| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6441172 | Lithos | 2011 | 19 Pages |
Abstract
⺠Granite plutons of the eastern Llano Uplift contain two types of magmatic enclaves. ⺠Type I enclaves are felsic in composition and similar to the host granites. ⺠Type II enclaves (intermediate) are chemically distinct from the host granite. ⺠Type II enclaves may have evolved by RFC processes. ⺠RFC modeling reproduces trace-element trends.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
R.K. Smith, Walt Gray,