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Snow pit sampling and ice cores (from Dome C) used to measured the cosmogenic radionucleide 32Si for depositional variation and determination of half life for radiometric dating methods
Entry ID: K110_2003_2004_NZ_1

Abstract: Ice core records are very useful for determining past climate because they store a wide variety of proxies for climate forcing and climate response. Accurate dating of ice cores is crucial to making use of this information and cosmogenic radionucleides are a natural indicator for dating. Until recently, there was no approprate radiometric dating method for mountain glacier ice in the time range ... View entire text
Geographic Coverage
Spatial coordinates   
  N: -77.85   S: -77.85   E: 166.75   W: 166.75

start here with 1 in span in link Ancillary Description
here with 2 in span in link Ancillary Description
here with 3 in span in link Ancillary Description
CORING DEVICES Ancillary Description
Quality The samples have not been measured due to difficulties with the measurement technique that need to be resolved before the samples are processed.
Data Set Progress
Data Center
Antarctica New Zealand, New Zealand Antarctic Institute, New Zealand Supplemental Info
Data Center URL: http://www.antarcticanz.govt.nz/

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Country: New Zealand
Phone: +64 4 570 4652
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Email: u.morgenstern at gns.cri.nz
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PO BOX 30368
City: Lower Hutt
Country: New Zealand
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Morgenstern, U., Fifield, L.K. and Tims, S.G. submitted. Progress in AMS measurement of natural 32Si for glacier ice dating. Nuclear Instruments Methods B
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DIF Creation Date: 2009-03-03
Last DIF Revision Date: 2017-08-24

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