造山带富集型上地幔形成的构造环境是：洋壳从扩张脊向两侧运移并最终拼入造山带这段时间内。

Tectonic environment of formation of enriched upper mantle is oceanic crust displacement from the oceanic mid-ridge to the orogenic zone.

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所有患者均使用改良Judet入路，三角肌后部自肩胛嵴切下向头侧掀起直到肩胛骨外侧缘。

A modified Judet approach was used in all patients. The posterior deltoid was incised off the scapular spine cephalad reaching the lateral scapular border.

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