2000
Because both crystallize at similar temperatures and pressures according to Bowen's Reaction Series.
Labradorite ((Ca,Na)(Al,Si)4O8) is a Plagioclase Feldspar mineral. It has a ratio of Calcium to Sodium of between 50%Ca:50%Na and 70%Ca:30%Na and as such forms part of the Plagioclase solid solution series between the Calcium (Anorthite - CaAl2Si2O8) and Sodium (Albite - NaAlSi3O8) rich feldspars.
The plagioclase feldspar ranges from sodium-rich albite at low temperatures to calcium-rich anorthite at high temperatures. The difference in the mineral's appearance is due to a slight change in the chemical composition and a difference in growth pattern as the temperature changes. At intermediate temperatures, both calcium and sodium are incorporated in the crystal structure, building up alternating layers that allow light to refract or scatter, producing a range of colors.
Diorite is a dark, granite-textured, crystalline rock that is rich in plagioclase and has a little amount of quartz. Its dominant mineral is the gray or white plagioclase feldspar.
Calcium
Olivine... if you can find on the internet the "Bowens Reaction Series" paper, it will tell you that Olivine is the first to crystallize
Plagioclase.
Anorthite
Basalt when metamorphosed turns to the following rocks: (LEAST PRESSURE AND TEMPERATURE TO THE MOST) + mineralogy -Greenschist-albite, epidote, chlorite -Amphibolite-amphioble, plagioclase feldspar -Granulite-calcium-rich pyroxene and plagioclase feldspar -Eclogite-sodium-rich pyroxene and garnet
Most commonly one expects the calcium-feldspar plagioclase as phenocryst.
It depends on the type of feldspar. Potassium Feldspar (also called K-Spar), contains potassium, aluminum, silicate: KAlSi3O8. Plagioclase Feldspar, on the other hand, contains calcium or sodium, aluminum, and silicate: NaAlSi3O8 or CaAl2Si2O8.
Because both crystallize at similar temperatures and pressures according to Bowen's Reaction Series.
Because both crystallize at similar temperatures and pressures according to Bowen's Reaction Series.
Because both crystallize at similar temperatures and pressures according to Bowen's Reaction Series.
Bowens' Reaction Series measures the melting points of various silicate minerals, with the ones with highest melting points at the top. So as a completely moltenmagma containing all these minerals cools down, the first to crystallise are:ABOUT 1400 CELSIUSOlivinePyroxene (e.g. augite)Amphibole (e.g. hornblende)Biotite micaOrthoclase feldsparMuscovite micaSilica (e.g. quartz).ABOUT 800 CELSIUSNotice I've deliberately left out plagioclase feldspar because plagioclases of different composition crystallise out at different temperatures. Calcium-rich plagioclase crystallises out at about the same temperature as olivine (mineral 1), but sodium-rich plagioclase crystallises out about the same temperature as biotite mica (mineral 4). All plagioclase crystallises out at a higher temperature than orthoclase (mineral 5).So in answer to your question the first minerals to form as a magma cools are olivine and calcium-rich plagioclase feldspar, at around 1400 Celsius.
Labradorite ((Ca,Na)(Al,Si)4O8) is a Plagioclase Feldspar mineral. It has a ratio of Calcium to Sodium of between 50%Ca:50%Na and 70%Ca:30%Na and as such forms part of the Plagioclase solid solution series between the Calcium (Anorthite - CaAl2Si2O8) and Sodium (Albite - NaAlSi3O8) rich feldspars.
The plagioclase feldspar ranges from sodium-rich albite at low temperatures to calcium-rich anorthite at high temperatures. The difference in the mineral's appearance is due to a slight change in the chemical composition and a difference in growth pattern as the temperature changes. At intermediate temperatures, both calcium and sodium are incorporated in the crystal structure, building up alternating layers that allow light to refract or scatter, producing a range of colors.