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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.
Bowen's reaction series
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Hornblende is a complex inosilicate series of minerals (ferrohornblende - magnesiohornblende).[3] It is not a recognized mineral in its own right, but the name is used as a general or field term, to refer to a dark amphibole.
Drama high series
Higher silica contents will be in the igneous rocks that form with lower temps. Ones that form earlier in the series like olivine have lower percentages of silica.
Olivine... if you can find on the internet the "Bowens Reaction Series" paper, it will tell you that Olivine is the first to crystallize
Minerals form in igneous rock as magma or lava cools. The minerals will form from the available chemicals in the magma as their crystallization temperature is reached. The sequence of mineral crystal formation from magma is described in the Bowen's Reaction Series. Metamorphic rock minerals are aligned, altered, or recrystallized from existing rock minerals due to the effects of heat and/or pressure.
Minerals form in igneous rock as magma or lava cools. The minerals will form from the available chemicals in the magma as their crystallization temperature is reached. The sequence of mineral crystal formation from magma is described in the Bowen's Reaction Series. Metamorphic rock minerals are aligned, altered, or recrystallized from existing rock minerals due to the effects of heat and/or pressure.
The purpose of Bowen's Reaction Series is to visually represent the conditions under which different igneous rocks form in an organized way that is easy for the viewer to understand. Bowen's Reaction Series is important to geologists because it helps them understand the order in which specific minerals were created.
Various minerals from magma.
FELDSPARS!!!!
Gabbro is mafic intrusive igneous rock and contains olivine, pyroxene, plagioclase and amphibole. These minerals are unstable at low pressure temperature conditions. In contrast, granite is felsic intrusive igneous rock and contains high amounts of quartz and orthoclase. Stability of minerals are increasing top to bottom in Bowen's Reaction Series.
Bowen's reaction series shows that one homogeneous body of magma can form more than kind of igneous rock. At its lowest temperature, it can form felsic igneous rock like Potassium Feldspar, muscovite, quartz or emerald. At its highest temperature, it can form mafic igneous rocks like olivine.
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.