OBJECTIVE: To demonstrate the contribution of magnetic resonance imaging to the elucidation of mechanisms involved in "osteonecrosis-like syndrome of the medial tibial plateau". PATIENTS AND METHODS: A magnetic resonance study with sagittal and coronal sections was done in 13 patients (age range, 57-95 years) two weeks to four months into a painful syndrome meeting the definition of "osteonecrosis-like syndrome of the medial tibial plateau". Gadolinium injection was used in nine patients. Clinical symptoms resolved within a few weeks in all 13 cases. RESULTS: T1-weighted images without gadolinium showed diffuse low signal from the epiphysis (n = 12) containing an area of even lower signal seen either as a crescent-shaped subchondral image (n = 3/12) or as a linear image (n = 9/12). On postgadolinium images, the low signal was abolished except for a line of low signal parallel to the subchondral bone. T2-weighted images demonstrated diffuse high signal from the medial tibial plateau with persistence of the line of low signal (n = 8/12). CONCLUSION: Magnetic resonance imaging allows to analyze the anatomic lesion responsible for "osteonecrosis-like syndrome of the medial tibial plateau". Our magnetic resonance findings were similar to those seen in stress fractures at other sites.
OBJECTIVE: To demonstrate the contribution of magnetic resonance imaging to the elucidation of mechanisms involved in "osteonecrosis-like syndrome of the medial tibial plateau". PATIENTS AND METHODS: A magnetic resonance study with sagittal and coronal sections was done in 13 patients (age range, 57-95 years) two weeks to four months into a painful syndrome meeting the definition of "osteonecrosis-like syndrome of the medial tibial plateau". Gadolinium injection was used in nine patients. Clinical symptoms resolved within a few weeks in all 13 cases. RESULTS: T1-weighted images without gadolinium showed diffuse low signal from the epiphysis (n = 12) containing an area of even lower signal seen either as a crescent-shaped subchondral image (n = 3/12) or as a linear image (n = 9/12). On postgadolinium images, the low signal was abolished except for a line of low signal parallel to the subchondral bone. T2-weighted images demonstrated diffuse high signal from the medial tibial plateau with persistence of the line of low signal (n = 8/12). CONCLUSION: Magnetic resonance imaging allows to analyze the anatomic lesion responsible for "osteonecrosis-like syndrome of the medial tibial plateau". Our magnetic resonance findings were similar to those seen in stress fractures at other sites.