answ2. Simple visual inspection is always the first method.
For a tiny sample, a few mg of pure material, x-ray diffraction XRD.
If a small sample, (<1gm) x-ray fluorescence XRF in an electron microscope.
A larger sample <100 gm) x-ray fluorescence using a powder sample.
The above methods assume easy access to the equipments.
Thin section microscopy is a simple technique, but takes some time in sample preparation.
The determination would start with the visual inspection of the hand sample.
You will know what the origin of the rock is, and that gives clues to the cohort of minerals expected.
This would be followed by grinding the rock to sort out the particular minerals you are interested in.
No. a mineral is a compound of fixed chemical composition and of fixed crystal structure.
Coprolite is a valuable trace fossil for the archaeologist, but is NOT a mineral.A mineral must be of fixed composition, and have a fixed crystal shape.
Yes
scratching the mineral acrros a glass plate
whether the cost of mining will be less than the value of the mineral
the streak test
Mainly abrupt changes in mineral layers or the fossils in them.
There are different types of geologists that study oil exploration, mineral exploration and mineral mining. There are also engineering geologists.
The minerals are for the most part observable in a coarse grained igneous rock such as granite. If necessary, however, thin slices of rocks are made to be viewable under a microscope that could help identify trace minerals.
They basically cut or slice the granite apart exposing the "real" minerals inside.
The chemical composition must be determined by analytical methods.
They look at the mineral composition of the rocks. There are some minerals that can only form in the presence of oxygen.
Through testing of a sample to determine hardness, luster, streak, density, and chemical composition.
Each known mineral has a specific chemical composition.
by observing it,we properties of different minerals,so by observing it we are able to know which mineral is which
The color of a mineral sample is determined by its chemical composition
Several minerals are evaporites, and therefore, there is not just one mineral composition but a different one for each mineral.