Ja. Hudson et al., THE MEAN TRANSMISSION PROPERTIES OF A FAULT WITH IMPERFECT FACIAL CONTACT, Geophysical journal international, 129(3), 1997, pp. 720-726
A model of a fault where the two faces do not exactly conform is chara
cterized by a distribution of approximately circular contacts; elsewhe
re, the faces are stress-free. This contrasts with most earlier models
, which have assumed the contact geometry to be equivalent to a plane
distribution of approximately circular cracks. The contact regions in
the present model are taken to be sparsely distributed, and averaged i
nterface conditions are derived that are accurate to second order. At
lowest order they agree with established formulae for the normal stiff
ness of non-conforming surfaces. These averaged, or mean, conditions a
re expected to hold at wavelengths long compared with the radii and sp
acing distance of the contact points. Unsurprisingly, they are equival
ent to the continuity conditions for a thin elastic layer whose proper
ties are given here in terms of the parameters of the contact surface.