40Ar/39Ar impact ages and time-temperature argon diffusion history of the Bunburra Rockhole anomalous basaltic achondrite

F. Jourdan, G.K. Benedix, Ela Eroglu, P.A. Bland, A. Bouvier

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Abstract

The Bunburra Rockhole meteorite is a brecciated anomalous basaltic achondrite containing coarse-, medium- and fine-grained lithologies. Petrographic observations constrain the limited shock pressure to between ca. 10GPa and 20GPa. In this study, we carried out nine 40Ar/39Ar step-heating experiments on distinct single-grain fragments extracted from the coarse and fine lithologies. We obtained six plateau ages and three mini-plateau ages. These ages fall into two internally concordant populations with mean ages of 3640±21Ma (n=7; P=0.53) and 3544±26Ma (n=2; P=0.54), respectively. Based on these results, additional 40Ar/39Ar data of fusion crust fragments, argon diffusion modelling, and petrographic observations, we conclude that the principal components of the Bunburra Rockhole basaltic achondrite are from a melt rock formed at ~3.64Ga by a medium to large impact event. The data imply that this impact generated high enough energy to completely melt the basaltic target rock and reset the Ar systematics, but only partially reset the Pb-Pb age. We also conclude that a complete 40Ar* resetting of pyroxene and plagioclase at this time could not have been achieved at solid-state conditions. Comparison with a terrestrial analog (Lonar crater) shows that the time-temperature conditions required to melt basaltic target rocks upon impact are relatively easy to achieve. Ar data also suggest that a second medium-size impact event occurred on a neighbouring part of the same target rock at ~3.54Ga. Concordant low-temperature step ages of the nine aliquots suggest that, at ~3.42Ga, a third smaller impact excavated parts of the ~3.64Ga and ~3.54Ga melt rocks and brought the fragments together. The lack of significant impact activity after 3.5Ga, as recorded by the Bunburra Rockhole suggests that (1) either the meteorite was ejected in a small secondary parent body where it resided untouched by large impacts, or (2) it was covered by a porous heat-absorbing regolith blanket which, when combined with the diminishing frequency of large impacts in the solar system, protected Bunburra from subsequent major heating events. Finally we note that the total (K/Ar) resetting impact event history recorded by some of the brecciated eucrites (peak at 3.8-3.5Ga) is similar to the large impact history recorded by the Bunburra Rockhole parent body (ca. 3.64-3.54Ga; this study) and could indicate a similar position in the asteroid belt at that time. © 2014 Elsevier Ltd.
Original languageEnglish
Pages (from-to)391-409
JournalGeochimica et Cosmochimica Acta
Volume140
DOIs
Publication statusPublished - 2014

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achondrite
Argon
argon
Rocks
Meteorites
history
melt
Lithology
resetting
rock
temperature
parent body
meteorite
Temperature
lithology
Heating
Asteroids
plateau
Solar system
heating

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Jourdan, F. ; Benedix, G.K. ; Eroglu, Ela ; Bland, P.A. ; Bouvier, A. / 40Ar/39Ar impact ages and time-temperature argon diffusion history of the Bunburra Rockhole anomalous basaltic achondrite. In: Geochimica et Cosmochimica Acta. 2014 ; Vol. 140. pp. 391-409.
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title = "40Ar/39Ar impact ages and time-temperature argon diffusion history of the Bunburra Rockhole anomalous basaltic achondrite",
abstract = "The Bunburra Rockhole meteorite is a brecciated anomalous basaltic achondrite containing coarse-, medium- and fine-grained lithologies. Petrographic observations constrain the limited shock pressure to between ca. 10GPa and 20GPa. In this study, we carried out nine 40Ar/39Ar step-heating experiments on distinct single-grain fragments extracted from the coarse and fine lithologies. We obtained six plateau ages and three mini-plateau ages. These ages fall into two internally concordant populations with mean ages of 3640±21Ma (n=7; P=0.53) and 3544±26Ma (n=2; P=0.54), respectively. Based on these results, additional 40Ar/39Ar data of fusion crust fragments, argon diffusion modelling, and petrographic observations, we conclude that the principal components of the Bunburra Rockhole basaltic achondrite are from a melt rock formed at ~3.64Ga by a medium to large impact event. The data imply that this impact generated high enough energy to completely melt the basaltic target rock and reset the Ar systematics, but only partially reset the Pb-Pb age. We also conclude that a complete 40Ar* resetting of pyroxene and plagioclase at this time could not have been achieved at solid-state conditions. Comparison with a terrestrial analog (Lonar crater) shows that the time-temperature conditions required to melt basaltic target rocks upon impact are relatively easy to achieve. Ar data also suggest that a second medium-size impact event occurred on a neighbouring part of the same target rock at ~3.54Ga. Concordant low-temperature step ages of the nine aliquots suggest that, at ~3.42Ga, a third smaller impact excavated parts of the ~3.64Ga and ~3.54Ga melt rocks and brought the fragments together. The lack of significant impact activity after 3.5Ga, as recorded by the Bunburra Rockhole suggests that (1) either the meteorite was ejected in a small secondary parent body where it resided untouched by large impacts, or (2) it was covered by a porous heat-absorbing regolith blanket which, when combined with the diminishing frequency of large impacts in the solar system, protected Bunburra from subsequent major heating events. Finally we note that the total (K/Ar) resetting impact event history recorded by some of the brecciated eucrites (peak at 3.8-3.5Ga) is similar to the large impact history recorded by the Bunburra Rockhole parent body (ca. 3.64-3.54Ga; this study) and could indicate a similar position in the asteroid belt at that time. {\circledC} 2014 Elsevier Ltd.",
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40Ar/39Ar impact ages and time-temperature argon diffusion history of the Bunburra Rockhole anomalous basaltic achondrite. / Jourdan, F.; Benedix, G.K.; Eroglu, Ela; Bland, P.A.; Bouvier, A.

