The Silurian System of the northern Molong Rise has been re-examined where well displayed between Neurea and Mumbil. The Mumbil Group, forming the upper part of the sequence, comprises the dolomitic Narragal Limestone and the overlying Barnby Hills Shale. The succession beneath the Narragal ...
Late Silurian pentameride brachio- pods from Yass and Molong, New South Wales. Alcheringa 29, 205-228.Strusz, D.L. (2005). Late Silurian pentameride brachiopods from Yass and Molong, New South Wales. Alcheringa 29, 205-228.Strusz, D.L., 2005: Late Silurian pentameride brachio- ...
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 ...
Structural evolution and granite chronology of the central Molong Zone, Eastern Lachlan Fold Belt, Australia. Austr. J. Earth Sci. 52, 79-99.LENNOX P. G., TRZEBSKI R., ARMSTRONG R. & SIEBEL W. 2005. Structural evolution and granite chronology of the central Molong Zone, Eastern Lachlan ...
Sheet lava and flow-foot breccia record the effusion of lava in air whereas the subaqueous breccias arenites and lutites form an encircling sedimentary apron. The sedimentary apron volumetrically contains more material than the lava pile.doi:10.1071/EG976022aDennis J. MortonExploration Geophysics...
Molong Volcanic BeltNew South WalesDiverse shallow water assemblages dominated by brachiopods, molluscs, sponges and stromatoporoids, and a tabulate coral, in the Wahringa Limestone Member (Darriwilian-Gisbornian), and Yuranigh Limestone Member (Gisbornian, or early Late Ordovician) of the ...
For the northern Molong Rise, three Silurian longitudinal palaeogeographic units are postulated: essentially a shallow basin flanked by two acid igneous complexes (Figs. 1, 2). At the time of maximal carbonate development, a central Narragal Lagoon passed westwards onto a shelf edge characterised ...
It is a distinctive, competent structural and stratigraphic datum for the Trough sequence (Fig. 1). Unfolding suggests that it may have had 1 times to twice its present areal extent of approximately 1,850 km2 with the major shortening being in an east-west direction....
Geology of hill end trough Molong high: multiple deformation associated with the wiagdon fault zone along the turon river, near sofalaIn an area (3 ? 4 km) immediately west of the Wiagdon Fault Zone near Sofala, four crenulation cleavages with associated folds postdate the regional slaty ...
Geology of hill end trough Molong high: The stratigraphy and structure of the Upper Devonian rocks between Mt. Horrible and the Razorback Road, and the implications for the tectonics of NSWRecent mapping of Upper Devonian ? ?Early Carboniferous rocks north of Mt. Horrible reveals a coarsening-...