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Australian Journal of Earth Sciences
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Research Article

Nundorite: a geological oddity of critical minerals significance from the Mount Arrowsmith Volcanics, northwestern NSW

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Received 14 Nov 2023, Accepted 21 Mar 2024, Published online: 28 Apr 2024

Figures & data

Figure 1. Visual and chemical features of nundorite. (a) Photo of a polished cut slab of ‘outcrop’ nundorite with green aegirine crystals evident. (b) Zirconium vs Al2O3/SiO2 of peralkaline igneous rocks from the global igneous geochemistry database of Gard et al. (Citation2019). The data were filtered for intermediate to felsic composition (>50 wt% SiO2) and evolved compositions with P2O5 <0.04 wt% and TiO2 <0.46 wt% to match the characteristics of nundorite. Note, very few rocks globally compare to the composition of nundorite.

Figure 1. Visual and chemical features of nundorite. (a) Photo of a polished cut slab of ‘outcrop’ nundorite with green aegirine crystals evident. (b) Zirconium vs Al2O3/SiO2 of peralkaline igneous rocks from the global igneous geochemistry database of Gard et al. (Citation2019). The data were filtered for intermediate to felsic composition (>50 wt% SiO2) and evolved compositions with P2O5 <0.04 wt% and TiO2 <0.46 wt% to match the characteristics of nundorite. Note, very few rocks globally compare to the composition of nundorite.

Figure 2. (a) Location, (b) geological setting of the northern Koonenberry Belt of western NSW and (c) local geological setting of the nundorite outcrop, adapted from Greenfield and Reid (Citation2010) and Mills et al. (Citation2015). Sample locations are presented by the coloured symbols, and nundorite sample locations are numbered (c).

Figure 2. (a) Location, (b) geological setting of the northern Koonenberry Belt of western NSW and (c) local geological setting of the nundorite outcrop, adapted from Greenfield and Reid (Citation2010) and Mills et al. (Citation2015). Sample locations are presented by the coloured symbols, and nundorite sample locations are numbered (c).

Figure 3. Textural and mineralogical changes across nundorite sampling traverse from outcrop to foliated varieties from left to right. (a) Hand-sample photos of nundorite. Note, the prominent green aegirine in the outcrop nundorite samples and increasing degree of foliation across the sample series. (b) MLA mineral maps of nundorite samples (note, the MLA technique could not be used to distinguish natrolite from analcime). The colours refer to minerals shown in (c). (c) Modal mineralogy across the sample series based on MLA mapping result, EDS and WDS analysis, thin-section petrography and XRD analysis.

Figure 3. Textural and mineralogical changes across nundorite sampling traverse from outcrop to foliated varieties from left to right. (a) Hand-sample photos of nundorite. Note, the prominent green aegirine in the outcrop nundorite samples and increasing degree of foliation across the sample series. (b) MLA mineral maps of nundorite samples (note, the MLA technique could not be used to distinguish natrolite from analcime). The colours refer to minerals shown in (c). (c) Modal mineralogy across the sample series based on MLA mapping result, EDS and WDS analysis, thin-section petrography and XRD analysis.

Figure 4. Backscattered electron images of outcrop nundorite samples. (a) Major and minor minerals in sample MA0802. (b) Monazite in interstices of aegirine, sample MA0804. (c) Euhedral schizolite and skeletal albite intergrown with matrix natrolite of sample MA0802. (d) Accessory REE and Zr phases in sample Nund-1. (e) Zr alkali silicate intergrown with aegirine in sample Nund-1. (f) Complexly zoned Zr alkali silicate associated with microcline and cerite-group minerals in sample MA0802. Mineral abbreviations: Aeg, aegirine; Crt, cerite-group mineral; Mnz, monazite; Nb, unidentified Nb-rich mineral; Ntr, natrolite; Mic, microcline; ZAS, zirconium alkali silicate.

Figure 4. Backscattered electron images of outcrop nundorite samples. (a) Major and minor minerals in sample MA0802. (b) Monazite in interstices of aegirine, sample MA0804. (c) Euhedral schizolite and skeletal albite intergrown with matrix natrolite of sample MA0802. (d) Accessory REE and Zr phases in sample Nund-1. (e) Zr alkali silicate intergrown with aegirine in sample Nund-1. (f) Complexly zoned Zr alkali silicate associated with microcline and cerite-group minerals in sample MA0802. Mineral abbreviations: Aeg, aegirine; Crt, cerite-group mineral; Mnz, monazite; Nb, unidentified Nb-rich mineral; Ntr, natrolite; Mic, microcline; ZAS, zirconium alkali silicate.

Table 1. Representative major element oxide (wt%) composition of rare metal-bearing accessory phases found in nundorite.

