Precise lead isotope fingerprinting of hydrothermal activity associated with Ordovician to Carboniferous metallogenic events in the Lachlan fold belt of New South Wales

1995 ◽  
Vol 90 (6) ◽  
pp. 1467-1505 ◽  
Author(s):  
Graham R. Carr ◽  
Judith A. Dean ◽  
David W. Suppel ◽  
Paul S. Heithersay
Keyword(s):  
Lead Isotope ◽  
New South ◽  
New South Wales ◽  
Hydrothermal Activity ◽  
Fold Belt ◽  
South Wales ◽  
Lachlan Fold Belt

Lachlan Fold Belt in New South Wales

1978 ◽  
Vol 48 (3-4) ◽  
pp. 217-265 ◽  
Author(s):  
L.B. Gilligan ◽  
E. Scheibner
Keyword(s):  
New South ◽  
New South Wales ◽  
Fold Belt ◽  
South Wales ◽  
Lachlan Fold Belt

Vanadium-Bearing Margarite from the Lachlan Fold Belt, New South Wales, Australia

1988 ◽  
Vol 52 (366) ◽  
pp. 341-345 ◽  
Author(s):  
V. J. Morand
Keyword(s):  
Solid Solution ◽  
Local Reaction ◽  
New South ◽  
New South Wales ◽  
Contact Aureole ◽  
Fold Belt ◽  
Metamorphic Mineral ◽  
South Wales ◽  
Lachlan Fold Belt ◽  
Black Slate

AbstractMargarite occurs in Ordovician black slate within the contact aureole of the Wyangala Batholith, in the Lachlan Fold Belt in New South Wales. This occurrence is the first described from New South Wales. It is a regional metamorphic mineral replacing chiastolitic andalusite, and contains up to 1.07% V2O3 and up to 0.37% Cr2O3. Vanadium and chromium here substitute for octahedral aluminium. Margarite is produced by a local reaction in which Ca and H2O are introduced into andalusite grains. There is a significant paragonite component in the margarite but negligible muscovite solid solution.

Porphyry gold-copper mineralisation in the Cadia district, eastern Lachlan Fold Belt, New South Wales, and its relationship to shoshonitic magmatism

2002 ◽  
Vol 37 (1) ◽  
pp. 100-116 ◽  
Author(s):  
John Holliday ◽  
Alan Wilson ◽  
Philip Blevin ◽  
Ian Tedder ◽  
Paul Dunham ◽  
...  
Keyword(s):  
New South ◽  
New South Wales ◽  
Fold Belt ◽  
South Wales ◽  
Lachlan Fold Belt
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