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• W2400886135 abstract "ABSTRACTQuartz arenites are a very common geological feature on the South Island of New Zealand. The provenance of the quartz grains that form these arenites is not well constrained because standard point-counting techniques do not provide enough detailed information. In this study we distinguish different quartz types using scanning electron microscopy–cathodoluminescence combined with standard optical microscopy on the same individual quartz grains. This is done on a suite of samples collected from shallow marine quartz arenites of the Paleocene–Eocene Blondin Sand Member of the Broken River Formation (Eyre Group) at Mt Somers in the Canterbury basin on the South Island of New Zealand. Our results show that the volcanic quartz grains were derived from local volcanic source rocks, whereas metamorphic quartz grains may have been derived from either local source rocks of the Torlesse Supergroup or from distant metamorphic sources rocks via longshore transport. Plutonic quartz grains were exclusively derive..." @default.
• W2400886135 created "2016-06-24" @default.
• W2400886135 creator A5080792534 @default.
• W2400886135 creator A5090868924 @default.
• W2400886135 date "2016-04-02" @default.
• W2400886135 modified "2023-09-25" @default.
• W2400886135 title "Quartz types of the Eocene Broken River Formation, Mount Somers, South Island, New Zealand" @default.
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• W2400886135 doi "https://doi.org/10.1080/00288306.2015.1132743" @default.
• W2400886135 hasPublicationYear "2016" @default.
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