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A pyroxenite is an ultramafic rock composed mainly by clinopyroxene, orthopyroxene and in minor amount, olivine (less than 40%). Depending of the modal mineralogy, the can be subclassified as orthopyroxenite (90% or more of opx), clinopyroxenite (90% or more than cpx), websterite (10% or less of olivine) and olivine-websterite (10-40% of olivine). Because the composition of these mineral phases is highly variable, pyroxenites have a broad range of compositions, however, they usually tend to have more SiO2 than peridotites.
Quartz consists of silicon and oxygen (2 times as many oxygen atoms than silicon atoms).
1) The covalent bonds in quartz are much stronger than the ionic bonds in halite. 2) The stronger bonds of quartz make it harder than halite. 3) You can easily scratch halite with a steel knife ,while you cannot scratch quartz.
No, oil does not pour faster than water
Glass will absorb radiation below 320nm whereas quartz will allow transmission of the UV wavelengths. So use glass cuvettes for wavelengths in the visible range from 380nm to 780nm and quartz cuvettes for wavelengths below 380nm.
Olivine would weather faster than quartz
Following Goldich Dissolution Series (Or going backwards by Bowen's Reaction Series), olivine weathers before Quartz. Quartz has a framework silicate structure and olivine has a isolated silicate structure.
no it doesnt
this indicates that gold is much more dense than quartz and olivine
The denser the faster. ie: it will travel faster through quartz than sandstone.
Basalts are higher in plagioclase feldspar, pyroxene, olivine and iron content than granites, which are typically higher in quartz, alkali feldspars, and micas.
Quartz is a mineral that is resistant to weathering due to its chemistry and crystalline structure. Granite will weather faster than quartzite because granite is only partially quartz in composition.
Olivine does not contain Gabbro. Gabbro can contain olivine. Usually no more than a few percent.
A pyroxenite is an ultramafic rock composed mainly by clinopyroxene, orthopyroxene and in minor amount, olivine (less than 40%). Depending of the modal mineralogy, the can be subclassified as orthopyroxenite (90% or more of opx), clinopyroxenite (90% or more than cpx), websterite (10% or less of olivine) and olivine-websterite (10-40% of olivine). Because the composition of these mineral phases is highly variable, pyroxenites have a broad range of compositions, however, they usually tend to have more SiO2 than peridotites.
There are many sorts of igneous rocks. Granite is made of quarts, feldspar, and mica, while basalts are made of less than 20% quartz and less than 10% feldspar and the rest made up of pyroxenes and olivine.
The mineral assemblage of Rhyolite is usually quartz, alkali feldspar and plagioclase (in a ratio > 1:2) and biotiteand hornblende are common accessory minerals. More importantly quartz has got to comprise more than 69% of the rock.
That's like asking whether a car is faster than a Ford, or whether an animalcan outrun a horse.Sunlight is light, and it travels at the speed of that which it is.