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Title: 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 » 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.« less

Authors:
ORCiD logo [1];  [2]
  1. Univ. of Munster (Germany); Lawrence Livermore National Lab. (LLNL), Livermore, CA (United States)
  2. 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}
}

Journal Article:

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Cited by: 18 works
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Figures / Tables:

Fig. 1 Fig. 1: (a.) ε196Pt (8/5) vs. ε192Pt (8/5), and (b.) ε194Pt (8/5) vs. ε194Pt (6/5) data for IIE iron meteorites and the Portales Valley metal vein. Distinguished are IIE irons without silicate inclusions (square symbols), with fractionated silicate inclusions (diamonds), and with unfractionated silicate inclusions (circles). Grey squares represent modeledmore » predictions for secondary neutron capture and the solid black line is a calculated mixing line between the terrestrial Pt isotope composition and presumed nucleosynthetic s- and r-process components (Kruijer et al., 2013). Ir/Pt for Miles, Mont Dieu and Weekeroo Station are from Wasson (2017).« less

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Figures/Tables have been extracted from DOE-funded journal article accepted manuscripts.