Stable Potassium and Iron Isotopes in Apollo 17 core 73001-2

Creator(s):
Broussard, Megan A; ORCID: 0009-0002-9207-8835
Neuman, Mason; ORCID: 0000-0002-4026-4313
Jolliff, Brad
Koefoed, Piers; ORCID: 0000-0002-4036-6088
Korotev, Randy; ORCID: 0000-0002-1292-4994
Wang, Kun; ORCID: 0000-0003-0691-7058
Abstract:
Stable potassium and iron isotopes in Apollo 17 double drive tube 73001/2. Measurements were made on the <1 mm size fraction from the 0.5 cm intervals of dissection Pass 2, after chemical dissolution and column chemistry using the Thermo Scientific Neptune Plus multicollector inductively coupled plasma mass spectrometer at Washington University in St. Louis. Isotopes are reported in delta notation in per mil units. Potassium isotopes are relative to the standard NIST SRM 3141a and iron isotopes are relative to the standard IRMM-014.
How to cite this dataset:
Broussard, M. A., Neuman, M., Jolliff, B., Koefoed, P., Korotev, R., Wang, K., 2024. Stable Potassium and Iron Isotopes in Apollo 17 core 73001-2, Version 1.0. Interdisciplinary Earth Data Alliance (IEDA). https://doi.org/10.60520/IEDA/113142. Accessed 2025-07-08.
DOI Creation Date:
2024-03-09
Related
Publication(s):
Broussard, M., Neuman, M., Jolliff, B. L., Koefoed, P., Korotev, R. L., Morris, R. V., et al. (2025). The Isotopic variation of K and Fe in Apollo 17 double drive tube 73001/2 and implications for regolith history and space weathering. Journal of Geophysical Research: Planets, 130, e2024JE008371. https://doi.org/10.1029/2024JE008371
Publication DOI:
License:
Creative Commons Attribution 4.0 International [CC-BY-4.0]
User Contributed Keyword(s):
Fe isotopes, K isotopes
Data Available On:
2024-09-16
Resource Type:
Dataset
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3142-1_ADA_Broussard-Isotopes_K_Fe.xls
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