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A narrow vertical or slanted opening in solid
rocks, filled with fluid and coarse sediments.

The term "narrow" means that elongation of the fracture is much longer than its transversal size, called fracture width  or fracture aperture.

The contact area between the fracture opening and the rocks is called fracture plane.

All fractures are normally divided into two groups:

Natural fracturesInduced Hydraulic Fractures

which are naturally created,
as a result of sedimentation and tectonic activities

which are created as a result of anthropogenic invasion, called Hydraulic Fracturing


The difference between the origin of Natural fractures and Induced Hydraulic Fractures translates to the difference in fracture geometry and its dynamic behaviour.

This is why the two categories of fractures are normally covered by different  Subsurface E&P Disciplines.

See Also


Geology / Rocks 

Natural fracture ]

Petroleum Industry / Upstream / Well / Well-Reservoir Contact (WRC)  / Hydraulic Fracture ]

Production / Subsurface Production / Well & Reservoir Management (WRM) / Well stimulation /  Hydraulic Fracturing ]

Hydraulic Fracture @model ]

Infinite conductivity fracture ] [ Finite conductivity fracture ]

Fracture conductivity (FC) ][ Dimensionless fracture conductivity (FCD) ]

Fracture half-length (Xf) ][ Fracture width (kf) ][ Fracture volume (Vf) ][ Fracture pore volume (Vef) ][ Fracture permeability (kf) ][ Fracture width (wf) ][ Fracture height (hf) ]




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