“…We here develop them under the geometrical decompositions. First, by the use of (6), we re-decompose the independent displacements into the {x, y, z}directions o{x}(e)=[T({x})](e)o{x}(e) By employing me = 2e, rc= 2ec, y= 2eas the alternative shear components, we define deformation of (e) by ice)={eu, e, ecc, tnc, rcs, ran} (16) This deformation is in a one-to-one correspondence to shape g().…”