Zircon U-Pb strain chronometry reveals deep impact-triggered flow

Large (>100km) meteorite impact cratering events play important roles in surface and biosphere evolution, however, their potential for widespread ductile modification of the lithosphere has been difficult to assess, due partly to our inability to isotopically age-correlate deep mineral fabrics wi...

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Main Authors: Moser, D., Davis, W., Reddy, Steven, Flemming, R., Hart, R.
Format: Journal Article
Published: Elsevier 2009
Subjects:
Online Access:http://hdl.handle.net/20.500.11937/5030
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author Moser, D.
Davis, W.
Reddy, Steven
Flemming, R.
Hart, R.
author_facet Moser, D.
Davis, W.
Reddy, Steven
Flemming, R.
Hart, R.
author_sort Moser, D.
building Curtin Institutional Repository
collection Online Access
description Large (>100km) meteorite impact cratering events play important roles in surface and biosphere evolution, however, their potential for widespread ductile modification of the lithosphere has been difficult to assess, due partly to our inability to isotopically age-correlate deep mineral fabrics with surface records. We have integrated benchmark U-Pb zircon dating methods (ID-TIMS, SHRIMP) with new microstructural techniques (EBSD, XRD) to demonstrate that crystal-plastic deformation can cause rapid out-diffusion of radiogenic Pb and accompanying trace element alteration in crystalline zircon. We have used this phenomenon to directly date fabric in Archean zircons and xenoliths of the lower crust of South Africa at 2023 15 million years, coeval with the 2020 3 million year old Vredefort cratering event at surface, with extent > or =20,000 km2. Our findings indicate that regional exogenic fabrics, similar to high-temperature tectonic fabrics, exist in ancient crust. Moreover, our results establish that crystal-plastic deformation in the lithosphere can now be directly dated and linked to planetary evolution by zircon U-Pb strain chronometry.
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spelling curtin-20.500.11937-50302017-09-13T16:04:15Z Zircon U-Pb strain chronometry reveals deep impact-triggered flow Moser, D. Davis, W. Reddy, Steven Flemming, R. Hart, R. geochronology U-Pb dating EBSD zircon tectonics planetary deformation impact Large (>100km) meteorite impact cratering events play important roles in surface and biosphere evolution, however, their potential for widespread ductile modification of the lithosphere has been difficult to assess, due partly to our inability to isotopically age-correlate deep mineral fabrics with surface records. We have integrated benchmark U-Pb zircon dating methods (ID-TIMS, SHRIMP) with new microstructural techniques (EBSD, XRD) to demonstrate that crystal-plastic deformation can cause rapid out-diffusion of radiogenic Pb and accompanying trace element alteration in crystalline zircon. We have used this phenomenon to directly date fabric in Archean zircons and xenoliths of the lower crust of South Africa at 2023 15 million years, coeval with the 2020 3 million year old Vredefort cratering event at surface, with extent > or =20,000 km2. Our findings indicate that regional exogenic fabrics, similar to high-temperature tectonic fabrics, exist in ancient crust. Moreover, our results establish that crystal-plastic deformation in the lithosphere can now be directly dated and linked to planetary evolution by zircon U-Pb strain chronometry. 2009 Journal Article http://hdl.handle.net/20.500.11937/5030 10.1016/j.epsl.2008.09.036 Elsevier fulltext
spellingShingle geochronology
U-Pb dating
EBSD
zircon
tectonics
planetary
deformation
impact
Moser, D.
Davis, W.
Reddy, Steven
Flemming, R.
Hart, R.
Zircon U-Pb strain chronometry reveals deep impact-triggered flow
title Zircon U-Pb strain chronometry reveals deep impact-triggered flow
title_full Zircon U-Pb strain chronometry reveals deep impact-triggered flow
title_fullStr Zircon U-Pb strain chronometry reveals deep impact-triggered flow
title_full_unstemmed Zircon U-Pb strain chronometry reveals deep impact-triggered flow
title_short Zircon U-Pb strain chronometry reveals deep impact-triggered flow
title_sort zircon u-pb strain chronometry reveals deep impact-triggered flow
topic geochronology
U-Pb dating
EBSD
zircon
tectonics
planetary
deformation
impact
url http://hdl.handle.net/20.500.11937/5030