Can the size of K-feldspar phenocrysts be used to map the occurrence of mylonitic shear zones?: Results from the Wyangala Granite, Eastern Lachlan Fold Belt, New South Wales

L.T. White; P.G. Lennox

doi:10.1080/08120099.2010.481326

Can the size of K-feldspar phenocrysts be used to map the occurrence of mylonitic shear zones? Results from the Wyangala Granite, Eastern Lachlan Fold Belt, New South Wales

L.T. White
, P.G. Lennox

Earth Sciences

Research output: Contribution to journal › Article › peer-review

Original language	English
Pages (from-to)	395-410
Number of pages	16
Journal	Australian Journal of Earth Sciences
Volume	57
Issue number	4
DOIs	https://doi.org/10.1080/08120099.2010.481326
Publication status	Published - 1 Jun 2010

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10.1080/08120099.2010.481326

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Can the size of K-feldspar phenocrysts be used to map the occurrence of mylonitic shear zones? Results from the Wyangala Granite, Eastern Lachlan Fold Belt, New South Wales

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