Conference Proceedings
Young Professionals' Conference, Mt Isa, October 1995
Conference Proceedings
Young Professionals' Conference, Mt Isa, October 1995
Golden Plateau and Adjacent Deposits Structural Controls on Mineralisation
Structural Controls Interpretation of regional aeromagnetics, radiometrics and satellite image data has identified three structural
domains (fig 2): The Fairyland Domain: a general N - S structural trend.
The Cracow Domain: a general NW - SE structural trend.
The Bald Mountain Domain: a general N- S structural trend. Known mineralisation is confined to the Cracow Domain in which there occurs two major NW - SE trending fault
zones. The Cracow Fault Zone (CFZ) and the Immy Creek Fault Zone (ICFZ). Enhanced detail of the CFZ (fig 3)
shows three main structural trends within it: NW-SE structures which include the mineralised White Hope South fault zone and the Golden Mile fault
zone. NE-SW structures which have an influence on mineralisation in the Orange Creek, Fernyside and Golden
Plateau areas. N-S structures comprising several major structural zones.
domains (fig 2): The Fairyland Domain: a general N - S structural trend.
The Cracow Domain: a general NW - SE structural trend.
The Bald Mountain Domain: a general N- S structural trend. Known mineralisation is confined to the Cracow Domain in which there occurs two major NW - SE trending fault
zones. The Cracow Fault Zone (CFZ) and the Immy Creek Fault Zone (ICFZ). Enhanced detail of the CFZ (fig 3)
shows three main structural trends within it: NW-SE structures which include the mineralised White Hope South fault zone and the Golden Mile fault
zone. NE-SW structures which have an influence on mineralisation in the Orange Creek, Fernyside and Golden
Plateau areas. N-S structures comprising several major structural zones.
Contributor(s):
S R Law
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- Published: 1995
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