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Syenitoid
A rock classification type
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About Syenitoid
A coarse grained felsic igneous rock having an alkali-feldspar/plagioclase ratio from 0.9-0.35, 0-10% foids and 0-20% quartz.
Unique Identifiers
Mindat ID:
48178
Long-form identifier:
mindat:1:1:48178:8
Classification of Syenitoid

Rocks in sections 6,6*,6',7,7*,7',8,8* and 8' of the QAPF diagram.
Sub-divisions of Syenitoid
Mineralogy of Syenitoid
Essential minerals - these are minerals that are required within the classification of this rock:
| Feldspar > Alkali Feldspar | A subgroup of the Feldspar Group, poor in calcium, and mostly rich in potassium. |
Non-essential minerals - these minerals are common, sometimes major components, but are not always present:
| Amphibole > Hornblende | AnCa2(Z2+5-mZ3+m)(Si8-(n+m)Al(n+m))(OH,F,Cl)2 |
| Mica > Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
Pronunciation of Syenitoid
Pronunciation:
| Play | Recorded by | Country |
|---|---|---|
| Jolyon Ralph | United Kingdom |
Age distribution
Recorded ages:
to Neogene : 2360 ± 96 Ma to 10.4 ± 0.3 Ma - based on 74 recorded ages.
Sample ages:
| Sample ID | Recorded age | Geologic Time | Dating method |
|---|---|---|---|
| 1 | 11.1 ± 0.5 Ma | Miocene | |
| 2 | 24.1 ± 1.2 Ma | Oligocene | Rb-Sr |
| 3 | 45 ± 1 Ma | Eocene | K-Ar |
| 4 | 87.1 to 78.7 Ma | Late/Upper Cretaceous | K-Ar |
| 5 | 121 to 105 Ma | Early/Lower Cretaceous | |
| 6 | 127 ± 0.8 Ma | Early/Lower Cretaceous | U-Pb |
| 7 | 129.9 ± 0.8 Ma | Early/Lower Cretaceous | LA-ICP-MS zircon U-Pb |
| 8 | 130.1 ± 1.0 Ma | Early/Lower Cretaceous | LA-ICP-MS zircon U-Pb |
| 9 | 134.8 Ma | Early/Lower Cretaceous | K-Ar whole rock |
| 10 | 145 to 143 Ma | Early/Lower Cretaceous | K-Ar |
| 11 | 173 ± 2 Ma | Middle Jurassic | Rb-Sr whole rock |
| 12 | 223 ± 9 Ma | Late/Upper Triassic | Rb-Sr whole rock |
| 13 | 256 ± 6 to 261 ± 6 Ma | Permian | Whole rock K/Ar |
| 14 | 300 ± 6 Ma | Pennsylvanian | |
| 15 | 351 ± 7 Ma | Mississippian | K-Ar |
| 16 | 409 ± 2 Ma | Early/Lower Devonian | LA-ICP-MS zircon U-Pb |
| 17 | 526 ± 26 Ma | Terreneuvian | K-Ar |
| 18 | 767 ± 8 Ma | Tonian | Rb-Sr isochron |
| 19 | 1190 ± 25 Ma | Stenian | K-Ar |
| 20 | 2360 ± 96 Ma | Siderian | Rb-Sr of 6 syenites |
Sample references:
Chemical Analysis
Oxide wt%:
| 1 | 2 | 3 | |
|---|---|---|---|
| SiO2 | 56.86 % | 51.44 % | 55.75 % |
| Al2O3 | 19.46 % | 19.66 % | 16.31 % |
| TiO2 | 0.99 % | 1.65 % | 1.43 % |
| Fe2O3 | 2.00 % | 2.00 % | 3.09 % |
| FeO | 2.34 % | 4.5 % | 6.23 % |
| MgO | 0.63 % | 1.5 % | 1.32 % |
| MnO | 0.16 % | 0.27 % | 0.21 % |
| Na2O | 7.57 % | 7.10 % | 5.91 % |
| CaO | 3.72 % | 7.26 % | 3.54 % |
| K2O | 5.89 % | 3.85 % | 4.92 % |
| P2O5 | 0.12 % | 0.28 % | 0.5 % |
| H20 | 0.57 % | ||
| Total: | 99.74 % | 99.51 % | 99.78 % |
Sample references:
| ID | Locality | Reference | Notes |
|---|---|---|---|
| 1 | Mont Royal, Montréal, Québec, Canada | Wet chemical analysis by G. Woussen and B.M.Gunn. The Fe2O3 percentage is arbitrarily set to 2%. | |
| 2 | " " | Wet chemical analysis by G. Woussen and B.M.Gunn. The Fe2O3 percentage is arbitrarily set to 2%. | |
| 3 | Ilímaussaq complex, Kujalleq, Greenland | Average of 8 analyses of a rock containing K-feldspar/perthites (72.4 vol%), pyroxene (6.9vol%), amphibole(3.7 vol%), olivine (6.3 vol%), mica (5.5 vol%), apatite (1 vol%), opaques (3.6 vol%), chlorite (0.6 vol%) & nepheline (tr). Analytical method is not given but presumably wet chemical. |
Synonyms of Syenitoid
Internet Links for Syenitoid
mindat.org URL:
https://www.mindat.org/min-48178.html
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References for Syenitoid
Reference List:
Le Maitre, R. W. - Ed. (2002) Igneous Rocks - A Classification and Glossary of Terms (2nd ed.) Cambridge University Press. doi:10.1017/cbo9780511535581
Verner, Kryštof, Jiří Žák, , Hrouda, František, Holub, František V. (2006) Magma emplacement during exhumation of the lower- to mid-crustal orogenic root: The Jihlava syenitoid pluton, Moldanubian Unit, Bohemian Massif. Journal of Structural Geology, 28 (8). 1553-1567 doi:10.1016/j.jsg.2006.03.037
Janoušek, Vojtěch, Holub, František V., Verner, Kryštof, Čopjaková, Renata, Gerdes, Axel, Hora, John M., Košler, Jan, Tyrrell, Shane (2019) Two-pyroxene syenitoids from the Moldanubian Zone of the Bohemian Massif: Peculiar magmas derived from a strongly enriched lithospheric mantle source. Lithos, 342. 239-262 doi:10.1016/j.lithos.2019.05.028





Sagåsen Quarry, Sagåsen, Auenlandet, Porsgrunn, Telemark, Norway