Abstract - Overlapping opposed-dipping normal faults can have complementary displacement distributions, indicating
transfer of displacement between them in the same way as at relay zones between faults with the same dip
direction. We constrain the mechanism by which displacement is transferred between opposed-dipping faults by
examining the geometries of faulted horizons and fault throw distributions at these conjugate relay zones.
Structure contour maps of horizons offset by overlapping opposed-dipping faults from different extensional
settings display a consistent pattern. Above the line of intersection between the conjugate faults the deformed
horizon is flat between converging faults and displacement transfer is reflected in changes in footwall elevation.
Below the line of fault intersection the mutual footwall is flat and elevation changes occur in the hanging walls of
the divergent faults. These elevation changes can be explained as a simple superposition of the deformation
fields of two faults that have retarded lateral propagation due to the presence of the other synchronous fault,
irrespective of whether the two faults actually intersect. The observed patterns of horizon elevation strongly
resemble those seen at boundaries between adjacent basin-scale half-graben of opposed polarity.
Journal of Structural Geology , doi: https://doi.org/10.1016/j.jsg.2018.11.007, 2019.