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The changes in joint load angle across abduction are shown. The data represent the means (SDs omitted for clarity) of joint load angle averaged across all levels of the geometric parameters (Abduction Main Effect) and for differing levels of glenosphere lateralization (0, 5, 10 mm), which produced a significant interaction with abduction whereby lateralization decreased load angle early during abduction but had no effect at the end of motion. SDs range from 10° to 13°.
