Contents - Geoscience Australia
Contents - Geoscience Australia
Contents - Geoscience Australia
You also want an ePaper? Increase the reach of your titles
YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.
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