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Contents - Geoscience Australia

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APPENDIX “A”<br />

ANSIR project proposal<br />

ANSIR<br />

AUSTRALIAN<br />

NATIONAL<br />

SEISMIC IMAGING<br />

RESOURCE<br />

__________________________________________________________________________________________<br />

APPLICATION FOR USE OF FACILITY EQUIPMENT<br />

03-02R<br />

1. PROJECT TITLE<br />

Seismic imaging of the Meso-palaeoproterozoic basement architecture, Curnamona region,<br />

South <strong>Australia</strong>: Constraining the basement structure of the Curnamona Province and cratonic<br />

nucleus and implications for hydrothermal fluid flow and Pb-Zn and IOCG mineralisation<br />

2. PRINCIPAL INVESTIGATOR<br />

Name: Paul Heithersay<br />

Address: PIRSA Office of Minerals, Energy and Petroleum<br />

3. CO-INVESTIGATORS<br />

Name: Stuart Robertson<br />

Address: PIRSA Office of Minerals, Energy and Petroleum<br />

Name: Bruce Goleby (or other GA seismologist)<br />

Address: GA, Minerals and Geohazards Division<br />

4. SUMMARY OF SCIENTIFIC OBJECTIVES<br />

• Determine the depth, geometry and distribution of the Meso-Proterozoic<br />

basement, and unconformably overlying Neoproterozoic, Cambrian, Mesozoic<br />

and Tertiary sediments.<br />

• Determine the geometry, extent at depth and crustal significance of major<br />

structures.<br />

• Determine which structures controlled the original volcano-sedimentary basin<br />

geometry and changes in sedimentary and volcanic facies across the region. This<br />

will also involve developing a model that will distinguish on a seismic profile<br />

between steep late faults that offset stratigraphy and steep or deformed early<br />

faults that controlled stratigraphy.<br />

• Investigate the geometry of known and potential major fluid conduits and<br />

determine their role in the development of a) hydrothermal IOCG deposits (eg.<br />

Benagerie Ridge, Portia), and b) growth faults controlling potential syngenetic<br />

Pb-Zn metal deposition. The principal objective being vectoring to economic<br />

mineralisation under areas of barren cover.<br />

• Continue the seismic section westward from the present Broken Hill section,<br />

with the view of eventual east-west continuation across the Adelaide<br />

Geosyncline and the Gawler Craton.<br />

5. SUMMARY OF EQUIPMENT REQUEST<br />

ARAM24 seismic reflection recording system with 10Hz geophones<br />

4xIVI Vibrators<br />

6. PROPOSED TIMING<br />

April-June, 2004<br />

9

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