Proterozoic onset of crustal reworking and collisional tectonics: Reappraisal of the zircon oxygen isotope record

A global U-Pb and δ18O zircon database shows temporal changes in the magmatic record related to changes in the degree of crustal reworking. The δ18O composition of bulk sediment remains relatively constant through geologic time, with a mean value of 14.9‰. In contrast, the δ18O values in magmatic zi...

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Main Authors: Spencer, Christopher, Cawood, P., Hawkesworth, C.J., Raub, T.d, Prave, A.R., Roberts, N.M.
Format: Journal Article
Published: Geological Society of America 2014
Online Access:http://hdl.handle.net/20.500.11937/23948
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author Spencer, Christopher
Cawood, P.
Hawkesworth, C.J.
Raub, T.d
Prave, A.R.
Roberts, N.M.
author_facet Spencer, Christopher
Cawood, P.
Hawkesworth, C.J.
Raub, T.d
Prave, A.R.
Roberts, N.M.
author_sort Spencer, Christopher
building Curtin Institutional Repository
collection Online Access
description A global U-Pb and δ18O zircon database shows temporal changes in the magmatic record related to changes in the degree of crustal reworking. The δ18O composition of bulk sediment remains relatively constant through geologic time, with a mean value of 14.9‰. In contrast, the δ18O values in magmatic zircons vary from relatively low values averaging ~6‰ in the Archean to increasingly higher and scattered values defining a series of peaks and troughs in post-Archean data. The degree of crustal reworking increases at times of supercontinent assembly. Therefore we attribute the pattern of post-Archean δ18O values recorded by magmatic zircons to a significant increase in the incorporation of high δ18O sediment in response to enhanced crustal thickening and reworking associated with the onset of collisional tectonics, especially during formation of supercontinents.
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spelling curtin-20.500.11937-239482018-03-29T09:06:35Z Proterozoic onset of crustal reworking and collisional tectonics: Reappraisal of the zircon oxygen isotope record Spencer, Christopher Cawood, P. Hawkesworth, C.J. Raub, T.d Prave, A.R. Roberts, N.M. A global U-Pb and δ18O zircon database shows temporal changes in the magmatic record related to changes in the degree of crustal reworking. The δ18O composition of bulk sediment remains relatively constant through geologic time, with a mean value of 14.9‰. In contrast, the δ18O values in magmatic zircons vary from relatively low values averaging ~6‰ in the Archean to increasingly higher and scattered values defining a series of peaks and troughs in post-Archean data. The degree of crustal reworking increases at times of supercontinent assembly. Therefore we attribute the pattern of post-Archean δ18O values recorded by magmatic zircons to a significant increase in the incorporation of high δ18O sediment in response to enhanced crustal thickening and reworking associated with the onset of collisional tectonics, especially during formation of supercontinents. 2014 Journal Article http://hdl.handle.net/20.500.11937/23948 10.1130/G35363.1 Geological Society of America restricted
spellingShingle Spencer, Christopher
Cawood, P.
Hawkesworth, C.J.
Raub, T.d
Prave, A.R.
Roberts, N.M.
Proterozoic onset of crustal reworking and collisional tectonics: Reappraisal of the zircon oxygen isotope record
title Proterozoic onset of crustal reworking and collisional tectonics: Reappraisal of the zircon oxygen isotope record
title_full Proterozoic onset of crustal reworking and collisional tectonics: Reappraisal of the zircon oxygen isotope record
title_fullStr Proterozoic onset of crustal reworking and collisional tectonics: Reappraisal of the zircon oxygen isotope record
title_full_unstemmed Proterozoic onset of crustal reworking and collisional tectonics: Reappraisal of the zircon oxygen isotope record
title_short Proterozoic onset of crustal reworking and collisional tectonics: Reappraisal of the zircon oxygen isotope record
title_sort proterozoic onset of crustal reworking and collisional tectonics: reappraisal of the zircon oxygen isotope record
url http://hdl.handle.net/20.500.11937/23948