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Wyborn, L. (1998) Younger ca 1500 Ma granites of the Williams and Naraku Batholiths, Cloncurry district, eastern Mt Isa Inlier: Geochemistry, origin, metallogenic significance and exploration indicators. Australian Journal of Earth Sciences, 45 (3). p.397-411. doi:10.1080/08120099808728400

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Reference TypeJournal (article/letter/editorial)
TitleYounger ca 1500 Ma granites of the Williams and Naraku Batholiths, Cloncurry district, eastern Mt Isa Inlier: Geochemistry, origin, metallogenic significance and exploration indicators
JournalAustralian Journal of Earth Sciences
AuthorsWyborn, L.Author
Year1998 (June)Volume45
Page(s)397-411Issue3
PublisherInforma UK Limited
URL
DOIdoi:10.1080/08120099808728400Search in ResearchGate
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Mindat Ref. ID497128Long-form Identifiermindat:1:5:497128:7
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Full ReferenceWyborn, L. (1998) Younger ca 1500 Ma granites of the Williams and Naraku Batholiths, Cloncurry district, eastern Mt Isa Inlier: Geochemistry, origin, metallogenic significance and exploration indicators. Australian Journal of Earth Sciences, 45 (3). p.397-411. doi:10.1080/08120099808728400
Plain TextWyborn, L. (1998) Younger ca 1500 Ma granites of the Williams and Naraku Batholiths, Cloncurry district, eastern Mt Isa Inlier: Geochemistry, origin, metallogenic significance and exploration indicators. Australian Journal of Earth Sciences, 45 (3). p.397-411. doi:10.1080/08120099808728400
In(1998, June) Australian Journal of Earth Sciences Vol. 45 (3) Informa UK Limited

See Also

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Perkins, C.; Wyborn, L. A. I. (1998) Age of Cu‐Au mineralisation, Cloncurry district, eastern Mt Isa Inlier, Queensland, as determined by 40Ar/39Ar dating. Australian Journal of Earth Sciences, 45 (2). p.233-246. doi:10.1080/08120099808728384
Davidson, G. J. (1998) Variation in copper‐gold styles through time in the Proterozoic Cloncurry goldfield, Mt Isa Inlier: A reconnaissance view. Australian Journal of Earth Sciences, 45 (3) 445-462 doi:10.1080/08120099808728403
Williams, P. J. (1998) Metalliferous economic geology of the Mt Isa Eastern Succession, Queensland. Australian Journal of Earth Sciences, 45 (3) 329-341 doi:10.1080/08120099808728395
Page, R. W., Sun, S‐S. (1998) Aspects of geochronology and crustal evolution in the Eastern Fold Belt, Mt Isa Inlier∗. Australian Journal of Earth Sciences, 45 (3) 343-361 doi:10.1080/08120099808728396
Rubenach, M. J., Barker, A. J. (1998) Metamorphic and metasomatic evolution of the Snake Creek Anticline, Eastern Succession, Mt Isa Inlier. Australian Journal of Earth Sciences, 45 (3) 363-372 doi:10.1080/08120099808728397
Mark, G., Oliver, N. H. S., Carew, M. J. (2006) Insights into the genesis and diversity of epigenetic Cu – Au mineralisation in the Cloncurry district, Mt Isa Inlier, northwest Queensland. Australian Journal of Earth Sciences, 53 (1) 109-124 doi:10.1080/08120090500434583
Mares, V. M. (1998) Structural development of the Soldiers Cap Group in the Eastern Fold Belt of the Mt Isa Inlier: A succession of horizontal and vertical deformation events and large‐scale shearing. Australian Journal of Earth Sciences, 45 (3) 373-387 doi:10.1080/08120099808728398
Page, R. W., Sweet, I. P. (1998) Geochronology of basin phases in the western Mt Isa Inlier, and correlation with the McArthur Basin∗. Australian Journal of Earth Sciences, 45 (2) 219-232 doi:10.1080/08120099808728383
Williams, P. J. (1998) Magmatic iron enrichment in high‐iron metatholeiites associated with ‘Broken Hill‐type’ Pb‐Zn‐Ag deposits, Mt Isa Eastern Succession∗. Australian Journal of Earth Sciences, 45 (3) 389-396 doi:10.1080/08120099808728399
Austin, J. R., Blenkinsop, T. G. (2010) Cloncurry Fault Zone: strain partitioning and reactivation in a crustal-scale deformation zone, Mt Isa Inlier. Australian Journal of Earth Sciences, 57 (1) 1-21 doi:10.1080/08120090903416187
Davis, B. K., Pollard, P. J., Lally, J. H., McNaughton, N. J., Blake, K., Williams, P. J. (2001) Deformation history of the Naraku Batholith, Mt Isa Inlier, Australia: Implications for pluton ages and geometries from structural study of the Dipvale Granodiorite and Levian Granite. Australian Journal of Earth Sciences, 48 (1) 113-129 doi:10.1046/j.1440-0952.2001.00848.x
 
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