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Ground mass

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(Geol.) the fine-grained or glassy base of a rock, in which distinct crystals of its constituents are embedded.

See also: ground



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Cool storage for the wine is created by effective exploitation of thermal ground mass, and underground water is used to aid night-time heat exchange.
Silicification and propylization are the most common and pervasive alterations observed in the ground mass of the volcanic rocks.
 
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