Glass chemistry of eruption deposits from volcanoes around Mexico City (NERC Grant NE/S009035/1)
Electron microprobe glass chemistry data from explosive eruption deposits from Popocatépetl, Iztaccíhuatl and Tláloc-Telapón volcanoes in Central México, spanning the last 700 ka. Associated with the following paper: Sunyé-Puchol, I., Hodgetts, A.G.E., Watt, S.F.L., Arce, J.L., Barfod, D.N., Mark, D.F., Sosa-Ceballos, G., Siebe, C., Dymock, R.C., Blaauw, M., Smith, V.C., 2021. Reconstructing the middle to late Pleistocene explosive eruption histories of Popocatépetl, Iztaccíhuatl and Tláloc-Telapón volcanoes in Central México. J Volcanol Geoth Res 421, 107413. https://doi.org/10.1016/j.jvolgeores.2021.107413
dataset
https://webapps.bgs.ac.uk/services/ngdc/accessions/index.html#item182112
name: Data
function: download
http://data.bgs.ac.uk/id/dataHolding/13608103
eng
geoscientificInformation
publication
2008-06-01
NGDC Deposited Data
Volcanic ejecta
Volcanic eruption
revision
2022
NERC_DDC
-99.3700
-98.1700
19.3800
19.0000
revision
2009
MEX
creation
1979
MEXICO [id=798000]
revision
2009
MX
2019-06-01
2020-10-31
creation
2023-08-23
notApplicable
These major element concentrations in the glass shards were analysed using a JEOL JXA-8200 electron microprobe equipped with five wavelength-dispersive spectrometers in the School of Archaeology, University of Oxford, UK. A beam accelerating voltage of 15 kV was used with a 6 nA current and a beam diameter of 10 μm. A narrower beam of 5 μm was used for a few highly vesicular samples (noted by a * in the file). The EMP was calibrated using a suite of mineral standards. This calibration was verified using a range of secondary glass standards (ATHO-G, StHs6/80-G and GOR128-G; Jochum et al., 2006).
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
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