The crystal and magnetic structures of TbBaCo1.9Fe0.1O5.43 have been studied by neutron diffraction and magnetization measurements. It is shown that spontaneous magnetization develops at TN 305 K and decreases abruptly below 200 K. The crystal structure is described in the space group Pmmm, on a 2ap ap 2ap unit cell. It was shown that the extra oxygen vacancies are located mainly in the pyramidal sublattice, thus making tetrahedra. Magnetic structure in the high temperature magnetic phase consists of ferromagnetic and G type antiferromagnetic components, while in the low temperature phase only the G type component exists with a 2ap 2ap 2ap magnetic unit cell. The ferromagnetic component results from canting magnetic moments of Co3 ions which were found to be predominantly in the high spin state in pyramids. The refined values of the magnetic moments of the Co3 ions in the octahedra indicate a mixed high low spin state. It is assumed that non collinear magnetic structure results from a concurrence between positive and negative exchange interactions as well as magnetocrystalline anisotropy in the pyramidal sublattice. Using the concept of non collinear magnetic structure, the giant anisotropic magnetoresistive effect in layered cobaltites is explaine
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