Jana C. Schierjott coauthored three-dimensional ridge-transform models that favour excess lithospheric tension from transform fault shear as an explanation of asymmetric detachment fault formation.[ref]
How transform fault shear influences where detachment faults form near mid-ocean ridges by Jana C. Schierjott and others. Abstract: three-dimensional models and the stress mechanism for inside-corner detachment faulting
New to topics? Read the docs here!