The composition of texturally primary fluid inclusions and their host phases clinopyroxene, K-richterite, and zircon were investigated in two MARID-type (micaamphibolerutileilmenitediopside) mantle xenoliths sampled by the Kimberley cluster of Cretaceous kimberlites erupted in the central Kaapvaal Craton, South Africa. PT conditions of crystallization for the MARID assemblages of 4.2 GPa and 960 degrees C were estimated based on Ca-in-opx thermometry and the assumption of a 40 mW/m(2) geotherm applied to two orthopyroxene-bearing MARIDs collected from the same locality. Cooling/heating stage measurements and Raman spectroscopy indicate a fluid system dominated by H2O-NaCl-MgCl2 with variable total salinities in the range <= 6.4-32.4 mass% and minor amounts of MgCl2, the latter inferred from the crystallization of MgCl2 x 12H(2)O during cooling of the inclusions. In addition to liquid and vapour, enstatite, baddeleyite, barite, calcite and a KBaFeCr-titanate were identified as solid phases in opened fluid inclusions, indicating high LIL-(HFS) element concentrations in the saline hydrous fluids prior to solid phase precipitation. The Cl contents of apatite (<= 0.35 wt.%), phlogopite (<= 0.09 wt.%) and K-richterite (<= 0.025 wt.%) follow the enrichment pattern Clap >> Clphl > ClKr which is typical for upper mantle rocks. Fluid inclusion-bearing clinopyroxenes show very low H2O contents of 45 mu g/g which is consistent with a reduced aH(2)O of the fluids due to the presence of NaCl-MgCl2-SiO2-LILE combined with high fO(2) and very low Al-3+ contents of the clinopyoxenes. The zircons show a complex compositional zoning with variable and positively correlated Y (<= 1260 mu g/g), P (<= 1870 mu g/g) and Sc (<= 1373 mu g/g) contents, indicating a pretulite-type substitution Si-4+ + Zr-4+ = P-5+ + (Sc, Y, REE)(3)+. The Sc contents of the zircons are amongst the highest Sc concentrations reported so far for upper mantle silicates. Oxygen isotope analyses of selected zircons yields delta O-18 values as high as 6.7 %PLUSMN; 0.2 (2 sigma)parts per thousand and an overall average delta O-18 of 6.1 %PLUSMN; 0.2 parts per thousand which is slightly higher than that of zircon megacryst delta O-18 of 5.3 %PLUSMN; 0.3 parts per thousand reported from worldwide occurrences. The O-isotopic composition of the zircons is consistent with an open-system fractional crystallization of the MARID assemblage in an olivine-absent environment from very small batches of an alkali-rich hydrous saline high-density fluid or fluid-saturated melt. The hydrous saline fluids with LILE-(HFSE)-rich daughter crystals preserved in the two MARID xenoliths indicates that open-system fractional crystallization of MARID-type assemblages can generate small volumes of highly saline hydrous and incompatible trace element-enriched high-density fluids from larger volumes of alkali-rich hydrous melts of group-II kimberlite affinity. MARID crystallization is thought to be just one very specific example of a more general case of open-system crystallization in mantle veins of hydrous silicate-rich assemblages that can concentrate Cl in residual hydrous fluids to brine strength. Inclusions of KClPLILE-rich fluids trapped in diamonds from many locations worldwide provide evidence for a widespread operation of these processes in the subcontinental lithospheric mantle. (C) 2014 Elsevier Ltd. All rights reserved.
