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南秦岭早古生代地幔性质:来自超镁铁质、镁铁质岩脉及火山岩的Sr-Nd-Pb同位素证据
  • 期刊名称：2007. 中国科学(D辑), 37: 857-865
  • 时间：0
  • 相关项目：大陆岩石圈深部再循环与华北克拉通及其邻区中新生代演化
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大陆岩石圈深部再循环与华北克拉通及其邻区中新生代演化
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