O'Keeffe D, Nicholson D A, Driscoll P A, Marsh D
Royal Albert and Edward Infirmary, Wigan.
BMJ. 1994 Jan 29;308(6924):331-6. doi: 10.1136/bmj.308.6924.331.
The os trigonum is a common normal variant of the talus and is due to a separate ossification centre arising from the posterior tubercle. The appearance may resemble an old ununited fracture fragment. However, it is triangular, well corticated, in a classic location, and usually bilateral, which enables it to be distinguished from a fracture. Transverse, sclerotic, linear lines located at the metaphysis of growing long bones are due to short periods of growth arrest and have no clinical importance (fig 5). They may be confused with compression fractures, but again these lines are usually bilateral. Fibrous cortical defects are the most commonly seen benign lesions of long bones and are usually identified incidentally in radiographs taken for another reason. The defect is limited to the cortex, commonly found at the metaphysis, but may be located in the diaphysis as the bone grows. The lesion is well corticated (sclerotic margins) and usually does not produce signs or symptoms.
距骨三角骨是距骨常见的正常变异,由后结节处独立的骨化中心形成。其表现可能类似陈旧性未愈合的骨折碎片。然而,它呈三角形,皮质良好,位置典型,且通常为双侧性,这使其能够与骨折相鉴别。位于生长中长骨干骺端的横向、硬化、线性线是由于短期生长停滞所致,无临床意义(图5)。它们可能与压缩性骨折相混淆,但同样这些线通常也是双侧性的。纤维性皮质缺损是长骨最常见的良性病变,通常在因其他原因拍摄的X线片中偶然发现。缺损局限于皮质,常见于干骺端,但随着骨骼生长也可能位于骨干。病变皮质良好(边缘硬化),通常不产生体征或症状。