Ion probe Si and O zircon data (and standard characterisation) (NERC grant NE/R002134/1)
Provided here are in-situ Si and O isotope compositions of Detrital Jack Hills and Lachlan Fold Belt zircons. These data formed the basis of the research published as: Origin and significance of Si and O isotope heterogeneities in Phanerozoic, Archean, and Hadean zircon, Trail et al., (2018), PNAS 115 (41), 10287-10292 The data are provided in a single Excel spreadsheet, with multiple tabs, which are as follows: 1. Sample description and analytical method summaries 2. Solution and laser-fluorination data for characterisation of the standards used in the Ion Probe measurement sessions 3. Ion Probe (In-situ) Si and O isotope data for the Lachlan Fold Belt and Duluth Gabbro zircons 4. Ion Probe (In-situ) Si and O isotope data for the detrital Jack Hills zircons, as well as 207Pb/206Pb age estimates 5. Raw Ion Probe Si and O isotope data for LFB samples 6. Raw Ion Probe Si and O isotope data for Jack Hills samples 7. Ion Probe (In-situ) Si isotope data for the Lachlan Fold Belt zircons (utilising O- hyperion source)
nonGeographicDataset
https://www.bgs.ac.uk/services/ngdc/accessions/index.html#item126431
function: download
http://data.bgs.ac.uk/id/dataHolding/13607434
eng
geoscientificInformation
publication
2008-06-01
Zircon
Silicon isotopes
Oxygen isotopes
NGDC Deposited Data
revision
2022
NERC_DDC
2017-03-01
2018-08-31
creation
2019-03-05
notApplicable
The data provided here were generated via 3 broad methods: Ion Probe (in-situ Si and O isotope data), Solution MC-ICP-MS (Si isotope data) and laser fluorination (O isotope data). There are detailed below, but are also described more fully in the following journal article: Origin and significance of Si and O isotope heterogeneities in Phanerozoic, Archean, and Hadean zircon, Trail et al., (2018), PNAS 115 (41), 10287-10292 The O- and Si isotopic analyses were conducted on the University of California, Los Angeles (UCLA) CAMECA ims1290 ion microprobe. The solution Si isotope data were generated using a Neptune Plus MC-ICP-MS instrument - either at IPGP, Paris, or University of St Andrews. The laser fluorination O isotope data were generated using a MAT 253 mass spectrometer at the University of Oregon.
publication
2011
false
See the referenced specification
publication
2010-12-08
false
See http://eur-lex.europa.eu/LexUriServ/LexUriServ.do?uri=OJ:L:2010:323:0011:0102:EN:PDF
MS Excel
The copyright of materials derived from the British Geological Survey's work is vested in the Natural Environment Research Council [NERC]. No part of this work may be reproduced or transmitted in any form or by any means, or stored in a retrieval system of any nature, without the prior permission of the copyright holder, via the BGS Intellectual Property Rights Manager. Use by customers of information provided by the BGS, is at the customer's own risk. In view of the disparate sources of information at BGS's disposal, including such material donated to BGS, that BGS accepts in good faith as being accurate, the Natural Environment Research Council (NERC) gives no warranty, expressed or implied, as to the quality or accuracy of the information supplied, or to the information's suitability for any use. NERC/BGS accepts no liability whatever in respect of loss, damage, injury or other occurence however caused.
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2024-04-18