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Ian Matthews

Researcher at Royal Holloway, University of London

Publications -  75
Citations -  2161

Ian Matthews is an academic researcher from Royal Holloway, University of London. The author has contributed to research in topics: Tephra & Holocene. The author has an hindex of 22, co-authored 71 publications receiving 1865 citations. Previous affiliations of Ian Matthews include Swansea University & University of London.

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A new and less destructive laboratory procedure for the physical separation of distal glass tephra shards from sediments

TL;DR: In this paper, the authors proposed a less destructive procedure for tephra extraction based on stepped heavy liquid flotation and which results in samples of sufficient quality for analysis while preserving their geochemical integrity.
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Age modelling of late Quaternary marine sequences in the Adriatic: Towards improved precision and accuracy using volcanic event stratigraphy

TL;DR: In this article, a review of the problems that constrain the reliability of radiocarbon-based age models with particular focus on those used to underpin marine records is presented, and the importance of basing such comparisons on standardised geochemical and robust statistical procedures is stressed.
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Improved age estimates for key Late Quaternary European tephra horizons in the RESET lattice

TL;DR: The RESET project as mentioned in this paper used tephra layers to tie together and synchronise the chronologies of stratigraphic records at archaeological and environmental sites, and a chronology of the key tephras in the RESET tectra lattice in the time range 10-60
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Distal tephra record for the last ca 105,000 years from core PRAD 1-2 in the central Adriatic Sea: implications for marine tephrostratigraphy

TL;DR: In this paper, a total of 25 discrete tephra layers were discovered, only one of which was visible in the core sequence, and the other 24 are not visible to the naked eye, nor were the majority detected by routine down core scanning methods.
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Was the 12.1 ka Icelandic Vedde Ash one of a kind

TL;DR: The Vedde Ash is the most important volcanic event marker layer for the correlation of Late Quaternary palaeoenvironmental archives in Europe and the North Atlantic as discussed by the authors, and has been traced across much of northern and central Europe, into northwest Russia, within North Atlantic marine sediments and into the Greenland ice cores.