| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 8910441 | Chemical Geology | 2018 | 34 Pages |
Abstract
If Au concentrations in natural, quartz-hosted fluid inclusions from magmatic-hydrothermal ore deposits are affected, then they likely lost Au rather than gained it. At temperatures below 400 °C diffusional loss or gain of Au is considered unlikely in magmatic-hydrothermal systems, but potentially was significant in samples from orogenic Au gold deposits.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Haihao Guo, Andreas Audétat,