Controlled cooling-rate experiments on olivine-hosted melt inclusions: chemical diffusion and quantification of eruptive cooling-rates on Hawaii and Mars
Abstract:
Electron microprobe measurements of experimental and natural melt inclusions and their host olivines. The data are presented as weight percent concentration profiles that extend from the enclosing olivine on one side of an inclusion, across the inclusion center, and then back out into the olivine on the opposite side. Experiments were conducted in a 1 atmosphere gas-mixing furnace and consisted of a 24 hour homogenization stage followed by a controlled cooling stage. We also present data from unheated samples from three locations: (1) Papakolea, Hawaii (Mauna Loa), selected from the same cache of olivine beach sands that were used as the starting materials for the experiments, (2) Kilauea Iki, Hawaii, and (3) the shergottite Yamato 980459.
How to cite this dataset:
Saper, L. M., Stolper, E. M., 2020. Controlled cooling-rate experiments on olivine-hosted melt inclusions: chemical diffusion and quantification of eruptive cooling-rates on Hawaii and Mars, Version 1.0. Interdisciplinary Earth Data Alliance (IEDA).
https://doi.org/10.1594/IEDA/111467. Accessed 2024-04-19.
DOI Creation Date:
2020-01-03
Related
Publication(s):
Saper, L.M., Stolper, E.M., (2020), "Controlled cooling-rate experiments on olivine-hosted melt inclusions: chemical diffusion and quantification of eruptive cooling-rates on Hawaii and Mars", Geochemistry, Geophysics, Geosystems, in press
License:
Creative Commons Attribution-ShareAlike 4.0 International [CC-BY-SA-4.0]
Keyword(s):
Coverage Scope: Other
Geographic Location: Hawaii, Mars
User Contributed Keyword(s):
melt inclusions, experiments, cooling rates, diffusion, olivine, volcanic processes
Data Available On:
2020-01-03