7th National Opal Symposium “Unlocking Australia’s Opal Wealth” OPAL DOMES 7th National Opal Symposium Lightning Ridge 25-27 July 2011 David Horton
AUSTRALIAN OPAL MINING CENTRES
east Early west Late 80 90 110 120 130 CRETACEOUS 100 Kumbarilla Beds Bungil Formation Griman Ck Formation ** Surat Siltstone Doncaster Member ** Coreena Member Mackunda Formation ** These units host precious opal Cadna-Owie Formation Winton Formation ** Allaru Mudstone Toolebuc Formation Bulldog Shale ** Wallumbilla Formation Schematic cross-section showing opal-bearing geological units
24 Ma 60 Ma fresh host rocks silcrete chemically weathered host rocks 20 km Stage 2: Arid sub-tropical climate; lowering of alkaline water table during warping; remobilisation of silcrete; opalisation Stage 1: Wet temperate to sub-tropical climate; high acidic water table; chemical weathering of sediments; pedogenic silcrete 60 Ma 24 Ma later sediments opalisation
10 Ma - present Opal horizon Stage 3: Scarping 20 km Note: Vertical scale is highly exaggerated
AUSTRALIAN SEDIMENTARY OPAL – WHY IS AUSTRALIA UNIQUE? Australian Gemmologist, 21, 287-294 Published December 2002
Shuttle Radar Topography Mission Specially modified radar system that flew onboard the Space Shuttle Endeavour during an 11-day mission in February 2000
WINTON DOME Length: 90 km Width: 40 km
JUNDAH DOME Length: 145 km Width: 70 km
EROMANGA DOME Length: 145 km Width: 45 km
GRAWIN - GLENGARRY DOME LIGHTNING RIDGE DOME Length: 30 km Width: 30 km Length: 45 km Width: 45 km
ANDAMOOKA ?DOME Length: ?? km Width: 20 km
COOBER PEDY ?DOME Length: 100 km Width: +40km