Granitoid
A rock classification type
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About Granitoid
A granitoid is a coarse grained igneous rock composed mostly of quartz, K-feldspar (alkali-feldspar) and plagioclase, with 20-60% quartz on the QAPF diagram. It usually contains minor micas and/or amphiboles. Most commonly granite and granodiorite.
Unique Identifiers
Mindat ID:
48126
Long-form identifier:
mindat:1:1:48126:5
Similar Names
| Granaadid | A synonym of Garnet Supergroup |
| Granatit | A synonym |
Classification of Granitoid

Rocks in sections 2 (alkali-feldspar granite), 3 (granite), 4 (granodiorite) and 5 (tonalite) on the QAPF diagram.
Section 3 can be divided into 3a (syenogranite) and 3b (monzogranite).
Sub-divisions of Granitoid
- Granitoid
- Alkali-feldspar-granite
- Granite
- Adamellite
- Corcovadite
- Felsparite
- Fluorite granite
- Hypidiomorphic granite
- Lithian mica granite
- Muscovite granite
- Ongonite
- Orbicular granite
- Topaz granite
- Syenogranite
- Monzogranite
- Brecciated granite
- Muscovite-biotite granite
- Biotite granite
- Hornblende-biotite granite
- Aplitic granite
- Granophyric granite
- Porphyritic granite
- Leucogranite
- Charnockitic granite
- Melagranite
- Rapakivi granite
- Graphic granite
- Microgranite
- Pegmatitic granite
- Andengranite
- Hornblende granite
- Riebeckite granite
- Fluorine-rich granite
- Caucasite
- Elvan
- Engadinite
- Granodiorite
- Tonalite
- Greisen
- A-type granite
- I-type granite
- S-type granite
- C-type granite
- M-type granite
- Miarolite
Mineralogy of Granitoid
Essential minerals - these are minerals that are required within the classification of this rock:
Non-essential minerals - these minerals are common, sometimes major components, but are not always present:
| Amphibole | A petrological term for Amphibole Supergroup. |
| Feldspar > Alkali Feldspar | A subgroup of the Feldspar Group, poor in calcium, and mostly rich in potassium. |
| Feldspar > Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Mica | A petrological term for Mica Group. |
Age distribution
Recorded ages:
Neochaotian to Neogene : ~4600 Ma to 7.1 ± 0.2 Ma - based on 98 recorded ages.
Sample ages:
| Sample ID | Recorded age | Geologic Time | Dating method |
|---|---|---|---|
| 1 | At least 145 Ma | Late Jurassic | |
| 2 | 50.1 to 49 Ma | Eocene | Rb-Sr |
| 3 | 56.6 ± 1.0 Ma | Paleocene | K-Ar |
| 4 | 58.7 ± 1.6 Ma | Paleocene | Rb-Sr whole rock |
| 5 | 84.9 Ma | Late/Upper Cretaceous | Rb-Sr whole rock |
| 6 | 122 ± 5 Ma | Early/Lower Cretaceous | Rb-Sr whole rock |
| 7 | 129 ± 1 Ma | Early/Lower Cretaceous | U-Pb |
| 8 | 196 ± 4 Ma | Early Jurassic | Rb-Sr whole rock |
| 9 | 236 ± 5 to 194 ± 16 Ma | Mesozoic | Rb-Sr |
| 10 | 253 Ma | Lopingian | |
| 11 | 277 ± 3 Ma | Cisuralian | Rb-Sr isochron |
| 12 | 286 ± 3 Ma | Cisuralian | Rb-Sr whole rock |
| 13 | 302 ± 9 Ma | Pennsylvanian | Rb-Sr |
| 14 | 542 ± 3 Ma | Ediacaran | 207Pb/206Pb |
| 15 | 595 ± 20 Ma | Ediacaran | Rb-Sr seven-point whole rock |
| 16 | 1301 to 1241 Ma | Ectasian | K-Ar |
| 17 | 2500 to 541 ± 1.0 Ma | Proterozoic | |
| 18 | 4000 to 2500 Ma | Archean | |
| 19 | ~4600 to 541 ± 1.0 Ma | Precambrian | |
| 20 | ~4600 to 541 ± 1.0 Ma | Precambrian |
Sample references:
Synonyms of Granitoid
Common Associates
Associations Based on Photo Data:
| 4 photos of Granitoid associated with 'Amphibolite' | |
| 2 photos of Granitoid associated with Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| 1 photo of Granitoid associated with 'Paragneiss' | |
| 1 photo of Granitoid associated with Titanite | CaTiO(SiO4) |
| 1 photo of Granitoid associated with 'Metagabbro' | |
| 1 photo of Granitoid associated with K Feldspar | |
| 1 photo of Granitoid associated with 'Anatexite' | |
| 1 photo of Granitoid associated with 'Hornblende-rock' |
Internet Links for Granitoid
mindat.org URL:
https://www.mindat.org/min-48126.html
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References for Granitoid
Reference List:
Tulloch, A. J. (1979) Secondary Ca-Al silicates as low-grade alteration products of granitoid biotite. Contributions to Mineralogy and Petrology, 69 (2) 105-117 doi:10.1007/bf00371854
Neiva, A.M.R. (1981) Geochemistry of hybrid granitoid rocks and of their biotites from central northern Portugal and their petrogenesis. Lithos, 14 (2) 149-163 doi:10.1016/0024-4937(81)90051-7
Roberts, Malcolm P.; Clemens, John D. (1993) Origin of high-potassium, talc-alkaline, I-type granitoids. Geology, 21 (9). 825-828 doi:10.1130/0091-7613(1993)021<0825:oohpta>2.3.co;2
Barbarin, Bernard (1999) A review of the relationships between granitoid types, their origins and their geodynamic environments. Lithos, 46 (3) 605-626 doi:10.1016/s0024-4937(98)00085-1
FROST, B. RONALD, BARNES, CALVIN G., COLLINS, WILLIAM J., ARCULUS, RICHARD J., ELLIS, DAVID J., FROST, CAROL D. (2001) A Geochemical Classification for Granitic Rocks. Journal of Petrology, 42 (11) 2033-2048 doi:10.1093/petrology/42.11.2033
Bonin, Bernard; Janoušek, Vojtěch; Moyen, Jean-François (2020) Chemical variation, modal composition and classification of granitoids. Geological Society, London, Special Publications, 491 (1). 9-51 doi:10.1144/sp491-2019-138
Zheng, Yong-Fei; Miller, Calvin F.; Xu, Xisheng; Moyen, Jean-François; Wang, Xiao-Lei (2021) Introduction to the origin of granites and related rocks. Lithos, 402-403. 106380 doi:10.1016/j.lithos.2021.106380




Ylämaa area, Lappeenranta, South Karelia, Finland