Origin of megacrysts by carbonate-bearing metasomatism: A case study for the Muskox kimberlite, Slave craton, Canada.

• Main Authors: Cone, Dylan, Kopylova, Maya
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: Geological Society of London 2021
• Subjects: Geology; FOS Earth and related environmental sciences; Canada; muskox
• Online Access: https://dx.doi.org/10.6084/m9.figshare.c.5255825.v2; https://geolsoc.figshare.com/collections/Origin_of_megacrysts_by_carbonate-bearing_metasomatism_A_case_study_for_the_Muskox_kimberlite_Slave_craton_Canada_/5255825/2

Low-Cr and high-Cr clinopyroxene, garnet, olivine, and ilmenite megacrysts from the Muskox kimberlite (Canada) were analyzed for major and trace elements, as well as Sr, Nd, and Pb isotopes. Samples display compositional overlap with respective phases in websterites, while clinopyroxene isotope systematics reveal similarities with both websteritic and metasomatic clinopyroxene in peridotites from the same kimberlite, in addition to Muskox and Jericho kimberlites. All lithologies may represent the products of mixing between EM1 mantle, relic Proterozoic enriched mantle and HIMU carbonatitic fluid. Equilibrium melts calculated from clinopyroxene trace element data using experimental distribution coefficients for feasible proto kimberlitic melts yield a range of metasomatic agents. Conclusion on the carbonate bearing nature of the metasomatism is based on the presence of a HIMU isotopic signature and results obtained from thermodynamic modeling using the Deep Earth Water model. Modelling was carried out with three fluid compositions; asthenospheric, eclogitic and kimberlitic. Our results suggest mineral compositions analogous to megacrysts cannot be produced by metasomatism of mantle peridotite by carbonate-free hydrous fluids. Isotope systematics argue against a strictly cognate relationship between megacrysts and their host kimberlite, instead suggesting megacrysts and websterites may represent products of regional metasomatism by carbonatitic HIMU fluids shortly predating kimberlite magmatism.