
%0 Journal Article
%A Cas, R. 
%T Geology of hill end trough Molong high: The merrions tuff ? its Genesis
%J Exploration Geophysics
%D 1976/04/01
%V 7
%N 1
%P 26-26
%K 
%R https://doi.org/10.1071/EG976026
%U https://www.publish.csiro.au/paper/EG976026 
%X The Early Devonian Merrions Tuff is a volcanogenic pulse up to 990 m thick, interrupting the more normal deposition of greywacke-slate sequences of the Hill End Trough. It is a distinctive, competent structural and stratigraphic datum for the Trough sequence (Fig. 1). Unfolding suggests that it may have had 1½ times to twice its present areal extent of approximately 1,850 km2 with the major shortening being in an east-west direction. 
