期刊
AMERICAN MINERALOGIST
卷 108, 期 4, 页码 709-718出版社
MINERALOGICAL SOC AMER
DOI: 10.2138/am-2022-8403
关键词
Chloride-carbonate; saline HDF; carbonatitic HDF; T-X diagram; Earth's mantle
The phase relations in the NaCl-CaCO3 and NaCl-MgCO3 systems were experimentally studied using a multi-anvil press at 6 GPa and temperatures ranging from 1000 to 1600 degrees C. Both systems were found to have eutectic type phase diagrams, with subsolidus assemblages of halite + aragonite and halite + magnesite. The composition of the halite-aragonite eutectic was determined to be 40 wt% NaCl and 60 wt% CaCO3 at temperatures below 1200 degrees C, while the halite-magnesite eutectic had a composition of 72 wt% NaCl and 28 wt% MgCO3 at 1300 degrees C. Complete miscibility between carbonate and chloride liquids was observed up to 1600 degrees C.
The frequent occurrence of chlorides and carbonates in the form of microinclusions of melts or high-density fluid (HDF) in diamonds and igneous minerals of kimberlites worldwide generates genuine interest in their phase diagrams under pressure. Here, we present the first experimental results on the phase relations in the NaCl-CaCO3 and NaCl-MgCO3 systems at 6 GPa in the range 1000-1600 degrees C performed using a multi-anvil press. We found that both systems have the eutectic type of phase diagrams. The subsolidus assemblages are represented by halite + aragonite and halite + magnesite. Halite-aragonite eutectic is situated just below 1200 degrees C and has a composition of 40 wt% NaCl and 60 wt% CaCO3. Halite-magnesite eutectic is located at 1300 degrees C and has a composition of 72 wt% NaCl and 28 wt% MgCO3. The halite melting point was established at 1500 degrees C. Complete miscibility between carbonate and chloride liquids was observed up to 1600 degrees C. The results support the hypotheses that saline HDF is either a low-temperature derivative or precursor of mantle carbonatite HDF. The data also do not exclude an alternative hypothesis, according to which saline HDF are formed as a result of the reduction of the carbonate component of chloride-containing carbonatite melts to diamond.
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