Kinematics of Footwall Exhumation at Oceanic Detachment faults: Solid?Block Rotation and Apparent Unbending

Mylonitic Deformation at the Kane Oceanic Core Complex: Implications for the Rheological Behavior of Oceanic Detachment Faults

Recognizing detachment-mode seafloor spreading in the deep geological past

Large-offset oceanic detachment faults are a characteristic of slow- and ultraslow-spreading ridges, leading to the formation of oceanic core complexes (OCCs) that expose upper mantle and lower crustal rocks on the seafloor. The lithospheric extension accommodated by these structures is now recognized as a fundamentally distinct "detachment-mode" of seafloor spreading compared to classical magm...

Oceanic- and continental-type metamorphic terranes: Occurrence and exhumation mechanisms

Flexural Rotation of Normal Faults

A conceptual model is proposed for the generation of low-angle normal faults in Metamorphic Core Complexes. The model is based on three assumptions: (1) the isostatic response to normal fault motion is of regional extent; (2) when a fault segment is significantly rotated from the optimum angle of slip, relative to the crustal stress field, it is replaced by a new planar fault oriented in the op...

Evidence for weak oceanic transform faults

[1] We present the results of a series of 3-D boundary element calculations to investigate the effects of oceanic transform faults on stress state and fault development at adjacent mid-ocean ridge spreading centers. We find that the time-averaged strength of transform faults is low, and that on time scales longer than a typical earthquake cycle transform faults behave as zones of significant we...