Details
| Original language | English |
|---|---|
| Pages (from-to) | 1299-1306 |
| Number of pages | 8 |
| Journal | Mineralium deposita |
| Volume | 55 |
| Issue number | 7 |
| Early online date | 19 Dec 2019 |
| Publication status | Published - Oct 2020 |
Abstract
The solubility of scheelite in evolved granitic magmas (Qz-Ab-Or-An system with minor FeOtotal, TiO2, and CaO added) was studied experimentally at 200 MPa, 750–850 °C and relatively oxidizing condition (logfO2 = NNO + 2.3, where NNO is Ni-NiO oxygen buffer). Water-saturated granitic melts have been equilibrated with seeds of scheelite crystals. The resulted WO3 contents in the melts vary only slightly from 0.21 to 0.32 wt.% WO3 over the investigated temperature and compositional range (0.7 to 1.4 wt.% CaO) but tends to increase with increasing temperature and decreasing CaO concentration. One important message conveyed from the study is that WO3 concentrations at scheelite saturation are more dependent on temperature in evolved Ca-poor melts than in Ca-rich melts. Natural granitic rocks associated with scheelite mineralization and associated melt inclusions hosted in quartz have much lower W contents than the experimental melts equilibrated with scheelite. This implies that enrichment of tungsten (W) at magmatic stages is not sufficient to produce significant scheelite mineralization and confirms the important role of W mobilization by magmatic-hydrothermal fluids in the formation of scheelite deposits.
Keywords
- Experiment, Mineralization, Protracted enrichment, Scheelite, Solubility, Tungsten
ASJC Scopus subject areas
- Earth and Planetary Sciences(all)
- Geophysics
- Earth and Planetary Sciences(all)
- Geochemistry and Petrology
- Earth and Planetary Sciences(all)
- Economic Geology
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In: Mineralium deposita, Vol. 55, No. 7, 10.2020, p. 1299-1306.
Research output: Contribution to journal › Article › Research › peer review
}
TY - JOUR
T1 - Experimental evidence for a protracted enrichment of tungsten in evolving granitic melts
T2 - implications for scheelite mineralization
AU - Wang, Meng
AU - Deng, Jun
AU - Hou, Tong
AU - Derrey, Insa T.
AU - Botcharnikov, Roman E.
AU - Liu, Xi
AU - Zhang, Chao
AU - Qi, Dong Mei
AU - Zhang, Zhaochong
AU - Holtz, François
N1 - Funding information: J. D. was supported by the Major Research Project of the National Natural Science Foundation of China (NSFC Project; 91855217). M.W. and T.H. were supported by 2016FC0600502 and China Nature Foundation of Sciences (41761134086; 41922012), MOST Special Fund from the State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences (MSFGPMR201804 and MSFGPMR201809) and 111 Project (B18048). X. L was supported by the DREAM project of MOST, China (2016YFC0600408).
PY - 2020/10
Y1 - 2020/10
N2 - The solubility of scheelite in evolved granitic magmas (Qz-Ab-Or-An system with minor FeOtotal, TiO2, and CaO added) was studied experimentally at 200 MPa, 750–850 °C and relatively oxidizing condition (logfO2 = NNO + 2.3, where NNO is Ni-NiO oxygen buffer). Water-saturated granitic melts have been equilibrated with seeds of scheelite crystals. The resulted WO3 contents in the melts vary only slightly from 0.21 to 0.32 wt.% WO3 over the investigated temperature and compositional range (0.7 to 1.4 wt.% CaO) but tends to increase with increasing temperature and decreasing CaO concentration. One important message conveyed from the study is that WO3 concentrations at scheelite saturation are more dependent on temperature in evolved Ca-poor melts than in Ca-rich melts. Natural granitic rocks associated with scheelite mineralization and associated melt inclusions hosted in quartz have much lower W contents than the experimental melts equilibrated with scheelite. This implies that enrichment of tungsten (W) at magmatic stages is not sufficient to produce significant scheelite mineralization and confirms the important role of W mobilization by magmatic-hydrothermal fluids in the formation of scheelite deposits.
AB - The solubility of scheelite in evolved granitic magmas (Qz-Ab-Or-An system with minor FeOtotal, TiO2, and CaO added) was studied experimentally at 200 MPa, 750–850 °C and relatively oxidizing condition (logfO2 = NNO + 2.3, where NNO is Ni-NiO oxygen buffer). Water-saturated granitic melts have been equilibrated with seeds of scheelite crystals. The resulted WO3 contents in the melts vary only slightly from 0.21 to 0.32 wt.% WO3 over the investigated temperature and compositional range (0.7 to 1.4 wt.% CaO) but tends to increase with increasing temperature and decreasing CaO concentration. One important message conveyed from the study is that WO3 concentrations at scheelite saturation are more dependent on temperature in evolved Ca-poor melts than in Ca-rich melts. Natural granitic rocks associated with scheelite mineralization and associated melt inclusions hosted in quartz have much lower W contents than the experimental melts equilibrated with scheelite. This implies that enrichment of tungsten (W) at magmatic stages is not sufficient to produce significant scheelite mineralization and confirms the important role of W mobilization by magmatic-hydrothermal fluids in the formation of scheelite deposits.
KW - Experiment
KW - Mineralization
KW - Protracted enrichment
KW - Scheelite
KW - Solubility
KW - Tungsten
UR - http://www.scopus.com/inward/record.url?scp=85077019470&partnerID=8YFLogxK
U2 - 10.1007/s00126-019-00932-1
DO - 10.1007/s00126-019-00932-1
M3 - Article
AN - SCOPUS:85077019470
VL - 55
SP - 1299
EP - 1306
JO - Mineralium deposita
JF - Mineralium deposita
SN - 0026-4598
IS - 7
ER -