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| Content Provider | Springer Nature Link |
|---|---|
| Author | Zhao, Jun Hong Zhou, Mei Fu Zheng, Jian Ping |
| Copyright Year | 2013 |
| Abstract | Zircon textures and micro-chemical compositions precisely record the origin and petrogenesis of granitoids, which are crucial for evaluating crustal growth and reworking, thermal and geodynamic evolution. Zircons in peraluminous granitoids from the three largest 820 Ma complexes (Guibei, Yueyang and Jiuling) in the Jiangnan Fold Belt in South China are used to constrain their sources and petrogenetic processes. Zircons in the Guibei granitoids have complex internal structures. Nearly all magmatic and inherited zircons have similar εHf (−6.8 to +5.6) and δ18O values (8.8–11.6 ‰) and dominantly lie between εHf evolution vectors for a crust created between 1.7 and 2.1 Ga, suggesting that the Guibei granitoids were produced by partial melting of recycled heterogeneous supracrustal material. However, the Yueyang granitoids contain zircons with high εHf (−0.5 to +9.7) and relatively low δ18O values (5.9–8.4 ‰) and two-stage model ages of 1.1–1.8 Ga, and thus may have been formed by melting of mafic rocks from the lower crust. The Jiuling granitoids and their enclaves contain more complex zircons with more variable εHf (−7.2 to +9.7) and δ18O values (7.0–10.6 ‰), and lie along the mixing trend between the above-proposed infracrustal and supracrustal granitoids. Therefore, the Neoproterozoic peraluminous granitoids in the Jiangnan Fold Belt were produced by melting and mixing of continental crust. Compared with extremely low (≤4 ‰) and negative δ18O values of Neoproterozoic igneous zircons formed in its northern active continental margin, the high δ18O peraluminous granitoids in the southeastern Yangtze Block are considered to have been formed by melting of hydrothermally unaltered continental crust triggered by asthenosphere upwelling in the Nanhua back-arc basin. |
| Starting Page | 1505 |
| Ending Page | 1519 |
| Page Count | 15 |
| File Format | |
| ISSN | 00107999 |
| Journal | Contributions to Mineralogy and Petrology |
| Volume Number | 166 |
| Issue Number | 5 |
| e-ISSN | 14320967 |
| Language | English |
| Publisher | Springer Berlin Heidelberg |
| Publisher Date | 2013-09-27 |
| Publisher Place | Berlin/Heidelberg |
| Access Restriction | One Nation One Subscription (ONOS) |
| Subject Keyword | Peraluminous granitoid Zircon Oxygen isotope Hafnium isotope Neoproterozoic South China Geology Mineral Resources Mineralogy |
| Content Type | Text |
| Resource Type | Article |
| Subject | Geochemistry and Petrology Geophysics |
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