Influence of Hadean crust evident in basalts and cherts from the Pilbara Craton
Application of the 147Sm–143Nd and 146Sm–142Nd chronometers has suggested that the initial differentiation of Earth’s mantle into enriched and depleted reservoirs may have begun within the first 100–200 million years of Earth’s history1. However, little is known about the differentiation of the earl...
| Main Authors: | , , , , |
|---|---|
| Format: | Journal Article |
| Published: |
Nature Publishing Group, Macmillan Publishers Ltd
2010
|
| Online Access: | http://hdl.handle.net/20.500.11937/44645 |
| _version_ | 1848757060713316352 |
|---|---|
| author | Tessalina, Svetlana Bourdon, B. Van Kranendonk, M. Brick, J. Philippot, P. |
| author_facet | Tessalina, Svetlana Bourdon, B. Van Kranendonk, M. Brick, J. Philippot, P. |
| author_sort | Tessalina, Svetlana |
| building | Curtin Institutional Repository |
| collection | Online Access |
| description | Application of the 147Sm–143Nd and 146Sm–142Nd chronometers has suggested that the initial differentiation of Earth’s mantle into enriched and depleted reservoirs may have begun within the first 100–200 million years of Earth’s history1. However, little is known about the differentiation of the early crust; although evidence has suggested the presence of enriched crustal material2, 3, 4, 5, data regarding the nature and composition of this crust are limited. Here we present 147Sm–143Nd data from the weakly metamorphosed basalt and layered chert–barite successions from the Dresser Formation of the Pilbara Craton, Western Australia. The Sm–Nd isochron indicates an age of 3.49±0.10 billion years, in agreement with previous estimates from Pb–Pb (ref. 6) and U–Pb (ref. 7) dating, which indicates that the Sm–Nd system has not been reset. Our measured εNd value of −3.3±1.0 for the rocks at this site is consistent with formation from an older protolith. On the basis of our modelling of trace element and isotopic compositions from these rocks, we suggest that the older component was crustal in nature, and differentiated from the convective mantle more than 4.3 billion years ago. |
| first_indexed | 2025-11-14T09:22:06Z |
| format | Journal Article |
| id | curtin-20.500.11937-44645 |
| institution | Curtin University Malaysia |
| institution_category | Local University |
| last_indexed | 2025-11-14T09:22:06Z |
| publishDate | 2010 |
| publisher | Nature Publishing Group, Macmillan Publishers Ltd |
| recordtype | eprints |
| repository_type | Digital Repository |
| spelling | curtin-20.500.11937-446452017-09-13T14:10:55Z Influence of Hadean crust evident in basalts and cherts from the Pilbara Craton Tessalina, Svetlana Bourdon, B. Van Kranendonk, M. Brick, J. Philippot, P. Application of the 147Sm–143Nd and 146Sm–142Nd chronometers has suggested that the initial differentiation of Earth’s mantle into enriched and depleted reservoirs may have begun within the first 100–200 million years of Earth’s history1. However, little is known about the differentiation of the early crust; although evidence has suggested the presence of enriched crustal material2, 3, 4, 5, data regarding the nature and composition of this crust are limited. Here we present 147Sm–143Nd data from the weakly metamorphosed basalt and layered chert–barite successions from the Dresser Formation of the Pilbara Craton, Western Australia. The Sm–Nd isochron indicates an age of 3.49±0.10 billion years, in agreement with previous estimates from Pb–Pb (ref. 6) and U–Pb (ref. 7) dating, which indicates that the Sm–Nd system has not been reset. Our measured εNd value of −3.3±1.0 for the rocks at this site is consistent with formation from an older protolith. On the basis of our modelling of trace element and isotopic compositions from these rocks, we suggest that the older component was crustal in nature, and differentiated from the convective mantle more than 4.3 billion years ago. 2010 Journal Article http://hdl.handle.net/20.500.11937/44645 10.1038/ngeo772 Nature Publishing Group, Macmillan Publishers Ltd restricted |
| spellingShingle | Tessalina, Svetlana Bourdon, B. Van Kranendonk, M. Brick, J. Philippot, P. Influence of Hadean crust evident in basalts and cherts from the Pilbara Craton |
| title | Influence of Hadean crust evident in basalts and cherts from the Pilbara Craton |
| title_full | Influence of Hadean crust evident in basalts and cherts from the Pilbara Craton |
| title_fullStr | Influence of Hadean crust evident in basalts and cherts from the Pilbara Craton |
| title_full_unstemmed | Influence of Hadean crust evident in basalts and cherts from the Pilbara Craton |
| title_short | Influence of Hadean crust evident in basalts and cherts from the Pilbara Craton |
| title_sort | influence of hadean crust evident in basalts and cherts from the pilbara craton |
| url | http://hdl.handle.net/20.500.11937/44645 |