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Publikováno v:
Economic Geology. 117:1791-1807
The Ni-Cu-platinum group element (PGE) sulfide mineralization in the 1.85 Ga Sudbury impact structure occurs in two discrete environments: (1) mineralization along or near the basal contact, including disseminated to semimassive mineralization in an
Publikováno v:
Journal of Petrology. 61
The c. 1·85 Ga Sudbury Igneous Complex (SIC) is the igneous remnant of one of the oldest, largest and best-preserved impact structures on Earth and contains some of the world’s largest magmatic Ni–Cu–PGE sulfide deposits. Most of the mineraliz
Publikováno v:
Geology. 46:443-446
Autor:
J. Paul Golightly
Publikováno v:
Zeitschrift für Kristallographie. 130:310-313