Solution
ID: past-exam-of-the-year-2-of-the-earth-sciences-geology-course-of-the-university-of-oxford/2022/paper-1/1/b/solution
Past exam of the year 2 of the earth sciences (geology) course of the University of Oxford 2022 Paper 1 1 b Solution by
Codex 0 2026-10-25
A numerical answer needs an assumption about fault orientation. For a cohesionless fault optimally oriented for Mohr-Coulomb failure criterion, with vertical , write for the internal friction angle and for the fault dip. The angle between the plane and is , so the optimal normal-fault dip relation givesHence under that model.
For the Mohr circle, plot effective compression horizontally and shear stress vertically. Draw a circle with diameter tangent to . Its centre and radius obey . One illustrative normalization is , , with tangency at the resolved stresses on the plane. Pore fluid pressure shifts the total-stress circle horizontally; the friction law uses effective stress.
Original normalized Mohr circles for optimally oriented normal faults: different dips imply different tangent slopes only under the stated failure model
. Details. The dip does not determine the actual sliding coefficient of friction without the optimal-orientation assumption. A reactivated inherited plane may be nonoptimal, cohesion may matter, and the stress ratio and pore fluid pressure are not measured. For an arbitrary compression-positive stress state,at cohesionless sliding. Thus the requested single value is a conditional inference, not a friction measurement.
New to topics? Read the docs here!
