Microcracks in rock refer to very small fractures or cracks that occur within the mineral structure of the rock. These microcracks can be on a microscopic scale, often not visible to the naked eye, and can significantly affect the physical and mechanical properties of the rock. They can result from various processes, including: 1. **Stress and Strain**: During tectonic activity or other geological processes, rocks may experience stress that exceeds their strength, leading to the formation of microcracks.
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