Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
8910149 | Chemical Geology | 2018 | 71 Pages |
Abstract
The results of this study show that aqueous fluid saturation can take place at an early stage of pegmatite emplacement, and that magma evolution is matched by changes in the solute chemistry of the exsolving aqueous fluid. They also show that evolution to a more volatile-rich composition (H2Oâ¯+â¯Fâ¯+â¯Li) may have contributed to the increased mobility of later magma batches, thereby helping to explain the regional zonation of the pegmatites, from beryl-type within the pluton to spodumene-type in the adjacent amphibolite.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Thomas Mulja, Anthony E. Williams-Jones,