Audley-Charles (1968) mapped the Cablac
Mountain as massive shallow-water Cablac Formation and identified as Lower
Miocene in age. and after few years, Carter et al (1976) and Charlton (2002) also identified
following Audley-Charles’s interpretation.
Cablac
Mountain Range is formed a massif limestone. It characterizes a thrust
sheet stuck that dominated by Triassic to Paleogene limestone belong to the
Gondwana and Australian-Margin Megasequence (Haig et al, 2007; Haig &
McCartain, 2007).
The Cablac Mountain is composed of
breccia as a rock fragment and clasts contain peloid and
oolitic limestone of
the Upper Triassic – Lower Jurassic (Haig et al, 2007).
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