Geology of the Granville Harbour area and mineralization in the Gourlays Creek prospect
Norris, RG (1985) Geology of the Granville Harbour area and mineralization in the Gourlays Creek prospect. Honours thesis, University of Tasmania.
The dominantly (meta-)sedimentary sequence of the Granville Harbour area
ranges in age from Late,Proterozoic to Devonian. Five phases of deformation
are recognized in these sequences; two are correlated with the Late Proterozoic
Penguin Orogeny, one with the Upper Cambrian Jukesian Movement, and two with
the Early to late-Middle Devonian (Tabberabberan) Orogeny. Lower greenschist
facies metamorphism accompanied the Penguin Orogeny.
Faulted against the Oonah Formation and unconformably underlying the Mt
Zeehan Conglomerate are 415 m of interlayered schists, phyllites, quartzites
and dolomites. This sequence is a probable lithostratigraphic correlate of the
Crimson Creek Formation and has been named the Duck Creek Sequence. Minor
metavolcanics contained within the Duck Creek Sequence, Oonah Formation and
Whyte schist are defined chemically as ocean-floor tholeiite basalts.
Within the Gourlays Creek Prospect, the Oonah Formation hosts two
distinct styles of mineralization:
(i) syngenetic banded iron formation of chemical origin, and
(ii) calcic, garnet-pyroxene, metasomatic infiltration exoskarn.
The banded iron formation is a stratabound and stratiform horizon consisting of
massive and banded magnetite-pyrite-(quartz) and magnetite-barite
mineralization. This chemical exhalative, banded iron formation is a probable
analogue of the (Recent) Red Sea metalliferous sediments and is the only
recognized deposit of its type in Tasmania. Sulphur isotopes from this horizon
give 8 34 S values for pyrite in the range of -7.6 to +15.5%a and for barite,
+35.8%o. A combination of inorganic reduction of Precambrian seawater, (6 S =
+20 to +25% ), with isotope disequtlibrium, and biogenic reduction is required
to explain the range in pyrite s34s values.
Intrusion of the Devonian Heemskirk Granite was accompanied by the
formation of a garnet- pyroxene skarn. The dominantly calcic mineralogy of the
skarn is suggestive of a lime-rich protolith. The deposition of magnetitepyrrhotite-
chalcopyrite and pyrite occurred during retrograde skarn alteration.
Sulphur isotope studies of skarn-associated sulphides indicate a source
fluid with a 8
34s value of +7 to +15%0 • Such high values indicate an
inhomogeneous source consisting of barite from the banded iron formation,
primary pyrite and/or magmatic sulphur. From fluid inclusion studies,
homogenization temperatures for garnet and late-stage, retrograde quartz are
)500°C and 330-340°C respectively. Deposition of sulphides during retrograde
skarn alteration is inferred to occur at temperatures of 350-360°C, pressures
of 13-35 MPa and from a 20-21 wt% equiv. NaCl solution. Minor tin (<0.35%)
mineralization is considered to be associated with retrograde skarn formation.
|Item Type:||Thesis (Honours)|
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|Deposited On:||25 Jun 2012 13:47|
|Last Modified:||24 Sep 2012 11:23|
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