- Names
-
- A. Shatskiy
- P. N. Gavryushkin
- I. S. Sharygin
- K. D. Litasov
- I. N. Kupriyanov
- Y. Higo
- Y. M. Borzdov
- K.-I. Funakoshi
- Y. N. Palyanov
- E. Ohtani
- Title
- Melting and subsolidus phase relations in the system Na2CO3-MgCO3 H2O at 6 GPa and the stability of Na2Mg(CO3)2 in the upper mantle
- Abstract
- Phase relations in the Na2CO3-MgCO3 system have been studied in high-pressure high-temperature (HPHT) multi-anvil experiments using graphite capsules at 6.0 ± 0.5 GPa pressures and 900–1400 °C temperatures. Sub-solidus assemblages are represented by Na2CO3+Na2Mg(CO3)2 and Na2Mg(CO3)2+MgCO3, with the transition boundary near 50 mol% MgCO3 in the system. The Na2CO3-Na2Mg(CO3)2 eutectic is established at 1200 °C and 29 mol% MgCO3. Melting of Na2CO3 occurs between 1350 and 1400 °C. We propose that Na2Mg(CO3)2 disappears between 1200 and 1250 °C via congruent melting. Magnesite remains as a liquidus phase above 1300 °C. Measurable amounts of Mg in Na2CO3 suggest an existence of MgCO3 solid-solutions in Na2CO3 at given experimental conditions. The maximum MgCO3 solubility in Na-carbonate of about 9 mol% was established at 1100 and 1200 °C. The Na2CO3 and Na2Mg(CO3)2 compounds have been studied using in situ X‑ray coupled with a DIA-type multi-anvil apparatus. The studies showed that eitelite is a stable polymorph of Na2Mg(CO3)2 at least up to 6.6 GPa and 1000 °C. In contrast, natrite, γ-Na2CO3, is not stable at high pressure and is replaced by β-Na2CO3. The latter was found to be stable at pressures up to 11.7 GPa at 27 °C and up to 15.2 GPa at 1200 °C and temperatures at least up to 800 °C at 2.5 GPa and up to 1000 °C at 6.4 GPa. The X‑ray and Raman study of recovered samples showed that, under ambient conditions, β-Na2CO3 transforms back to γ-Na2CO3. Eitelite [Na2Mg(CO3)2] would be an important mineral controlling insipient melting in subducting slab and upwelling mantle. At 6 GPa, melting of the Na2Mg(CO3)2+MgCO3 assemblage can be initiated, either by heating to 1300 °C under “dry” conditions or at 900–1100 °C under hydrous conditions. Thus, the Na2Mg(CO3)2 could control the solidus temperature of the carbonated mantle under “dry” conditions and cause formation of the Na- and Mg-rich carbonatite melts similar to those found as inclusions in olivines from kimberlites and the deepest known mantle rock samples—sheared peridotite xenoliths (190–230 km depth).
- Keywords
- Raman spectroscopy, Raman spectra, X-ray, band position, high pressure, phase diagram, mineral, carbonate, magnesite, eitelite, natrite, Na2CO3, MgCO3, Na2Mg(CO3)2, Mn
- Content
- spectral data, band list data, experimental physics, earth sciences
- Year
- 2013
- Journal
- American Mineralogist
- Volume
- 98
- Number
- 11-12
- Pages
- 2172 - 2182
- Pages number
- 11
- Document type
- article
- Publication state
- published
- Doi
- 10.2138/am.2013.4418
- Identifiers
-
- bibcode: 2013AmMin..98.2172S