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| Content Provider | Springer Nature Link |
|---|---|
| Author | Lee, Insung Shin, Dongbok |
| Copyright Year | 2003 |
| Abstract | CO$_{2}$-rich fluid inclusions from quartz veins provide information about pressure-temperature conditions, as well as effervescence, in the gold-silver-bearing quartz veins in the Phuoc Thanh area, Central Vietnam. Homogenization temperatures of fluid inclusion are bimodal, and support textural evidence that mineralization occurred in two stages. 90% of the fluid inclusions in the quartz are CO$_{2}$-bearing. The trimodal distribution of CO$_{2}$ mole fraction of the inclusions are common in the area, which indicates the CO$_{2}$ unmixing, resulting the separation of the high (type IIb) and low (type IIa1) XCO$_{2}$ fluids from the parental fluid (type IIa2) with intermediate XCO$_{2}$. The precipitation of associated sulfide and Au−Ag minerals is related to CO$_{2}$ effervescence with a concomitant decrease in sulfur activity. The temperature of mineralization is estimated as the range from 300 to 380°C in stage I and from 230 to 300°C in stage II. Pressure of ore formation ranged from 350 to 500 bars during both stages. |
| Starting Page | 21 |
| Ending Page | 26 |
| Page Count | 6 |
| File Format | |
| ISSN | 12264806 |
| Journal | Geosciences Journal |
| Volume Number | 7 |
| Issue Number | 1 |
| e-ISSN | 15987477 |
| Language | English |
| Publisher | Springer-Verlag |
| Publisher Date | 2003-01-01 |
| Publisher Place | Berlin, Heidelberg |
| Access Restriction | One Nation One Subscription (ONOS) |
| Subject Keyword | fluid inclusion carbon dioxide Au Ag quartz vein effervescence Vietnam Geosciences |
| Content Type | Text |
| Resource Type | Article |
| Subject | Earth and Planetary Sciences Environmental Science |
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