Published July 10, 2002
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Figure 1 in The Tumbarumba Basaltic Gem Field, New South Wales: In Relation to Sapphire-Ruby Deposits of Eastern Australia
Description
Figure 1. Distribution of gem-gearing deposits (Co) related to Cainozoic basalts (enclosed areas) and deep leads (dashes) overlying basement rocks, with the Tumut Ponds serpentinite belt (filled areas). Modified from Wagga Wagga 1: 250 000 metallogenic map, showing locations of basalt sample (Nos), thin section (+) and analytical (×) sites, K-Ar basalt dates (Ma) with previous dating (O) and new dates (Z), zircon fission track dating sites (FT-Ma), zircon U/Pb isotope dating sites (U/Pb Ma), likely eruptive sites (Δ) and possible eruptive sites (Δ).
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Published as part of Sutherland, F. L., Graham, I. T., Pogson, R. E., Schwarz, D., Webb, G. B., Coenraads, Robert R., Fanning, C. M., Hollis, J. D. & Allen, T. C., 2002, The Tumbarumba Basaltic Gem Field, New South Wales: In Relation to Sapphire-Ruby Deposits of Eastern Australia, pp. 215-248 in Records of the Australian Museum 54 (2) on page 216, DOI: 10.3853/j.0067-1975.54.2002.1358, http://zenodo.org/record/10092489Files
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- Journal article: 10.3853/j.0067-1975.54.2002.1358 (DOI)
- Journal article: urn:lsid:plazi.org:pub:FF87A417FFAAFFA2FFF65863FF8EFFC6 (LSID)
- Journal article: https://zenodo.org/record/10092489 (URL)