-
RB 51/00121 Chowilla Dam site, River Murray. Stratigraphy and micropalaeontology.
Five stratigraphic bores at Chowilla Dam Site intersected Post-Tertiary river sands and silts, equivalents of the Loxton Sands grading downwards into highly glauconitic siltstone of the Bookpurnong Beds and, in two bores, Shelly glauconitic marls,...-
Document
Published: 01 Jan 1960
-
RB 55/00065 Woodside (Lakes Entrance) Oil Co. NL. Bundy 1, NSW. Palaeontological report.
Bundy No. 1 well near the eastern margin of the Murray Basin intersected a sequence 1340 feet thick of non marine lignitic sands and silts of Tertiary age. The oldest are Eocene and the youngest probably Pliocene. The well bottomed in granite at 1340...-
Document
Published: 01 Jan 1962
-
RB 55/00066 Woodside (Lakes Entrance) Oil Co. NL. Balranald 1, NSW. Palaeontological report.
There is no abstract created for this record-
Document
Published: 01 Jan 1962
-
RB 56/00032 Correlation of the Tertiary rocks of South Australia.
Marine and non-marine sediments of Paleocene to Pliocene age are represented in South Australia, although parts of the sequence are known only from subsurface sections. The Tertiary sequence is most complete in the Murray Basin, where Hantkenina...-
Document
Published: 01 Jan 1963
-
RB 49/00102 Stratigraphy of the Murray Basin in South Australia.
The Murray Basin is an area of Mesozoic and Tertiary sedimentation divided into two main units the Murray Basin proper separated by structural highs, the Padthaway “Horst”, from the Gambier Sunklands. Knowledge of the Mesozoic in the Murray Basin...-
Document
Published: 05 Oct 1959
-
RB 44/00088 Fauna of the Bookpurnong Beds outcropping 2.5 miles west of Loxton.
The report covers palaeontological examinations of seven samples collected by an officer of Frome Broken Hill Company Limited from the only known outcrop of the Bookpurnong Beds, 2½ miles west of Loxton. The fauna indicates worn shallow-water...-
Document
Published: 01 Jan 1957
-
RB 42/00075 Advance note on younger Tertiary sediments in the Murray Basin between Loxton and Morgan.
Drainage problems in the Loxton Irrigation area have called for a clearer understanding of the stratigraphy of the area between Loxton and Morgan. Apart from Quaternary sediments, the sequence is normal marine, in which five formations may be...-
Document
Published: 01 Jan 1956
-
RB 47/00028 Probable stratigraphy of water bores at Murrayville, Victoria.
Water Bores in the Murrayville area mostly intersect only the late Tertiary sequence of the Loxton Sands and Bookpurnong beds. Mid Tertiary limestones are encountered only below depths of about 300 feet. A similar sequence, reported to carry large...-
Document
Published: 01 Jan 1958
-
RB 47/00039 Report on Pata Limestone and Bookpurnong Beds standard subsurface section. Drainage shaft 18 Loxton.
The standard subsurface section for the Pata Limestone and Bookpurnong Beds of Miocene age is described. In upward sequence Morgan Limestone, Pata Limestone and Loxton Sands are intersected in Drainage Bore 18 on Section 377, Hundred of Gordon.-
Document
Published: 01 Jan 1958
-
Bull 036 Stratigraphy of the Murray Basin in South Australia
This publication details the stratigraphy of the Murray Basin Province of South Australia. The work leading up to this report has played a major part in the understanding of the sedimentary succession of this important basin-area of the State. The...-
Document
-
RI 041 Hydrocarbon Potential of Western Murray Basin and Infrabasins
The Murray Basin is a shallow, saucer-shaped Tertiary basin covering an area of 120 700 square miles extending from the western foot of the Snowy Mountains in New South Wales and Victoria to the Mount Lofty Ranges in South Australia. Geophysical work...-
Document
-
RB 00705 Australian Oil and Gas Corporation's Lake Victoria 1. Subsurface stratigraphy and micropalaeontology study.
There is no abstract created for this record-
Document
Published: 01 Jan 1964
-
RB 00717 Beach Petroleum NL Monash no. 1 well subsurface stratigraphy and micropalaeontology.
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,...-
Document
Published: 01 Jul 1900
-
RB 00673 Wentworth 1 well (NSW). Subsurface stratigraphy and micropalaeontology study. combined with RB 00673A - Summary report on the investigation of the Razorback Ridge deposit (Braemar Iron Formation).
Australian Oil and Gas Company Wentworth No.1 was drilled 25 miles north of Wentworth, N.S.W, to a depth of 2081 feet. The well penetrated a sequence of mainly marine Tertiary rocks to a depth of 1273 feet; it then intersected 331 feet of marine Lower...-
Document
Published: 01 Dec 1900
-
RB 00687 Australian Oil Corp.'s North Renmark no. 1 well. Subsurface stratigraphy and micropalaeontology study.
North Renmark 1 was drilled 6 miles north of Renmark, to a total depth of 4018 feet. The well penetrated a sequence of Tertiary, Cretaceous and Permian rocks, mostly of marine origin, and has given the most complete section so far known from the...-
Document
Published: 01 Apr 1900
-
RB 2002/00008 Palynological analyses and dating of Early Oligocene-Early Pliocene deposits in the western Murray Basin, South Australia.
A palynological analysis made of 25 cutting samples from three TEISA program stratigraphic drillholes (PIVA 1, PIVA 5 and PIVA 10) revealed distinctive microfloristic assemblages. Dinoflagellate cysts offer a reliable method for distinguishing the...-
Document
Published: 01 Apr 2002
-
RB 2003/00009 Northern Murray Basin drilling and interpretations, 2001.
Stratigraphic drilling has been undertaken by PIRSA in the South Australian portion of the northern Murray Basin to investigate the stratigraphy and sedimentology of the Cainozoic sedimentary sequences, as well as the heavy mineral sand potential of...-
Document
Published: 01 Aug 2003
-
Murray Basin stratigraphy. NSW. Palaeontological reports.
There is no abstract created for this record-
Document
-
Monash 1. Subsurface stratigraphy and micropalaeontology.
Monash 1 is located 30 km west of Renmark, and was drilled to a total depth of 1050 m. It penetrated a sequence of Tertiary, Cretaceous and Permian rocks, mostly of marine origin. Cuttings recovered from the hole interval below 1012 m depth extending...-
Document
Published: 01 Jan 1965
-
Canegrass Lobe. Progress reports to licence expiry/full surrender, for the period 3/3/1975 to 2/3/1976. Includes Palynological laboratory report no. 183/1. Appendix 1 in progress report for the period ended 2/6/1975.
The possibility that economic coal seams may occur in suspected buried Lower Permian sediments occupying the north-western corner of the Canegrass Lobe, where no deep stratigraphic drilling has hitherto been done, was investigated by Minad using...-
Document
