG-18 | Siliciclastic arenaceous protolith >50vol% pre-existing siliceous rock clasts. Clasts >50% or dominantly sand-grade, 0.032-2mm. qtz clasts & qtz cement. Deformed (brittle), no foliation or cohesion, >30% frags coarser than matrix, rotation/granulation | C | ||||
| 247 | BREC | Breccia - A type of silicate-conglomerate. In the Rock Classification Scheme, this term may be used for conglomerates made of sharply angular clasts. British Geological Survey Research Report RR/99/03, section 2.1 and fig. 2. Synonym: angular silicate-conglomerate. | N | Breccia | GRBA | 24-FEB-00 | TMCM | 08-MAR-19 | Deformed (brittle), no foliation or cohesion, >30% fragments coarser than matrix, some rotation/granulation. No protolith defined. | C | |||||
| 248 | BRECSL | Breccia, slide | U | Slide breccia | slide | DJLO | 15-DEC-06 | TMCM | 30-AUG-18 | I | Not Available | C | |||
| 249 | BRICK | Brick - A type of artifical deposit. It consists of clay kneaded, moulded, and baked (fired) or sun-dried, usually as small, rectangular blocks. British Geological Survey Research Report RR/99/04, appendix 1. | R | Brick | GRBA | 24-FEB-00 | TMCM | 13-MAR-19 | Not Available | C | |||||
| 250 | BRMA | Basaltic-rock, macroporphyritic (unclassed) | U | Macroporphyritic basaltic-rock (unclassed) | macroporphyritic | AWEL | 15-OCT-03 | TMCM | 31-AUG-18 | Fine-grained, av. <0.25mm normal crystalline extrusive/intrusive rock; CI >35 vol% >40 wt%; quartz <20% or feldspathoid <10% of QAPF, feld >65% plagioclase; TAS SiO2 <52wt%. Phenocrysts, larger, >2mm crystals in finer matrix, size, composition undefined. | C | ||||
| 251 | BRMI | Basaltic-rock, microporphyritic (unclassed) | U | Microporphyritic basaltic-rock (unclassed) | microporphyritic | AWEL | 15-OCT-03 | TMCM | 31-AUG-18 | Fine-grained, av. <0.25mm normal crystalline extrusive/intrusive rock; CI >35 vol% >40 wt%; quartz <20% or feldspathoid <10% of QAPF, feldspar >65% plagioclase; TAS SiO2 <52wt%. Larger but <0.25mm crystals in finer matrix, amount & composition undefined. | C | ||||
| 252 | BRPOCM | Basaltic-rock, plagioclase-olivine-clinopyroxene-macrophyric | U | Plagioclase-olivine-clinopyroxene-macrophyric basaltic-rock | plagioclase | olivine | clinopyroxene | macrophyric | AWEL | 08-OCT-03 | TMCM | 31-AUG-18 | Fine-grained, av. <0.25mm normal crystalline extrusive/intrusive rock; CI >35 vol% >40 wt%; qtz <20% or feldspathoid <10% of QAPF, feldspar >65% plag; TAS SiO2 <52wt%. Pagioclase |
C | |
| 253 | BRPOCP | Basaltic-rock, plagioclase-olivine-clinopyroxene-phyric | U | Plagioclase-olivine-clinopyroxene-phyric basaltic-rock | plagioclase | olivine | clinopyroxene | phyric | AWEL | 19-MAR-04 | TMCM | 31-AUG-18 | Fine-grained, av. <0.25mm normal crystalline extrusive/intrusive rock; CI >35 vol% >40 wt%; quartz <20% or feldspathoid <10% of QAPF, feldspar >65% plagioclase; TAS SiO2 <52wt%. Plagioclase| C |
| |
| 254 | BS | Boulders, sandy [Unlithified Deposits Coding Scheme] | U | Sandy boulders [UDCS] | sandy | AWEL | 17-DEC-04 | TMCM | 30-AUG-18 | Not Available | C | ||||
| 255 | BSC | Boulders, sandy, clayey [Unlithified Deposits Coding Scheme] | U | Clayey sandy boulders [UDCS] | sandy | clayey | DJLO | 20-FEB-09 | TMCM | 30-AUG-18 | I | Not Available | C | ||
