Mineral Environments Flashcards
Genisis
Primary crystallization, properties are explained by the conditions of formation
sources crystallizing magma
Aqueous 1
dehydrating sedimentary rocks
Aqueous 1
mantle degassing
aqueous 1
migrated meteoric and seawater
aqueous 1
heated solution transport and precipitate along path where minerals like calcite can accumulate
aqueous 1
hydrothermal endogenic
aqueous 1
surface solutions or brines (exogenic)
aqueous 2
ground, karst and soil water
aqueous 2
what type of sea do we have?
Aragonite sea that is high in magnesium
Evaporite minerals
halite, gypsum
Gas and fluid minerals
Hematite and sulfur
volcanic gas vents (fumaroles)
gas and fluids
skarns and metamorphism of limestone
gas and fluids
Ocean floor silt, clay minerals
Colloidal solutions
Al, Fe, Mn-HYdroxides
Colloidal solutions
amorphous opal
colloidal solutions
Silica tetrahedron present as dissolved clusters
magma
silicate liquids with silica tetrahedron chains
magma
Parameters of magma
Temp and pressure, partial pressures of H2O and O2
< 45% SiO2
Ultramafic
About 50% SiO2
Mafic
about 60% SiO2
intermediate
> 65% SiO2
felsic
Polymorphic transitions
Solid systems
Prophyroblasts: garnet in a schist or gneiss
solid systems
replacement processes
solid systems
Mineral crystallization types
Free space, metasomatism, recrystallization
Freely grow in gas, melt, solution
free space
euhedral crystal habits
free space
sulfur in volcanic gas, amethyst in hydrothermal solutions, porphyritic feldspars in magma
free space
chemical composition is changed due to liquid flow
metasomatism
simultaneous capillary dissolution and crystallization where a mineral replaces another
metasomatism
Magmatic mineral deposits (exo vs. endo)
endogenic
metamorphic mineral deposits (endo vs. exo)
endogenic
Supergene mineral deposits (exo vs. endo)
exogenic
sedimentary mineral deposit (exo vs. endo)
exogenic