Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
6438241 | Geochimica et Cosmochimica Acta | 2014 | 58 Pages |
Abstract
This new understanding has implications for the interpretation of solids within fluid inclusions (e.g., Ti- and Al-minerals) and for the elemental analysis of hydrothermal and metamorphic quartz and its fluid inclusions by microbeam methods such as LA-ICPMS and SIMS. As Ti is a common trace element in quartz, its sequestration by fluid inclusions and its depletion in zone-refined patches impacts on applications of the Ti-in-quartz geothermometer.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Glenn Lambrecht, Larryn William Diamond,