| 256 | BSN | Basanite - A type of tephritic-rock. In the Rock Classification Scheme, this name is used for a fine-grained crystalline igneous rock when the modal mineralogy is available, and the mineral mode plots in field 14 of the quartz - alkali feldspar - plagioclase - feldspathoid (QAPF) diagram. Basanite and tephrite are distinguished by the amount of olivine in the CIPW norm: if normative olivine exceeds 10% the rock is basanite. British Geological Survey Research Report RR/99/06, section 5.2 and figs. 17a, 19. | R | Basanite | GRBA | 24-FEB-00 | TMCM | 22-FEB-19 | Fine-grained, av.<0.25mm normal crystalline extrusive/intrusive rock; feldspathoids 10-60% of QAPF, feldspar >90% plagioclase, olivine >10% TAS SiO2 41-49.4wt%, Na2O+K2O 3-9.4wt% | C | |||||
| 257 | BSNAN | Basanite, analcime | U | Analcime basanite | analcime | AWEL | 07-OCT-03 | TMCM | 31-AUG-18 | Fine-grained, av.<0.25mm normal crystalline extrusive/intrusive rock; feldspathoids 10-60% of QAPF, feldspar >90% plagioclase, olivine >10% TAS SiO2 41-49.4wt%, Na2O+K2O 3-9.4wt%. 5-20% analcime. | C | ||||
| 258 | BSNBT | Basanite, biotite | U | Biotite basanite | biotite | AWEL | 26-FEB-01 | TMCM | 31-AUG-18 | Fine-grained, av.<0.25mm normal crystalline extrusive/intrusive rock; feldspathoids 10-60% of QAPF, feldspar >90% plagioclase, olivine >10% TAS SiO2 41-49.4wt%, Na2O+K2O 3-9.4wt%. 5-20% biotite. | C | ||||
| 259 | BSNFDI | Basanitic-foidite - A type of foiditic-rock. In the Rock Classification Scheme, this name is used for a fine-grained crystalline igneous rock when the modal mineralogy is available, and the mineral mode plots in field 15b of the quartz - alkali feldspar - plagioclase - feldspathoid (QAPF) diagram. Basanitic-foidite and tephritic-foidite are distinguished by the amount of olivine in the CIPW norm: if normative olivine exceeds 10% the rock is basanitic-foidite. British Geological Survey Research Report RR/99/06, section 5.2 and figs. 17a, 19. | R | Basanitic-foidite | GRBA | 24-FEB-00 | TMCM | 22-FEB-19 | Fine-grained, av.<0.25mm normal crystalline extrusive/intrusive rock; feldspathoids 60-90% of QAPF, feldspar >50% plagioclase, olivine >10%+B35 | C | |||||
| 260 | BSNT | Basanite (TAS) - A type of tephritic-rock, classified using the total alkali silica (TAS) classification. The TAS classification may be used if the mineral mode of a normal fine-grained crystalline rock cannot be determined due either to the presence of glass or to the fine-grained nature of the rock. The definition of basanite (TAS) is as shown in British Geological Survey Research Report RR/99/06, section 5.2 and figs. 17b, 20. | R | Basanite (TAS) | GRBA | 24-FEB-00 | TMCM | 22-FEB-19 | Fine-grained, av.<0.25mm normal crystalline extrusive/intrusive rock; olivine >10%; TAS SiO2 41-49.4wt%, Na2O+K2O 3-9.4wt% | C | |||||
| 261 | BSP | Boulders, sandy, peaty [Unlithified Deposits Coding Scheme] | U | Peaty sandy boulders [UDCS] | sandy | peaty | AWEL | 17-MAR-04 | TMCM | 30-AUG-18 | Not Available | C | |||
| 262 | BSV | Boulders, sandy, gravelly [Unlithified Deposits Coding Scheme] | U | Gravelly sandy boulders [UDCS] | sandy | gravelly | DJLO | 20-FEB-09 | TMCM | 30-AUG-18 | I | Not Available | C | ||
| 263 | BTLAVA | Lava, basaltic-trachyandesite | U | Basaltic-trachyandesite lava | basaltic | trachyandesite | AWEL | 30-MAY-02 | TMCM | 31-AUG-18 | Fine-grained, av. <0.25mm normal crystalline rock; TAS SiO2 49.4-57wt%, Na2O+K2O 5-9.3wt%. Extruded in molten state & solidified. | C | |||
| 264 | BUXCLY | Bauxite-clay | N | Bauxite-clay | AWEL | 09-MAR-00 | TMCM | 31-AUG-18 | Unlithified material, sediment, particles >50% aluminium hydroxides & iron oxide, dominantly clay-grade <0.004mm. Other mineral particles/grains present as impurities. | C | |||||
| 265 | BV | Boulders, gravelly [Unlithified Deposits Coding Scheme] | U | Gravelly boulders [UDCS] | gravelly | DJLO | 20-FEB-09 | TMCM | 30-AUG-18 | I | Not Available | C |
Displaying rows 246 to 265 of 3025