The Fe-Zn Isotopic Characteristics and Fractionation Models: Implications for the Genesis of the Zhaxikang Sb-Pb-Zn-Ag Deposit in Southern Tibet
The genesis of the Zhaxikang Sb-Pb-Zn-Ag deposit remains controversial. Three different geological environments have been proposed to model mineralization: a hot spring, a magmatic-hydrothermal fluid, and a sedimentary exhalative (SEDEX) overprinted by a hot spring. Here, we present the electron pro...
| Príomhchruthaitheoirí: | , , , |
|---|---|
| Formáid: | Alt |
| Teanga: | English |
| Foilsithe / Cruthaithe: |
Wiley
2018-01-01
|
| Sraith: | Geofluids |
| Rochtain ar líne: | http://dx.doi.org/10.1155/2018/2197891 |