| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4723556 | Precambrian Research | 2012 | 15 Pages |
Abstract
⺠The ca. 2.7 Ga leucogranitoids were mainly derived from local TTGs. ⺠The compositional scatter, in both major and trace-elements is considerable. ⺠Melting was caused by thickening of the crust in response to collisional tectonics. ⺠Melting occurred under water-fluxed conditions. ⺠Potential fluid sources are lower crust and late mantle derived intrusives.
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Authors
Perttu Mikkola, Laura S. Lauri, Asko Käpyaho,