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南极洲东部的沙克尔顿山(Shackleton Range)位于S80°—81°,东西向狭长分布,长约240km,宽50~70km,为活动的Ross造山带与稳定的南极洲东克拉通之间的过渡带。许多人把它视为一条具薄皮的冲断推覆构造的碰撞造山带。沙克尔山岩石包括含石榴子石和/或尖晶石橄榄岩和辉岩。石榴子?
The Shackleton Range in eastern Antarctica lies S80 ° -81 ° with an elongated east-west distribution with a length of 240 km and a width of 50-70 km. It is a transition between the active Ross orogenic belt and the stable East Coat of Antarctica band. Many see it as a thin-skinned thrust nappe or thrust belt. Shaker mountains include garnets and / or spinel peridotites and pyroxenites. Pomegranate?