All rocks in the earth's crust are fractured to some extent. Fractures form in response to stress. The origin of stress can be lithostatic (arising from the weight of the earth's crust), high fluid ...
Previous chapters have addressed fracture geometry, physical and geomechanical properties of single fractures, fracture detection, and the interpretation of hydraulic and tracer tests. All of these ...
Some results have been hidden because they may be inaccessible to you
Show inaccessible results