Geological Setting, Deposit, Mineralisation (i) Describe the regional geology Sample Clauses

Geological Setting, Deposit, Mineralisation (i) Describe the regional geology. The Butcher Well project is situated in the Laverton district, within the eastern part of the Kurnalpi Tectonic Terrane, a subdivision of the Eastern Goldfields Superterrane of the Archean Yilgarn Craton, Western Australia (Figure 2). The Kurnalpi Terrane is the second most gold-endowed Terrane in the Yilgarn (following the Kalgoorlie Terrane), and hosts the Xxxxxxx Xxx (0Xxx), Xxxxxxx (0Xxx) and several more significant gold deposits within 50 km of Butcher Well. All are orogenic- style deposits hosted within amalgamated greenstone belts between granite plutons. A major structure within the western margin of the Laverton district is the easterly-dipping Xxxxx Fault. The major gold deposits are located off steeper secondary structures within its hangingwall. Butcher Well and Mt. Xxxxxx are located between two major north-northeast trending faults. The area between the two Xxxxx faults is characterised by broad-scale north-northwest trending isoclinal folds and shears, collectively named the Mt. Hornet Shear Zone, in sub-vertically dipping intermediate to mafic volcanic and volcaniclastic rocks, epiclastic sedimentary rocks and chert or BIF. Figure 2: Terrane map of the Yilgarn Craton (after Xxxxxxx et al. 2006), and location of the Laverton district (blue box). (ii) Describe the project geology including deposit type, geological setting and style of mineralisation. Butcher Well appears to be on the sub-vertical eastern limb of an isoclinal fold, possibly an anticline, with mafic volcanic rocks forming its core (approximately of 2.5km wide), flanked by clastic sedimentary rocks. (iii) Discuss the geological model or concepts being applied in the investigation and on the basis of which the exploration programme is planned. Describe the inferences made from this model. Gold is associated principally with finely-disseminated pyrite and arsenopyrite within the host rock, concentrated within narrow planar zones, rather than in large auriferous quartz veins as is more common in orogenic gold deposits. Fresh-rock mineralisation is associated with host-rock brecciation, dense micro-veining, and intense sulphidic alteration with classic lower-greenschist alteration mineralogy: quartz-albite-ankerite-pyrite-arsenopyrite. The mineralised zones often do not host obvious measurable structures such as vein sets or foliation. Further details on alteration are in the Alteration section below. Leapfrog Geo was also used to model the mineralisation. The Vein System tool was ...
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