Fracture Gradient Above Overburden
/Does anyone know of any published material on Barents Sea fracture gradients which explain why sometimes the fracture gradient is equal to or greater than the overburden gradient?
Does anyone know of any published material on Barents Sea fracture gradients which explain why sometimes the fracture gradient is equal to or greater than the overburden gradient?
I have assumed sediments density at the earth surface in a case in order to calculate overburden stress and gradient and now i have to extrapolate it to the first measurement point on the density log. How this extrapolation will be carried out?
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