Lithic fragments of plutonic rocks are more rare, while fragments of volcanic rocks are more common. Feldspar is much softer and unstable at the surface, subject to chemical decomposition. In terms of mineralogical maturity, a rock is immature when it contains a mix of stable and unstable minerals, and is mature when it contains only stable minerals.
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The high portion of extremely stable materials and the well-bedded texture indicate supermature composition and texture. The result is increased sorting during transportation:
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