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Articles

U-Th-Pb zircon and monazite geochronology of Western Province gneissic rocks, central-south Westland, New Zealand

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Pages 241-269 | Published online: 27 Oct 2010

Figures & data

Fig. 1 Geological map of Western Province basement granitic, gneissic and metasedimentary rocks and key faults in central Westland (modified after Nathan et al. Citation2002; Cox & Barrell Citation2007) showing sample locations. The 10 km grid is in NZTM2000 coordinates. The inset map shows the New Zealand basement terranes in the central South Island (after Mortimer Citation2004).

Fig. 1  Geological map of Western Province basement granitic, gneissic and metasedimentary rocks and key faults in central Westland (modified after Nathan et al. Citation2002; Cox & Barrell Citation2007) showing sample locations. The 10 km grid is in NZTM2000 coordinates. The inset map shows the New Zealand basement terranes in the central South Island (after Mortimer Citation2004).

Table 1  Sample locations and lithological descriptions.

Fig. 2 Tera-Wasserberg concordia diagrams presenting uncorrected 238U/206Pb–207Pb/206Pb ratios of all zircon analyses.

Fig. 2  Tera-Wasserberg concordia diagrams presenting uncorrected 238U/206Pb–207Pb/206Pb ratios of all zircon analyses.

Fig. 3 Tera-Wasserberg concordia diagrams presenting uncorrected 238U/206Pb–207Pb/206Pb ratios of all monazite analyses (A–J). Correlations between 206Pb/238U and 208Pb/232Th ages for all monazite analyses (K–T).

Fig. 3  Tera-Wasserberg concordia diagrams presenting uncorrected 238U/206Pb–207Pb/206Pb ratios of all monazite analyses (A–J). Correlations between 206Pb/238U and 208Pb/232Th ages for all monazite analyses (K–T).

Fig. 4 Probability density plots for all samples. Orthogneiss ages >600 Ma omitted for clarity. For all plots 238U/206Pb ages <800 Ma are corrected for common Pb based on 207Pb. 207Pb/206Pb ages >800 Ma are corrected for common Pb based on 204Pb.

Fig. 4  Probability density plots for all samples. Orthogneiss ages >600 Ma omitted for clarity. For all plots 238U/206Pb ages <800 Ma are corrected for common Pb based on 207Pb. 207Pb/206Pb ages >800 Ma are corrected for common Pb based on 204Pb.

Fig. 5 Zircon cathodoluminesence (CL) and monazite back-scattered electron (BSE) grain images and SHRIMP analytical spot ages for representative (A) paragneiss A546; (C) orthogneiss A551; and (E) orthogneiss A552. Excellent agreement exists between monazite 206Pb/238U (*) and 208Pb/232Th (‘) ages. Cumulative histogram of (B) paragneiss zircon, (D) orthogneiss zircon and (F) combined paragneiss and orthogneiss monazite age structures. For all histograms 238U/206Pb ages <800 Ma are corrected for common Pb based on 207Pb. 207Pb/206Pb ages >800 Ma are corrected for common Pb based on 204Pb.

Fig. 5  Zircon cathodoluminesence (CL) and monazite back-scattered electron (BSE) grain images and SHRIMP analytical spot ages for representative (A) paragneiss A546; (C) orthogneiss A551; and (E) orthogneiss A552. Excellent agreement exists between monazite 206Pb/238U (*) and 208Pb/232Th (‘) ages. Cumulative histogram of (B) paragneiss zircon, (D) orthogneiss zircon and (F) combined paragneiss and orthogneiss monazite age structures. For all histograms 238U/206Pb ages <800 Ma are corrected for common Pb based on 207Pb. 207Pb/206Pb ages >800 Ma are corrected for common Pb based on 204Pb.

Table 2  U-Th-Pb geochronology results from analysis of paragneiss zircon. f206 = fraction of common 206Pb of the total measured Pb. Total ratios are given as measured and are uncorrected for common Pb. Correction method 1 is based on 207Pb (with 238U/206Pb ages <800 Ma). Correction method 2 is based on 204Pb (with 207Pb/206Pb ages >800 Ma).

Table 3  U-Th-Pb geochronology results from analysis of orthogneiss zircon. f206 = fraction of common 206Pb of the total measured Pb. Total ratios are given as measured and are uncorrected for common Pb. Correction method 1 is based on 207Pb (with 238U/206Pb ages <800 Ma). Correction method 2 is based on 204Pb (with 207Pb/206Pb ages >800 Ma). Spot analyses used for weighted mean 206Pb/238U age calculations of selected samples are marked in bold.

Table 4  U-Th-Pb geochronology results from analysis of paragneiss and orthogneiss monazite. f206 or f208 = fraction of common 206Pb or 208Pb of the total measured Pb. Total ratios are given as measured and are uncorrected for common Pb. Correction is based on 207Pb. Spot analyses used for weighted mean 206Pb/238U or 208Pb/232Th age calculations of selected samples are marked in bold.

Fig. 6 Map showing histograms of zircon (black) and monazite (grey) age structures for paragneisses (left) and orthogneisses (right). For all histograms, 238U/206Pb ages <800 Ma are corrected for common Pb based on 207Pb and all 207Pb/206Pb ages >800 Ma are corrected for common Pb based on 204Pb.

Fig. 6  Map showing histograms of zircon (black) and monazite (grey) age structures for paragneisses (left) and orthogneisses (right). For all histograms, 238U/206Pb ages <800 Ma are corrected for common Pb based on 207Pb and all 207Pb/206Pb ages >800 Ma are corrected for common Pb based on 204Pb.

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