| value | description | source | basis | axis | genesis | SMR comments |
| Alkalic | Peacock (1931) alkali-lime index is less than 51, i.e. the total of alkali oxides (Na20+K20) exceeds that of Ca0 at a silica content less than 51 percent. | Neuendorf et al 2005; SMR | chemical | (Na+K)/Ca oxides | igneous | technically should be defined for a series of related (comagmatic) igneous rocks) |
| Alkali-calcic | Peacock (1931) alkali-lime index is between 51 and 56, i.e. the total of alkali oxides (Na20+K20) exceeds that of Ca0 at a silica content between 51 and 56 percent. | Neuendorf et al 2005; SMR | chemical | (Na+K)/Ca oxides | igneous | technically should be defined for a series of related (comagmatic) igneous rocks) |
| ALKALINE | syn alkalic | deprecate | igneous | use alkalic | ||
| AMPHIBOLE PHYRIC | deprecate | igneous | ||||
| Amphibole-rich mafic | material consisting of greater than or equal to 40 percent dark-colored amphibole | NADM SLTTm nongenetic | mineralogy | amphibole | NA | too specific, use earth material composition |
| AMPHIBOLITIC | deprecate | Amphibole | metamorphic | usage generally seems to mean amphibolite-like, but quantification is unconstrained | ||
| BIOTITE PHYRIC | deprecate | biotite | igneous | don'tinclude phenocryst mineralogy as composition category | ||
| BIOTITIC | deprecate | biotite | NA | not quantitative, overlaps with mafic | ||
| Calc-alkalic | Peacock (1931) alkali-lime index is between 56 and 61, i.e. the total of alkali oxides (Na20+K20) exceeds that of Ca0 at a silica content between 56 and 61 percent. | Neuendorf et al 2005; SMR | chemical | (Na+K)/Ca oxides | igneous | technically should be defined for a series of related (comagmatic) igneous rocks) |
| Calcareous quartzo-feldspathic | material consists of 10-50 percent carbonate or calcsilicate minerals, and micaceous or aluminous minerals form less than 40 percent of non-(carbonate or calcsilicate) minerals and quartz forms less than 60 percent of the non-carbonate + calcsilicate minerals. | NADM metamorphic rock vocabulary SLTTm1.0 | deprecate | carbonate, calcsilicate, micaceous/aluminous, quartz | NA | since multiple values are allowed for composition category, this could be represented as calcareous, and quarzto-feldspathic |
| Calcareous-pelitic | material consists of 10-50 percent carbonate or calcsilicate minerals, and micaceous or aluminous minerals form greater than or equal to 40 percent of non-(carbonate or calcsilicate) minerals. | NADM metamorphic rock vocabulary SLTTm1.0 | deprecate | carbonate, calcsilicate, micaceous/aluminous, quartz | NA | since multiple values are allowed for composition category, this could be represented as calcareous, and pelitic |
| Calcareous-quartzose | material consists of 10-50 percent carbonate or calcsilicate minerals, and micaceous or aluminous minerals form less than 40 percent of non-(carbonate or calcsilicate) minerals, and quartz forms greater than or equal to 75 percent of the non-(carbonate + calcsilicate) minerals | NADM metamorphic rock vocabulary SLTTm1.0 | deprecate | carbonate, calcsilicate, micaceous/aluminous, quartz | NA | since multiple values are allowed for composition category, this could be represented as calcareous, and quartzsose |
| Calcareous-semi-pelitic | material for which the sum of modal quartz+feldspar+ mica + aluminous mineral is greater than or equal to 70 percent, and quartz+ feldspar less than 60 percent and carbonate + calcsilicate minerals greater than 10 percent. | NADM metamorphic rock vocabulary SLTTm1.0 | deprecate | carbonate, calcsilicate, micaceous/aluminous, quartz | NA | since multiple values are allowed for composition category, this could be represented as calcareous, and semi |
| Calcic | Peacock (1931) alkali-lime index is greater than 61 i.e. the total of alkali oxides (Na20+K20) exceeds that of Ca0 at a silica content greater than 61 percent. | Neuendorf et al 2005; SMR | chemical | (Na+K)/Ca oxides | igneous | technically should be defined for a series of related (comagmatic) igneous rocks) |
| Cherty | Sedimentary material contains enough secondary-chert nodules to influence the geologist’s description | deprecate | outcrop level, Geologic unit, not material term. Deprecate | |||
| Eclogite composition | material consists of greater than 75 percent garnet (almandine-pyrope) and sodic pyroxene (omphacite). | NADM metamorphic rock vocabulary SLTTm1.0 | mineralogy | garnet, pyroxene | NA | too specific, use earth material composition |
| Epidositic | Material consists of greater than 75 percent epidote, and greater than 50 percent of non-epidote mineral is quartz. | NADM metamorphic rock vocabulary SLTTm1.0 | mineralogy | epidote | NA | too specific, use earth material composition |
| FELDSPAR PHYRIC | deprecate | feldspar | igneous | don'tinclude phenocryst mineralogy as composition category | ||
| FERRUGINIZED | deprecate | metasomatic | not sure what this means… | |||
| garnetifierous | significant garnet is present | mineralogy | garnet | NA | too specific, use earth material composition | |
| Greisen composition | Material consists of greater than 70 percent quartz + muscovite or lepodilite, with accessory (greater than 1 percent) topaz or tourmaline (or other flourine-bearing phase). In a hierarchy based purely on description, would be a kind of semi-pelitic rock (10-40 percent aluminous minerals; less than 60 percent quartz+feldspar) or quartz-feldspathic (less than 40 percent aluminous and greater than 60 percent quartz + feldspar). | NADM metamorphic rock vocabulary SLTTm1.0 | deprecate | quartz, muscovite, tourmaline | NA | duplicate value--could use semi-pelitic or quartz-feldspathic |