In: Geochimica et Cosmochimica Acta, Vol. 140, 2014, p. 391-409.

Research output: Contribution to journalArticle

TY - JOUR

T1 - 40Ar/39Ar impact ages and time-temperature argon diffusion history of the Bunburra Rockhole anomalous basaltic achondrite

AU - Jourdan, F.

AU - Benedix, G.K.

AU - Eroglu, Ela

AU - Bland, P.A.

AU - Bouvier, A.

PY - 2014

Y1 - 2014

N2 - The Bunburra Rockhole meteorite is a brecciated anomalous basaltic achondrite containing coarse-, medium- and fine-grained lithologies. Petrographic observations constrain the limited shock pressure to between ca. 10GPa and 20GPa. In this study, we carried out nine 40Ar/39Ar step-heating experiments on distinct single-grain fragments extracted from the coarse and fine lithologies. We obtained six plateau ages and three mini-plateau ages. These ages fall into two internally concordant populations with mean ages of 3640±21Ma (n=7; P=0.53) and 3544±26Ma (n=2; P=0.54), respectively. Based on these results, additional 40Ar/39Ar data of fusion crust fragments, argon diffusion modelling, and petrographic observations, we conclude that the principal components of the Bunburra Rockhole basaltic achondrite are from a melt rock formed at ~3.64Ga by a medium to large impact event. The data imply that this impact generated high enough energy to completely melt the basaltic target rock and reset the Ar systematics, but only partially reset the Pb-Pb age. We also conclude that a complete 40Ar* resetting of pyroxene and plagioclase at this time could not have been achieved at solid-state conditions. Comparison with a terrestrial analog (Lonar crater) shows that the time-temperature conditions required to melt basaltic target rocks upon impact are relatively easy to achieve. Ar data also suggest that a second medium-size impact event occurred on a neighbouring part of the same target rock at ~3.54Ga. Concordant low-temperature step ages of the nine aliquots suggest that, at ~3.42Ga, a third smaller impact excavated parts of the ~3.64Ga and ~3.54Ga melt rocks and brought the fragments together. The lack of significant impact activity after 3.5Ga, as recorded by the Bunburra Rockhole suggests that (1) either the meteorite was ejected in a small secondary parent body where it resided untouched by large impacts, or (2) it was covered by a porous heat-absorbing regolith blanket which, when combined with the diminishing frequency of large impacts in the solar system, protected Bunburra from subsequent major heating events. Finally we note that the total (K/Ar) resetting impact event history recorded by some of the brecciated eucrites (peak at 3.8-3.5Ga) is similar to the large impact history recorded by the Bunburra Rockhole parent body (ca. 3.64-3.54Ga; this study) and could indicate a similar position in the asteroid belt at that time. © 2014 Elsevier Ltd.

AB - The Bunburra Rockhole meteorite is a brecciated anomalous basaltic achondrite containing coarse-, medium- and fine-grained lithologies. Petrographic observations constrain the limited shock pressure to between ca. 10GPa and 20GPa. In this study, we carried out nine 40Ar/39Ar step-heating experiments on distinct single-grain fragments extracted from the coarse and fine lithologies. We obtained six plateau ages and three mini-plateau ages. These ages fall into two internally concordant populations with mean ages of 3640±21Ma (n=7; P=0.53) and 3544±26Ma (n=2; P=0.54), respectively. Based on these results, additional 40Ar/39Ar data of fusion crust fragments, argon diffusion modelling, and petrographic observations, we conclude that the principal components of the Bunburra Rockhole basaltic achondrite are from a melt rock formed at ~3.64Ga by a medium to large impact event. The data imply that this impact generated high enough energy to completely melt the basaltic target rock and reset the Ar systematics, but only partially reset the Pb-Pb age. We also conclude that a complete 40Ar* resetting of pyroxene and plagioclase at this time could not have been achieved at solid-state conditions. Comparison with a terrestrial analog (Lonar crater) shows that the time-temperature conditions required to melt basaltic target rocks upon impact are relatively easy to achieve. Ar data also suggest that a second medium-size impact event occurred on a neighbouring part of the same target rock at ~3.54Ga. Concordant low-temperature step ages of the nine aliquots suggest that, at ~3.42Ga, a third smaller impact excavated parts of the ~3.64Ga and ~3.54Ga melt rocks and brought the fragments together. The lack of significant impact activity after 3.5Ga, as recorded by the Bunburra Rockhole suggests that (1) either the meteorite was ejected in a small secondary parent body where it resided untouched by large impacts, or (2) it was covered by a porous heat-absorbing regolith blanket which, when combined with the diminishing frequency of large impacts in the solar system, protected Bunburra from subsequent major heating events. Finally we note that the total (K/Ar) resetting impact event history recorded by some of the brecciated eucrites (peak at 3.8-3.5Ga) is similar to the large impact history recorded by the Bunburra Rockhole parent body (ca. 3.64-3.54Ga; this study) and could indicate a similar position in the asteroid belt at that time. © 2014 Elsevier Ltd.

U2 - 10.1016/j.gca.2014.05.039

DO - 10.1016/j.gca.2014.05.039

M3 - Article

VL - 140

SP - 391

EP - 409

JO - Geochimica et Cosmochimica Acta

JF - Geochimica et Cosmochimica Acta

SN - 0016-7037

ER -