Publication details for Prof Ken McCaffreyFarangitakis, G.P., Sokoutis, D., McCaffrey, K.J.W., Willingshofer, E., Kalnins, L.M., Phethean, J.J.J., van Hunen, J. & van Steen, V. (2019). Analogue modeling of plate rotation effects in transform margins and rift-transform intersections. Tectonics 38(3): 823-841.
- Publication type: Journal Article
- ISSN/ISBN: 1944-9194
- DOI: 10.1029/2018TC005261
- Further publication details on publisher web site
- Durham Research Online (DRO) - may include full text
Author(s) from Durham
Transform margins are first‐order tectonic features that accommodate oceanic spreading. Uncertainties remain about their evolution, genetic relationship to oceanic spreading, and general structural character. When the relative motion of the plates changes during the margin evolution, further structural complexity is added. This work investigates the evolution of transform margins, and associated rift‐transform intersections, using an analogue modelling approach that simulates changing plate motions. We investigate the effects of different crustal rheologies by using either a) a two‐layer brittle‐ductile configuration to simulate upper and lower continental crust, or b) a single layer brittle configuration to simulate oceanic crust. The modeled rifting is initially orthogonal, followed by an imposed plate vector change of 7o that results in oblique rifting and plate overlap (transpression) or underlap (transtension) along each transform margin. This oblique deformation reactivates and overprints earlier orthogonal structures, and is representative of natural examples. We find that: a) a transtensional shift in the plate direction produces a large strike‐slip principal displacement zone, accompanied by en‐echelon oblique‐normal faults that accommodate the horizontal displacement until the new plate motion vector is stabilized, while b) a transpressional shift produces compressional structures such as thrust fronts in a triangular zone in the area of overlap. These observations are in good agreement with natural examples from the Gulf of California (transtensional) and Tanzania Coastal Basin (transpressional) shear margins, and illustrate that when these deformation patterns are present, a component of plate vector change should be considered in the evolution of transform margins.