Granitic Rocks
encompasses diorite, granodiorite and granite (“granitoids”)
coarse-grained analogues of andesite,dacite & rhyolite, respectively
occur in various tectonic settings: orogenic & collision zones, intraplate, small volumes in MORs and ophiolite complexes
associated hydrothermal mineralization & ore deposits
Common Minerals in Granitic Rocks
quartz
alkali feldspar
plagioclase
pyroxene
amphibole (hornblende)
biotite
muscovite
tourmaline
Mineralogy of Granitic Rocks
diorite: plg + mafic mineral
tonalite: plg + qtz
granodiorite: sodic plg + qtz + alk fsp (plg > alk fsp)
granite: alk fsp + qtz + sodic plg (alk fsp > plg)
alkali granite: alk fsp + qtz
Associated Rocks
Feldspars in Plutonic Rocks
simple twinning → sanidine
tartan twinning → microcline
exsolution texture → perthite
polysynthetic twinning → plagioclase
“Granitic” Rocks
charnockites and mangerites
opx-bearing granites
opx replaces hbl, minor biotite is the only hydrous phase
associated with Proterozoic massif-type anorthosite complexes
Classification of Granitoid Intrusions
Classification of Granitoid Intrusions
I-type granitoids
partial melting of igneous crustal rocks
metaluminous
hornblende and biotite
S-type granitoids
pelitic rocks
peraluminous
muscovite
A-type granitoids
continental rifts
metaluminous or peralkaline
mafic minerals
Alkali Rocks
constitute <1% of all igneous rocks exposed on the Earth’s surface
SiO2 deficiency leads to the various feldspathoids in place of feldspars
magmas formed by partial melting at higher P compared to subalkaline magmas
high concentrations of incompatible elements in many alkali magmas
Nomenclature of Fine-grained Alkali Roks
diversity of feldspathoids: complex nomenclature of alkali rocks
sodic rocks - intraplate and constructive margins (hotspots and divergent)
mildly potassic rocks – island arc and collisional environments (convergent)
Associated Rocks
carbonatite
igneous rock consisting mainly of carbonate minerals (e.g. calcite, dolomite, siderite, ankerite)
crystallized from a carbonate-dominated melt
occurrence: intrusive, effusive or pyroclastic
primarily related to intraplate magmatism; very rare reports from orogenic zones and oceanic basins
rare minerals and metals - REEs, Nb
kimberlite
ultramafic rock consisting of large anhedral olivine (“macrocrysts”) and other mafic minerals in a finer-grained matrix
crystallized from a volatile and chiefly CO2 rich magma
restricted to ancient continental cratons
contains mantle xenoliths – subcontinental lithospheric mantle (SCLM)
economic interest: Diamond xenocrysts (e.g. Africa)