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The fresh granites are hard rocks and the constituent minerals are mostly unaltered.
Calcium phosphate minerals are mostly known as bone substitutive materials due to their outstanding biocompatibility [10].
At the same time, since these minerals are mostly soluble minerals, they provide necessary materials for the later dissolution.
The titanium minerals are mostly anatase and rutile, and zirconium occurs in the mineral zircon.
These minerals are mostly found in China, the United States, Brazil, India, Sri Lanka and Australia Chinaa is by far the world leader in samarium mining and production.
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The curves show that the magnetic minerals were mostly saturated at ~300 mT.
This observation suggests that dissolution of carbonate and silicate minerals is mostly controlled by the groundwater chemistry in the study area.
For example, the effect of KAX as a collector was not significant in the initial period of flotation, suggesting that these minerals were mostly relying on their self-induced floatability due to involvement of a metastable form of sulphur.
The reddish-brown mineral is mostly composed of iron, silicon, zirconium, and titanium, but it also includes trace amounts of rare elements such as yttrium.
The light minerals, consisting mostly of quartz and feldspar, are the hardest and most resistant, whereas the dark minerals, which are mostly biotite mica and hornblende, are softer and weather out faster.
India's mineral resources are mostly found in areas inhabited by indigenous tribal populations.
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CEO of Professional Science Editing for Scientists @ prosciediting.com