摘要
Structure and composition of the Uralian ophiolites reflect a large spectrum of geodynamic environment of their creation during Paleozoic time： from mid-ocean ridge, rift zone in continental margin, and suprasubduction spreading zone （SSZ） with resultant lherzolite or harzburgite ophiolite type （LOT and HOT）.
Structure and composition of the Uralian ophiolites reflect a large spectrum of geodynamic environment of their creation during Paleozoic time： from mid-ocean ridge, rift zone in continental margin, and suprasubduction spreading zone （SSZ） with resultant lherzolite or harzburgite ophiolite type （LOT and HOT）.