| Iron oxide bearing | greater than accessory amounts (greater than 5 percent by volume) of iron oxide mineral phases are present | Struik etal 2002; SMR defintion | mineralogy | iron oxide | NA | too specific, use earth material composition |
| Manganese oxide bearing | greater than accessory amounts (greater than 5 percent by volume) of manganese oxide mineral phases are present | Struik etal 2002; SMR defintion | mineralogy | MnOx | NA | too specific, use earth material composition |
| MUSCOVITE-BEARING | Material contains signficant muscovite | deprecate | muscovite | NA | better represented through material composition to minerals | |
| Non-carbonate chemical | a chemical sedimentary or metasomatic rock predominantly comprised of non-carbonate minerals | deprecate | carbonate | NA | too genetic, no composition information | |
| OLIVINE PHYRIC | deprecate | olivine | igneous | don'tinclude phenocryst mineralogy as composition category | ||
| Organic | organic—“Pertaining or relating to a compound containing carbon, especially as an essential component....A substance containing carbon, as in such expressions as “organic-rich shale” Glossary of Geology (Jackson, 1997, p. 451) | Jackson 1997 | deprecate | carbon | NA | genetic denotation is undesirable |
| PALAGONITIZED | alteration | palagonite | metasomatic | Palagonitization is a common, but imperfectly defined process that greatly modifies the physical and chemical properties of glassy basaltic tephra deposited in subaquatic/subglacial environments , ,, the process of palagonitization (1) initially results in the formation of ‘palagonitized glass’, a quasi- or nano-crystalline, rind-like material that contains smectite, as well as lesser amounts of other clays (e.g. serpentine), and (2) eventually results in consolidation of tephra, mediated through the accretion of palagonitized glass and later-formed authigenic cements. (Schiffman, Southard, Eberl, Bishop, 2002, Geological Society, London, Special Publications; v. 202; p. 393-405; DOI: 10.1144/GSL.SP.2002.202.01.20) Palagonite is an altered basaltic glass (Neuendorf et al 2005). | ||
| PYROXENE PHYRIC | deprecate | pyroxene | igneous | don'tinclude phenocryst mineralogy as composition category | ||
| PYROXENE-BEARING | Material contains significant pyroxene | mineralogy | pyroxene | NA | better represented through material composition to minerals | |
| QUARTZ PHYRIC | deprecate | quartz | igneous | don'tinclude phenocryst mineralogy as composition category | ||
| SEMIPELITIC | deprecate | |||||
| Serpentinite composition | Material consists of greater than 75 percent serpentine. | NADM metamorphic rock vocabulary SLTTm1.0 | deprecate | serpentine | NA | too specific |
| SILICEOUS | deprecate | SiO2 | NA | meaning not quantified | ||
| Siliciclastic | a clastic sedimentary rock comprised of silicate minerals | sed petrography | quartz feldspar | sedimentary | redundant with silicic or quartzo-feldspathic | |
| Special composition | Mineral composition that doesn't fit in any other defined composition class. A modal mineral description is essential. Material consists of less than 40 percent ferromagnesian minerals and less than 50 percent carbonate + calcsilicate minerals and less than 70 percent Q+Fs + mica + aluminous minerals. | NADM metamorphic rock vocabulary SLTTm1.0 | deprecate | carbonate, calcsilicate, micaceous/aluminous, quartz | NA | duplicate with other composition |
| x Argillic | Apparently clay mineral-rich material. | NADM metamorphic rock vocabulary SLTTm1.0 | deprecate | clay | NA | duplicate |
| xacid | an igneous rock containing greater than 60-65% SiO2 by weight | deprecate | SIO2 | igneous | use high silica, intermediate silica, low silicat to make meaning clearer. | |
| xACID-INTERMEDIATE | deprecate | SIO2 | igneous | use high silica, intermediate silica, low silicat to make meaning clearer. | ||
| xArgillaceous | Sedimentary material contains > 10% detrital clay minerals, based on field inspection | deprecate | clay | sedimentary | use argillic | |
| xbasic | an igneous rock containing SiO2 approximately in the range 44-52% | deprecate | SiO2 | igneous | use high silica, intermediate silica, low silicat to make meaning clearer. | |
| xBASIC-ULTRABASIC | deprecate | SiO2 | igneous | use high silica, intermediate silica, low silicat to make meaning clearer. | ||
| xcalcsilicate or impure carbonate | a sedimentary or metamorphosed sedimentary rock comprised of calcsilicate or carbonate and silicate minerals | deprecate | carbonate, calcsilicate | sedimentary, metamorphic | use Impure calcsilicate or carbonate | |
| xcarbonaceous | “(a) Said of a rock or sediment that is rich in carbon; coaly. (b) Said of a sediment containing organic matter” (Jackson, 1997, p. 39). | Jackson 1997 | deprecate | carbon, hydrocarbon | NA | |
| xcarbonate | Material composed of carbonate minerals | deprecate | carbonate | NA | ||
| xINTERMEDIATE-BASIC | deprecate | SiO2 | igneous | use high silica, intermediate silica, low silicat to make meaning clearer. | ||
| xPSAMMITIC | deprecate | deprecate | Originally used as synonym for arenite; used to describe metamorphic rock derived from sandy protolith (Neuendorf et al2005); connotation of quartzo-feldspathic composition is common | |||
| xquartz-lithic | deprecate | QFL | not clear what this is supposed to mean | |||
| xQuartzose | Material contains enough quartz to influence the geologist’s description | deprecate | quartz | duplicate | ||
| xultrabasic | an igneous rock containing less than about 44% SiO2 | deprecate | SiO2 | igneous | use high silica, intermediate silica, low silicat to make meaning clearer. | |