Figure 5. Backscattered electron images of mineral textures in foliated nundorite. (a) Poikiolitic aegirine with nepheline inclusions in sample MA0808. (b) Intergrown aegirine and aegirine-augite surrounded, and partly replaced by, hematite, sphalerite and clustered cerite-group minerals; sample MA0807. (c) Fine zircon and mica grains rimming microcline in sample MA0807. (d) Schizolite associated with zircon and cerite in sample MA0807. Mineral abbreviations: Aeg, aegirine; Aeg-Aug, aegirine-augite; Crt, cerite; Hem, hematite; Or, microcline; Sp, sphalerite; Szl, schizolite; Zrn, zircon.

Figure 5. Backscattered electron images of mineral textures in foliated nundorite. (a) Poikiolitic aegirine with nepheline inclusions in sample MA0808. (b) Intergrown aegirine and aegirine-augite surrounded, and partly replaced by, hematite, sphalerite and clustered cerite-group minerals; sample MA0807. (c) Fine zircon and mica grains rimming microcline in sample MA0807. (d) Schizolite associated with zircon and cerite in sample MA0807. Mineral abbreviations: Aeg, aegirine; Aeg-Aug, aegirine-augite; Crt, cerite; Hem, hematite; Or, microcline; Sp, sphalerite; Szl, schizolite; Zrn, zircon.

Table 2. Representative major silicate mineral compositions (wt%) of nundorite samples.

Figure 6. Changes in endmember proportions of aegirine (in clinopyroxene) and pectolite (in schizolite) across the nundorite alteration series.

Figure 6. Changes in endmember proportions of aegirine (in clinopyroxene) and pectolite (in schizolite) across the nundorite alteration series.

Table 3. Major and trace-element geochemistry and Nd isotope composition of samples of nundorite and associated mafic volcanic rocks.

Figure 7. Total-alkali vs silica diagram (from Le Maitre et al., Citation2002) of nundorite and basanite samples, and MAV rocks from Greenfield et al. (Citation2011) and references therein. The data have been filtered to exclude analyses with >8 wt% LOI, and anomalously low Na2O (<1 wt%) and K2O (<0.10 wt%), indicative of modification via alteration. Diamond symbols are data from the literature, and circle symbol are data from this study.

Figure 7. Total-alkali vs silica diagram (from Le Maitre et al., Citation2002) of nundorite and basanite samples, and MAV rocks from Greenfield et al. (Citation2011) and references therein. The data have been filtered to exclude analyses with >8 wt% LOI, and anomalously low Na2O (<1 wt%) and K2O (<0.10 wt%), indicative of modification via alteration. Diamond symbols are data from the literature, and circle symbol are data from this study.

Figure 8. NMORB-normalised multi-trace element plots of nundorite (n = 7) compared with; (a) syenites (n = 2) and basanites (n = 3) of the Mount Arrowsmith Volcanics, and (b) evolved, high alumina phonolites from the Apiau Alkaline Complex (AAC), Guyana Shield (n = 13; Figueiredo et al., Citation2022) and the Dunedin volcano (n = 11; Pontesilli et al., Citation2022; Price et al., Citation2003). Samples normalised to NMORB values of Sun and McDonough (Citation1989).

Figure 8. NMORB-normalised multi-trace element plots of nundorite (n = 7) compared with; (a) syenites (n = 2) and basanites (n = 3) of the Mount Arrowsmith Volcanics, and (b) evolved, high alumina phonolites from the Apiau Alkaline Complex (AAC), Guyana Shield (n = 13; Figueiredo et al., Citation2022) and the Dunedin volcano (n = 11; Pontesilli et al., Citation2022; Price et al., Citation2003). Samples normalised to NMORB values of Sun and McDonough (Citation1989).

Figure 9. εNd vs bulk rock Zr concentration on nundorite and rocks of the Mount Arrowsmith Volcanics (MAV). Note the similar εNd of nundorite and the MAV rocks. Circles are data from this study, and diamonds are data from Crawford et al. (Citation1997), Zhou and Whitford (Citation1994), and Greenfield et al. (Citation2011). Symbol size is larger than measurement uncertainties.

Figure 9. εNd vs bulk rock Zr concentration on nundorite and rocks of the Mount Arrowsmith Volcanics (MAV). Note the similar εNd of nundorite and the MAV rocks. Circles are data from this study, and diamonds are data from Crawford et al. (Citation1997), Zhou and Whitford (Citation1994), and Greenfield et al. (Citation2011). Symbol size is larger than measurement uncertainties.
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Data availability statement

The authors confirm that the data supporting the findings of this study are available within the article and its supplementary materials.