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Lamprophyre
A rock classification type
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About Lamprophyre
A group of hypabyssal igneous rocks characterised by abundant primary hydrous silicates (usually amphiboles or biotite) in phenocrysts and/ or groundmass, lacking felsic phenocrysts, and usually occurring in dykes. They have widely varying origin and compositions, commonly alkaline and basic to ultrabasic.
They are dark-colored and porphyritic, characterized by panidiomorphic texture, and a high percentage of mafic minerals (esp. biotite, hornblende, and pyroxene), which form the phenocrysts. The fine-grained groundmass contains the same mafic minerals in addition to feldspars and/or feldspathoids. Most lamprophyres are highly altered.
They are commonly associated with carbonatites.
They are dark-colored and porphyritic, characterized by panidiomorphic texture, and a high percentage of mafic minerals (esp. biotite, hornblende, and pyroxene), which form the phenocrysts. The fine-grained groundmass contains the same mafic minerals in addition to feldspars and/or feldspathoids. Most lamprophyres are highly altered.
They are commonly associated with carbonatites.
Unique Identifiers
Mindat ID:
48064
Long-form identifier:
mindat:1:1:48064:6
Classification of Lamprophyre
- Rock
- Igneous rock
- Exotic crystalline igneous rock
- Lamprophyre
- Ultrapotassic rock
- Lamprophyre
- Exotic crystalline igneous rock
- Igneous rock
Sub-divisions of Lamprophyre
Mineralogy of Lamprophyre
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 > K Feldspar | Potassium-dominant feldspars with variable crystal symmetry and Al-Si ordering state; they are a subgroup of ... |
| Feldspar > Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Feldspathoid | A family of rock-forming minerals consisting of aluminosilicates of sodium, potassium, or calcium and having too ... |
| Mica | A petrological term for Mica Group. |
Age distribution
Recorded ages:
Phanerozoic : 296 ± 5 Ma to 22 Ma - based on 15 recorded ages.
Sample ages:
| Sample ID | Recorded age | Geologic Time | Dating method |
|---|---|---|---|
| 1 | 22 Ma | Miocene | K-Ar |
| 2 | 22.78 ± 0.88 Ma | Miocene | K-Ar |
| 3 | 95.2 ± 4.8 Ma | Late/Upper Cretaceous | K-Ar |
| 4 | 107 ± 4 Ma | Early/Lower Cretaceous | K-Ar |
| 5 | 110 ± 3 to 108 ± 3 Ma | Early/Lower Cretaceous | |
| 6 | 183.2 ± 2.2 Ma | Early Jurassic | Ar-Ar |
| 7 | 229 Ma | Late/Upper Triassic | Rb-Sr whole rock |
| 8 | 235 Ma | Late/Upper Triassic | K-Ar |
| 9 | 245 ± 12 Ma | Middle Triassic | K-Ar |
| 10 | 279 ± 6 Ma | Cisuralian | K-Ar |
| 11 | 291 ± 6 Ma | Cisuralian | |
| 12 | 296 ± 5 Ma | Cisuralian | K-Ar |
Sample references:
Chemical Analysis
Oxide wt%:
| 1 | 2 | |
|---|---|---|
| SiO2 | 43.14 % | 39.75 % |
| Al2O3 | 12.07 % | 15.11 % |
| TiO2 | 3.11 % | 3.97 % |
| Fe2O3 | 2.00 % | 2.00 % |
| FeO | 10.97 % | 11.42 % |
| MgO | 10.32 % | 6.45 % |
| MnO | 0.17 % | 0.22 % |
| Na2O | 2.93 % | 3.66 % |
| CaO | 12.72 % | 13.17 % |
| K2O | 0.95 % | 1.8 % |
| P2O5 | 0.40 % | 1.19 % |
| Total: | 98.78 % | 98.74 % |
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%. |
Other Language Names for Lamprophyre
German:Lamprophyr
Common Associates
Associations Based on Photo Data:
| 2 photos of Lamprophyre associated with Calcite | CaCO3 |
| 2 photos of Lamprophyre associated with 'Leucogranite' | |
| 1 photo of Lamprophyre associated with Andradite | Ca3Fe3+2(SiO4)3 |
| 1 photo of Lamprophyre associated with 'Marble' | |
| 1 photo of Lamprophyre associated with 'Skarn' | |
| 1 photo of Lamprophyre associated with Silvialite | (Ca,Na)4(Al6Si6O24)(SO4,CO3) |
Internet Links for Lamprophyre
mindat.org URL:
https://www.mindat.org/min-48064.html
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Palafrugell, Girona, Catalonia, Spain