Luminescence dating of young coastal deposits from New Zealand using feldspar

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Abstract

A new measurement protocol has been tested on K-feldspars from Whanganui Inlet and Parengarenga Harbour, New Zealand. A Single Aliquot Regenerative (SAR) dose protocol, using two successive infrared (IR) stimulations (post-IR IR SAR protocol) is setup for these young (<1000 years) coastal sediments. Significant anomalous fading (g2days=7 %/decade) is observed using the conventional IR signal measured at 50°C. In contrast, the fading rate of the IR signal measured at ele-vated temperature (150°C) after the IR stimulation at 50°C (a post-IR IR signal) is not significant (g 2days = 1 %≤decade). Surprisingly low residual infrared stimulated luminescence (IRSL) signals were observed for a surface sample, suggesting that accurate ages as young as ∼50 years can be obtained for these recent deposits. IRSL ages ranging between 48±6 years and 1050±50 years are obtained from six samples, indicating that sediment accumulation has occurred at the two sites during the last millennia, despite a falling trend in relative sea-level in Whanganui Inlet and a stable relative sea-level at Parengarenga Harbour. © 2011 Silesian University of Technology, Gliwice, Poland. All rights reserved.

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Madsen, A. T., Buylaert, J. P., & Murray, A. S. (2011). Luminescence dating of young coastal deposits from New Zealand using feldspar. Geochronometria, 38(4), 379–390. https://doi.org/10.2478/s13386-011-0042-5

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