
%0 Journal Article
%A Russell, H.Y. 
%T Geology of hill end trough Molong high: The geometry of the Gowan Green Overfold and its relationship to the regional deformational history
%J Exploration Geophysics
%D 1976/04/01
%V 7
%N 1
%P 22-25
%K 
%R https://doi.org/10.1071/EG976022B
%U https://www.publish.csiro.au/paper/EG976022B 
%X The Gowan Green Overfold southwest of Mumbil (Fig. 1) , is a downward-facing antiformal syncline (Fig. 2) which is anomalous in the regional upward-facing structures of the Molong anticlinorial zone. Extending north from the overfold for 20 km is a discontinuous belt of overturned beds offset by faults (Figs. 1 and 3; Russel, 1975). The overfold and the overturned beds can be interpreted as a single coherent structure (Fig. 4) with an original strike length of 20 km and a width of 11 km. 
