packing proximity
Quick Summary
In geology, "packing proximity" refers to the number of grain-to-grain contacts within a sedimentary rock. This is a component of a rock's fabric, which influences its porosity and permeability—its ability to hold and transmit fluids like oil and water. Packing is determined by factors such as grain size, shape, and the degree of compaction, and it affects the rock's overall density. Analyzing thin sections under a microscope helps geologists understand packing density and proximity. This concept is distinct from mathematical packing problems, which involve arranging figures within a given space.12
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