Some researchers believe that copper and gold are derived from sulfides in the mantle, which are decomposed for interaction with Fe3+-rich fluids or melts derived from the subducted oceanic slab.

 
  • 斑巖銅礦伴生金屬組分的含量受許多因素控制,其中包括巖漿源區地幔演化、火成巖巖石類(lèi)型、巖漿侵位深度和成礦溫度等多個(gè)方面。
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