Topographic anomalies: Caurnamont (E. loop in Murray); Karoonda (NW centre); Moorlands (E. boundary); Coonalypn (dune distribution); Calburra (confuses old beach dunes with faults); Tintinara (south centre, NW structural trend); Keith (NW of town,...

Continuous reflection work over about 47 miles of total traverses was carried out south of Loxton. The individual lines are not interconnected and the correlation method is used for tie in. Shothole interval is 1/4 mile with straddle spread 1320 feet...

Comprises details of the operations, field acquisition, results and interpretation of the seismic and gravity surveys. The seismic survey aimed to extend results of earlier surveys and to search for anticlinal structures. The accompanying detailed...

Comprises details of the operations, field acquisition, results and interpretation of the seismic survey. One E-W traverse of 14 miles was carried out. Results indicate depths of potential sediments to about 4000 ft.

Summarises available data on history, economics and geology of oil exploration in Australia with particular reference to Hackathorn exploration in the Murray Basin.

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Microfloras in 8 drill core samples and 1 drill cuttings sample taken from Monash 1 have indicated and confirmed the presence of Palaeocene, Cretaceous and Permian sediments. Correlations in the Palaeocene are made with the type sequence in...

Beach Petroleum NL Monash 1 exploratory well located 5 miles north-west of Monash, and 20 miles south-west of Renmark, was drilled to a total depth of 3445 feet. The well penetrated a sequence of Tertiary, Cretaceous and Permian sedimentary rocks,...

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1 Second travelling time to basal reflection (approx. 4,000). Loxton electric log shows top of Cretaceous at 1,370. First strong reflection at 1,800 (corresponds to 15,000 f.p.s. refraction observed by BMR). If this is base of Cretaceous, minimum...

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There is no abstract created for this record

Structure E of Murray Bridge. River makes horseshoe curve at plunge of structure and outlines western closure. Vegetation and outlines of formation suggest closures to the east. (Plan without scale or title is presumably a structural contour plan of...

A short review of previous work is given and the difficulty is emphasised of interpreting deeper geological structure due to extensive alluvaeolian sediments. Monoclinal meridional escarpments are evident in the Morgan area. They are attributed to...

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