A higher-order shear deformation theory is presented for vibration ana
lysis of thick, doubly curved shallow shells. An orthogonal curvilinea
r coordinate system is employed to arrive at the strain components. A
third-order displacement field in transverse coordinate is adopted. Th
ough no transverse normal stress is assumed, the theory accounts for c
ubic distribution of the transverse shear strains through the shell th
ickness in contrast with existing parabolic shear distribution. The un
symmetric shear distribution is a physical consequence of the presence
of shell curvatures where the stress and strain of a point above the
mid-surface are different from its counterpart below the mid-surface.
Imposing the vanishing of transverse shear strains on top and bottom s
urfaces, the rotation field is reduced from a six-degree to a two-degr
ee system. The discrepancy between the existing and the present theori
es is highlighted.