Connecting with tephras: principles, functioning, and applications of tephrochronology in Quaternary science

dc.contributor.authorLowe, David J.
dc.coverage.spatialConference held at National Isotope Centre, GNS Science, Lower Hutt, Wellingtonen_NZ
dc.date.accessioned2013-09-05T02:56:24Z
dc.date.available2013-09-05T02:56:24Z
dc.date.issued2013
dc.description.abstractTephrochronology is a unique method for linking and dating geological, palaeoecological, palaeoclimatic, or archaeological sequences or events. The method relies firstly on stratigraphy and the law of superposition, which apply in any study that connects or correlates deposits from one place to another. Secondly, it relies on characterising and hence identifying or ‘fingerprinting’ tephra layers using either physical properties evident in the field or those obtained from laboratory analysis, including mineralogical examination by optical microscopy or geochemical analysis of glass shards or crystals (e.g., Fe-Ti oxides, ferromagnesian minerals) using the electron microprobe and other tools. Thirdly, the method is enhanced when a numerical age is obtained for a tephra layer by (1) radiometric methods such as radiocarbon, fission-track, U-series, or Ar/Ar dating, (2) incremental dating methods including dendrochronology or varved sediments or layering in ice cores, or (3) age-equivalent methods such as palaeomagnetism or correlation with marine oxygen isotope stages or palynostratigraphy. Once known, that age can be transferred from one site to the next using stratigraphic methods and by matching compositional characteristics, i.e., comparing ‘fingerprints’ from each layer. Used this way, tephrochronology is an age-equivalent dating method.en_NZ
dc.format.mimetypeapplication/pdf
dc.identifier.citationLowe, D. J. (2013). Connecting with tephras: principles, functioning, and applications of tephrochronology in Quaternary science. In: Prior, C., Rogers, K., Vandergoes, M. (eds), 10th Quaternary Techniques Short Course, Techniques of Palaeoclimatic and Palaeoenvironmental Reconstruction. National Isotope Centre, GNS Science, Lower Hutt (16-17 May), pp.1-28.en_NZ
dc.identifier.urihttps://hdl.handle.net/10289/7971
dc.language.isoenen_NZ
dc.rights© 2013 the author.
dc.source10th Quaternary Techniques Short Course. Techniques of Palaeoclimatic and Palaeoenvironmental Reconstructionen_NZ
dc.titleConnecting with tephras: principles, functioning, and applications of tephrochronology in Quaternary scienceen_NZ
dc.typeConference Contributionen_NZ
pubs.elements-id22908
pubs.finish-date2013-05-17en_NZ
pubs.start-date2013-05-16en_NZ
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