
TY  - JOUR
A1  - Cas, R. 
T1  - Geology of hill end trough Molong high: The merrions tuff ? its Genesis
JF  - Exploration Geophysics
JO  - Explor. Geophys.
Y1  - 1976
VL  - 7
IS  - 1
SP  - 26
EP  - 26
KW  - 
UR  - https://doi.org/10.1071/EG976026 
N2  - 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. 
ER  -

