pore-bearing fossils
pore-bearing rocks
pore-bearing structures
pore-bearing material
pore-bearing zone
pore-bearing layer
pore-bearing surface
pore-bearing formation
pore-bearing sediments
pore-bearing environment
the ancient rock contained numerous pore-bearing structures.
pore-bearing basalt is common in oceanic crust.
we analyzed the pore-bearing characteristics of the shale.
the reservoir's pore-bearing capacity significantly impacted production.
microscopic examination revealed extensive pore-bearing networks.
the cementation process reduced the pore-bearing space.
pore-bearing sediments accumulate in low-energy environments.
fluid flow is facilitated by the pore-bearing system.
the core samples showed a high degree of pore-bearing.
we used x-ray microtomography to image the pore-bearing features.
the presence of pore-bearing minerals influenced permeability.
pore-bearing fossils
pore-bearing rocks
pore-bearing structures
pore-bearing material
pore-bearing zone
pore-bearing layer
pore-bearing surface
pore-bearing formation
pore-bearing sediments
pore-bearing environment
the ancient rock contained numerous pore-bearing structures.
pore-bearing basalt is common in oceanic crust.
we analyzed the pore-bearing characteristics of the shale.
the reservoir's pore-bearing capacity significantly impacted production.
microscopic examination revealed extensive pore-bearing networks.
the cementation process reduced the pore-bearing space.
pore-bearing sediments accumulate in low-energy environments.
fluid flow is facilitated by the pore-bearing system.
the core samples showed a high degree of pore-bearing.
we used x-ray microtomography to image the pore-bearing features.
the presence of pore-bearing minerals influenced permeability.
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