The Cymbric Vale tenement is
located in the Koonenberry Belt on the eastern margin of the Curnamona
Craton, approximately 120 kilometres northeast of Broken Hill. The
Koonenberry Belt extends over a strike length of at least 200 kilometres and
is characterised by multiple, deep crustal, dip-slip fault structures with
subsidiary splays and cross structures. A number of ultramafic intrusives
occur in the region (such as at Mt Wright and Cymbric Vale) suggesting that
these faults are mantle tapping structures - favourable indications for the
occurrence of sulphide nickel deposits. Large parts of the Koonenberry Belt
are being actively explored for nickel by major nickel companies.
The Mt Wright intrusive is
anomalous in nickel and copper, however, this area lies within a national
park and is not accessible for exploration. The PlatSearch/Paradigm Cymbric
Vale tenement is located immediately south of Mt Wright and embraces a large
aeromagnetic anomaly feature considered to be a possible ultramafic
intrusive similar to Mt Wright. Bondi will undertake RAB drilling to confirm
the source of this aeromagnetic anomaly and investigate its potential for
nickel mineralisation.
Work has already commenced on
a ground magnetic survey and Bondi must complete as a minimum commitment a
RAB drilling programme costing $50,000 within the first six months.
Continuance of the agreement is subject to Bondi achieving a listing on the
Australian Stock Exchange before 31 January 2007.
Bob Richardson
Managing Director
Please direct any questions
to Bob Richardson on (02) 9906 5220 or 0414 592 080.