Age and origin of IIE iron meteorites inferred from Hf-W chronology
Abstract
Non-magmatic iron meteorites, including the IIE group, can provide important insights into the history of metal-silicate differentiation and collisions on planetesimals. To better constrain the evolution of metal segregation and impacts on the IIE parent body, W isotopic data are reported for 10 IIE iron meteorites and a metal vein from the Portales Valley H6 chondrite. In addition, Pt isotopic data were obtained to quantify cosmic ray-induced neutron capture effects on W isotopes. After correction for these effects, the IIE iron meteorites exhibit variable pre-exposure 182W compositions, translating into Hf-W model age clusters of ~4–5 million years (Ma), ~10 Ma, ~15 Ma, and ~27 Ma after CAI formation. These distinct 182W clusters likely represent samples from several discrete metallic melt pools on the IIE parent asteroid. The earliest metal segregation event at ~4–5 Ma was likely facilitated by 26Al decay as an internal heat source. By contrast, the younger Hf-W model ages may not be chronologically meaningful, and probably reflect the effects of secondary mixing and re-equilibration of metal and silicates, likely facilitated by impacts on the IIE parent body. Thus, contrary to prior work, the Hf-W systematics of IIE iron meteorites do not require a protracted history of metal-silicatemore »
- Authors:
-
- Univ. of Munster (Germany); Lawrence Livermore National Lab. (LLNL), Livermore, CA (United States)
- Univ. of Munster (Germany)
- Publication Date:
- Research Org.:
- Lawrence Livermore National Lab. (LLNL), Livermore, CA (United States)
- Sponsoring Org.:
- USDOE National Nuclear Security Administration (NNSA)
- OSTI Identifier:
- 1592021
- Alternate Identifier(s):
- OSTI ID: 1703160
- Report Number(s):
- LLNL-JRNL-768656
Journal ID: ISSN 0016-7037; 959749; TRN: US2100900
- Grant/Contract Number:
- AC52-07NA27344; AC52-07NA2734; LLNL-JRNL-768656
- Resource Type:
- Accepted Manuscript
- Journal Name:
- Geochimica et Cosmochimica Acta
- Additional Journal Information:
- Journal Volume: 262; Journal Issue: C; Journal ID: ISSN 0016-7037
- Publisher:
- Elsevier; The Geochemical Society; The Meteoritical Society
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 58 GEOSCIENCES; Hf-W chronology; Metal-silicate separation; Iron meteorites; Planetesimals; Collisions; Planetary differentiation
Citation Formats
Kruijer, Thomas S., and Kleine, Thorsten. Age and origin of IIE iron meteorites inferred from Hf-W chronology. United States: N. p., 2019.
Web. doi:10.1016/j.gca.2019.07.039.
Kruijer, Thomas S., & Kleine, Thorsten. Age and origin of IIE iron meteorites inferred from Hf-W chronology. United States. https://doi.org/10.1016/j.gca.2019.07.039
Kruijer, Thomas S., and Kleine, Thorsten. Mon .
"Age and origin of IIE iron meteorites inferred from Hf-W chronology". United States. https://doi.org/10.1016/j.gca.2019.07.039. https://www.osti.gov/servlets/purl/1592021.
@article{osti_1592021,
title = {Age and origin of IIE iron meteorites inferred from Hf-W chronology},
author = {Kruijer, Thomas S. and Kleine, Thorsten},
abstractNote = {Non-magmatic iron meteorites, including the IIE group, can provide important insights into the history of metal-silicate differentiation and collisions on planetesimals. To better constrain the evolution of metal segregation and impacts on the IIE parent body, W isotopic data are reported for 10 IIE iron meteorites and a metal vein from the Portales Valley H6 chondrite. In addition, Pt isotopic data were obtained to quantify cosmic ray-induced neutron capture effects on W isotopes. After correction for these effects, the IIE iron meteorites exhibit variable pre-exposure 182W compositions, translating into Hf-W model age clusters of ~4–5 million years (Ma), ~10 Ma, ~15 Ma, and ~27 Ma after CAI formation. These distinct 182W clusters likely represent samples from several discrete metallic melt pools on the IIE parent asteroid. The earliest metal segregation event at ~4–5 Ma was likely facilitated by 26Al decay as an internal heat source. By contrast, the younger Hf-W model ages may not be chronologically meaningful, and probably reflect the effects of secondary mixing and re-equilibration of metal and silicates, likely facilitated by impacts on the IIE parent body. Thus, contrary to prior work, the Hf-W systematics of IIE iron meteorites do not require a protracted history of metal-silicate separation on the IIE parent body. Instead the results of this study are fully consistent with a single partial metal-silicate differentiation event driven by endogenic heating at ~4–5 Ma, followed by one or multiple impact events causing mixing and re-equilibration of metal and silicates at a later stage. As a result, the exact timing of these impact event(s) remains poorly constrained, but they most likely occurred in the first few tens of Ma of Solar System history.},
doi = {10.1016/j.gca.2019.07.039},
journal = {Geochimica et Cosmochimica Acta},
number = C,
volume = 262,
place = {United States},
year = {Mon Jul 29 00:00:00 EDT 2019},
month = {Mon Jul 29 00:00:00 EDT 2019}
}
Web of Science
Figures / Tables:
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