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When burial pressures and temperatures get too great, the rocks melt completely, becoming new igneous rocks.To fully understand Gentry's hypothesis a basic background in geology, mineralogy, and radiation physics is helpful.Both types of igneous rocks comprise a mixture of different minerals.As igneous rocks cool, mineral crystals form following a specific sequence.Metamorphic rocks represent alterations of precursor sedimentary, igneous, or other metamorphic rocks.Through the cycles of burial, folding, faulting, and subduction of crustal plates, rocks get pushed and dragged down to depths where - under heat and pressure - changes take place.
Other plutonic rocks have less quartz and potassium, and different ratios of calcium and sodium feldspar minerals.In metamorphic rocks, new minerals form that are more stable at higher temperatures and pressures.Sometimes the minerals segregate into distinct bands.True granites are relative latecomers on the geologic scene as they required a number of recycles of crustal material to differentiate and concentrate potassium.In an earlier edition of , Lorence Collins (March/April, 1999) provided a thorough overview of the origin and nature of granitic rocks.
These haloes were considered to be the result of damage to the crystal structure of the host minerals caused by high energy alpha particles.
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