Fluids in the peridotite–water system up to 6 GPa and 800°C: new experimental constrains on dehydration reactions

• Published in: Contributions to mineralogy and petrology 2011-06, Vol.161 (6), p.829-844
• Main Authors: Dvir, O., Pettke, T., Fumagalli, P., Kessel, R.
• Format: Article
• Language: English
• Subjects: Dehydration; Earth and Environmental Science; Earth Sciences; Fluid dynamics; Geology; Geophysics; Mineral Resources; Mineralogy; Original Paper; Petrology; Silicates; Solutes
• ISSN: 0010-7999; 1432-0967
• DOI: 10.1007/s00410-010-0567-2

The phase assemblages and compositions in a K-free lherzolite + H 2 O system were determined between 4 and 6 GPa and 700–800°C, and the dehydration reactions occurring at subarc depth in subduction zones were constrained. Experiments were performed on a rocking multi-anvil apparatus using a diamond-trap setting. The composition of the fluid phase was measured using the recently developed cryogenic LA–ICP–MS technique. Results show that, at 4 GPa, the aqueous fluid coexisting with residual lherzolite (~85 wt% H 2 O) doubles its solute load when chlorite transforms to the 10-Å phase between 700 and 750°C. The 10-Å phase breaks down at 4 and 5 GPa between 750 and 800°C and at 6 GPa between 700 and 750°C, leaving a dry lherzolite coexisting with a fluid phase containing 58–67 wt% H 2 O, again doubling the total dissolved solute load. The fluid fraction in the system increases from 0.2 when a hydrous mineral is present to 0.4 when coexisting with a dry lherzolite. Our data do not reveal the presence of a hydrous peridotite solidus below 800°C. The directly measured fluid compositions demonstrate a fundamental change in the (MgO + FeO) to SiO 2 mass ratio of fluid solutes occurring at a depth of ca. 120–150 km (in the temperature window of 700–800°C), from (MgO–FeO)-dominated at 4 GPa [with (MgO + FeO)/SiO 2 ratio of 1.41–1.56] to SiO 2 -dominated at 5–6 GPa (ratios of 0.61–0.82). The mobility of Al 2 O 3 increases by more than one order of magnitude across this P–T interval and demonstrates that Al 2 O 3 is compatible in an aqueous fluid coexisting with the anhydrous ol-opx-cpx ± grt assemblage. This shift in the fluid composition correlates with changes in the phase assemblage of the residual silicates. The hitherto unknown fundamental change in (MgO + FeO)/SiO 2 ratio and prominent increase in Al 2 O 3 of the aqueous fluid with progressive subduction will likely inspire novel concepts on mantle wedge metasomatism by slab fluids.