The long-uncertain crystal structure of ZnTe phase III, stable above 11 GPa, has been determined at 16 GPa using angle-dispersive powder-diffraction techniques with an image-plate area-detector and synchrotron radiation. The structure is orthorhombic, space group Cmcm, and is site ordered. This is a new high-pressure structure, which can be derived by distortion of the rocksalt structure. But the coordination is quite different from NaCl: There are only five nea est neighbors (all unlike) around each atom at {~}2.7 {} and then three next-nearest-neighbors (of which two are like atoms) at 3.0-3.4 {}.
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Nelmes et al. (1994) studied this question.
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