Decrease in the Permeability of Microcracked and Macrocracked Granite at Elevated Pressure and Temperature
Abstract Pressure and temperature increase with depth, modifying the microstructure of crustal rocks. The opening or closing of micro‐ and macrocracks resulting from variations in the in‐situ conditions influences the permeability of crustal rocks. While confining pressure is known to close pre‐exis...
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| Main Authors: | , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Wiley
2025-04-01
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| Series: | Geophysical Research Letters |
| Online Access: | https://doi.org/10.1029/2024GL112970 |
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