C. J. MacLeod
0000-0002-0460-1626
Cardiff University
3 papers found
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Frictional Characteristics of Oceanic Transform Faults: Progressive Deformation and Alteration Controls Seismic Style
Extension parallel to the rift zone during segmented fault growth: application to the evolution of the NE Atlantic
Tectonic structure, evolution, and the nature of oceanic core complexes and their detachment fault zones (13°20′N and 13°30′N, Mid Atlantic Ridge)
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