Cooling and soildification of magma.
Feldspars, biotite, magnetite, and quartz are found in varying degrees in igneous andesitic rocks.
iron
Plagioclase Feldspar and Biotite and Amphibole
Amphibole, plagioclase feldspars, olivine, pyroxene, and biotite mica have the highest crystallization temperatures.
Contrast: Granite consists mainly of quartz, feldspar, and ferromagnesian ("dark") minerals Diorite may be incorrectly called "granite". Diorite contains virtually no quartz, no muscovite, and no K-feldspar. It also contains a higher percentage of dark silicate minerals. Diorite has a salt and pepper appearance. Compare: Both granite and diorite are phaneritic (course-grained) rocks. Diorite is primarily sodium- rich plagioclase feldspar and amphibole, with lesser amounts of biotite. On other minor constituents of granite include muscovite and some dark silicates, particularly biotite and amphibole.
potassiun feldspar, quartz, plagioclase feldspar,biotite, and amphibole.
Feldspars, biotite, magnetite, and quartz are found in varying degrees in igneous andesitic rocks.
iron
Plagioclase Feldspar and Biotite and Amphibole
Plagioclase Feldspar and Biotite and Amphibole
Plagioclase Feldspar and Biotite and Amphibole
Amphibole, plagioclase feldspars, olivine, pyroxene, and biotite mica have the highest crystallization temperatures.
Common rock-forming mafic minerals include olivine, pyroxene,amphibole, biotite mica, and the plagioclase feldspars
Contrast: Granite consists mainly of quartz, feldspar, and ferromagnesian ("dark") minerals Diorite may be incorrectly called "granite". Diorite contains virtually no quartz, no muscovite, and no K-feldspar. It also contains a higher percentage of dark silicate minerals. Diorite has a salt and pepper appearance. Compare: Both granite and diorite are phaneritic (course-grained) rocks. Diorite is primarily sodium- rich plagioclase feldspar and amphibole, with lesser amounts of biotite. On other minor constituents of granite include muscovite and some dark silicates, particularly biotite and amphibole.
Quartz, Potassium Feldspar, Plagioclase Feldspar, Muscovite (mica), Biotite (mica), Amphibole (hornblende), Pyroxene, Olivine, Calcite, Dolomite.
It could be any number of minerals such as biotite mica, or hornblende.
Igneous rocks are usually classified first by their color index. The color index is separated into four categories. Felsic rocks are the lightest and are composed of mostly quartz and potassium feldspar. Intermediate rocks are the second lightest and are made up of mostly plagioclase feldspar, pyroxene, amphibole, and biotite. Mafic rocks are made up of plagioclase feldspar, pyroxene, and amphibole. Ultramafic is made up of mostly olivine, with pyroxene and amphibole.