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股骨转子间骨折的病理解剖和病理力学:一项 MRI 研究。

Pathoanatomy and pathomechanics of pertrochanteric fractures - an MRI study.

出版信息

Rozhl Chir. 2024;103(8):299-304. doi: 10.48095/ccrvch2024299.

Abstract

BACKGROUND AND STUDY AIMS

Magnetic resonance imaging (MRI) has been used for more than 20 years in the region of the proximal femur to diagnose occult, or incomplete, fractures of the femoral neck and the trochanteric segment. MRI has also potential to contribute to the understanding of the pathogenesis and pathoanatomy of trochanteric fractures.

METHODS

The group including 13 patients was examined by MRI for a suspected, or incomplete, fracture of the trochanteric segment within 24 hours post-injury. In all cases, this was the first injury to the hip joint, with the other hip joint remaining intact.

RESULTS

The coronal scans showed a marked fracture line which, in the region of the intertrochanteric line, extended from the base of the greater trochanter (GT) medially and distally and involved the medial cortex. This inclination, however, was gradually changing posteriorwards and close before the posterior cortex. The fracture line was passing vertically along the lateral trochanteric wall as far as the level of the lesser trochanter (LT). Then the fracture line changed its course and ran horizontally to the cortex of the LT. Sagittal scans showed clearly the primary fracture line originating in the greater trochanter, extending medially and starting to separate the posterior cortex.

CONCLUSION

Analysis of MRI findings has documented that the primary fracture line in pertrochanteric fractures originates in the GT and extends distally, medially and anteriorly towards the anterior cortex, the intertrochanteric line and the LT. Thus, the GT presents a rather vulnerable site and is always broken into more fragments than shown by a radiograph.

摘要

背景与研究目的

磁共振成像(MRI)在股骨近端区域已使用超过 20 年,用于诊断股骨颈和转子间段的隐匿性或不完整骨折。MRI 还有助于理解转子间骨折的发病机制和病理解剖。

方法

该组包括 13 名患者,在受伤后 24 小时内因疑似或不完整的转子间段骨折接受 MRI 检查。在所有情况下,这都是髋关节的首次损伤,而另一侧髋关节保持完整。

结果

冠状扫描显示明显的骨折线,在转子间线区域,从大转子(GT)的内侧和远端基底向内侧和远端延伸,并累及内侧皮质。然而,这种倾斜度逐渐向后变化,并在接近后皮质之前发生变化。骨折线沿外侧转子壁垂直延伸至小转子(LT)水平。然后骨折线改变其方向,向 LT 的皮质水平横向延伸。矢状扫描清楚地显示出起源于 GT 的原发性骨折线,向内侧延伸并开始分离后皮质。

结论

MRI 检查结果分析表明,转子间骨折的原发性骨折线起源于 GT,并向远端、内侧和前方向前皮质、转子间线和 LT 延伸。因此,GT 呈现出一个相当脆弱的部位,总是比 X 线片显示的骨折线更易断裂成更多的碎片。

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