作者: B.M. England , J. Ostwald
DOI: 10.1016/0169-1368(93)90002-G
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摘要: Abstract Base-metal sulphide deposits within the Tasman Fold Belt, New South Wales, Australia, contain a range of pyrite textural types which suggest evidence for transformation framboidal into atoll structures in variety and non-sulphide matrices. The writers that occurred while sulphidic sediments existed as colloids (gels), rather than by growth solid state. resulting conceptual model provides scheme explanation wide textures these deposits, also comparison with similar other related ore genesis.