scholarly journals Use of U-isotopes in exploring groundwater flow and inter-aquifer leakage in the south-western margin of the Great Artesian Basin and Arckaringa Basin, central Australia

2018 ◽  
Vol 98 ◽  
pp. 331-344 ◽  
Author(s):  
Stacey C. Priestley ◽  
Timothy E. Payne ◽  
Jennifer J. Harrison ◽  
Vincent E.A. Post ◽  
Paul Shand ◽  
...  
Keyword(s):  
Groundwater Flow ◽  
The South ◽  
Artesian Basin ◽  
Western Margin ◽  
Great Artesian Basin ◽  
Central Australia

scholarly journals A Reappraisal of the Hydrogeology of the Western Margin of the Great Artesian Basin: Chemistry, Isotopes and Groundwater Flow

2017 ◽  
Vol 17 ◽  
pp. 428-431 ◽  
Author(s):  
Andrew J. Love ◽  
Paul Shand ◽  
Simon Fulton ◽  
Daniel Wohling ◽  
Karl E Karlstrom ◽  
...  
Keyword(s):  
Groundwater Flow ◽  
Artesian Basin ◽  
Western Margin ◽  
Great Artesian Basin

Hydrochemical variations of groundwater and spring discharge of the western Great Artesian Basin, Australia: implications for regional groundwater flow

2019 ◽  
Vol 28 (1) ◽  
pp. 263-278 ◽  
Author(s):  
Stacey C. Priestley ◽  
Paul Shand ◽  
Andrew J. Love ◽  
Laura J. Crossey ◽  
Karl E. Karlstrom ◽  
...  
Keyword(s):  
Groundwater Flow ◽  
Spring Discharge ◽  
Artesian Basin ◽  
Great Artesian Basin ◽  
Regional Groundwater

THE LAKE FROME EMBAYMENT AREA

1966 ◽  
Vol 6 (1) ◽  
pp. 93 ◽  
Author(s):  
Ralph N. Freeman
Keyword(s):  
Older Age ◽  
Structural Configuration ◽  
The South ◽  
The West ◽  
Artesian Basin ◽  
South Eastern ◽  
Great Artesian Basin ◽  
The North

The Lake Frome Embayment Area occupies a position in the southernmost extension of the Great Artesian Basin. It is bounded on the west by the North Flinders limb of the Adelaide Geosyncline and on the east by the Tibooburra Block. It is limited on the south by the Olary Region and the arbitrary northern limits are taken at the south-eastern extension of the Muloorina Gravity Swell.The structural configuration of the area is fault controlled, and is believed to be related to block movements in the basement. A complex of evolved troughs is present. Two major troughs are especially evident, the Bancannia Trough in the east and the Lake Frome Gravity Depression in the west.Remnants of Cambro-Ordovician sediments are preserved on both sides of the Embayment, although outcrop is dominated by rocks of Proterozoic and older age. Devonian sediments are present in the eastern part of the area. Jurassic-Cretaceous sediments related to the Great Artesian Basin sequence are present.

A REGIONAL INVESTIGATION TO DETERMINE TIME-DEPTH AND VELOCITY-DEPTH RELATIONSHIPS APPLICABLE IN CENTRAL AUSTRALIA

1966 ◽  
Vol 6 (1) ◽  
pp. 50
Author(s):  
Alvin R. Hosking
Keyword(s):  
Power Laws ◽  
Artesian Basin ◽  
Great Artesian Basin ◽  
Central Australia ◽  
Using Data ◽  
Sonic Logs ◽  
Time Information

Simple time-depth and velocity-depth relationships have been derived in the Western Great Artesian Basin which can be employed with seismic time information in the prediction of depth and instantaneous velocity.These relationships have been formed by using data from calibrated sonic logs and by combining a similarity between Acheson's velocity-depth equation and the “theoretical one-sixth power laws”.Variations, corresponding to horizons encountered, in the parameter “a” the equation t = aZ.83 enable the prediction of depths to the horizons C, P and Z.

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