Since it was developed by Cox [Cox, H.L., 1952. The elasticity and str
ength of paper and other fibrous materials. Br. J. Appl. Phys. 3, 72-7
9.], the shear-lag model (SLM) or fiber-loading theory has been widely
used by material scientists and structural geologists as a powerful a
nalytical method for analyzing mechanical interactions between hard an
d soft phases (layers) in composites and two-phase rocks. We found tha
t several approximations in previous mechanical derivations of the mod
el can be improved in terms of mechanical equilibrium and boundary con
ditions. Our refinements make the model more rigorous and elaborate. A
pplications of the improved model include: (1) prediction of the axial
tensile stress in strong inclusions embedded in a continuous weak mat
rix, and consequently interpretation of extension fracture boudinage;
(2) modeling of the distribution of shear stresses in the weak matrix
surrounding the strong inclusions and, accordingly, interpretation of
the variations of dislocation density and of recrystallized grain size
in composites and polyphase rocks; and (3) prediction of mechanical p
roperties of industrial composites and two-phase rocks. The analytical
results of the improved model agree approximately with those obtained
from both experimental investigations and numerical calculations.