logo
    Diamondiferous garnet harzburgites from the Finsch kimberlite, Northern Cape, South Africa
    Contributions to Mineralogy and Petrology (1992)
    Fanus ViljoenP. M. SwashM OtterD. J. SchulzeP. J. LAWLESS
    42
    Citation
    22
    Reference
    10
    Related Paper
    Citation Trend
    Keywords:
    Xenolith
    Peridotite
    Mineral resource classification
    Phlogopite
    Topics:
    Geological and Geochemical Analysis
    earthquake and tectonic studies
    High-pressure geophysics and materials
    The geology and mineralogy of the Anuri kimberlite, Nunavut, Canada
    Lithos (2004)
    K.M. MasunBuddy DoyleS. BallSamuel Walker
    Xenolith
    Phlogopite
    Lapilli
    Diatreme
    Country rock
    Citations (21)
    Phlogopite-rich and phlogopite-poor kimberlite intrusions within the Du Toitspan kimberlite pipe, South Africa: Petrogenetic relationships and localised source heterogeneity
    Lithos (2021)
    Lesego RamokgabaAnton le RoexJock Robey
    Phlogopite
    Country rock
    Citations (3)
    Mineralogy of Peridotite Xenoliths from the Komsomol’skaya–Magnitnaya Kimberlite Pipe (Upper Muna Field, Siberian Craton)
    Doklady Earth Sciences (2022)
    I. V. YakovlevV. G. MalkovetsА. А. ГибшерА. M. DymshitsD. V. Kuzmin
    Peridotite
    Xenolith
    Metasomatism
    Chromite
    Phlogopite
    Carbonatite
    Citations (0)
    The Pipe-15 kimberlite: A new addition to the Wajrakarur cluster of the Wajrakarur kimberlite field, Eastern Dharwar craton, Southern India
    Journal of the Geological Society of India (2015)
    Ashish DongreFanus ViljoenM. Malandkar
    Dharwar Craton
    Citations (3)
    Some petrological aspects of the Prairie Creek diamond-bearing kimberlite diatreme, Arkansas
    Contributions to Mineralogy and Petrology (1978)
    Subbarayudu V. GogineniCharles E. MeltonA. A. Giardini
    Diatreme
    Phlogopite
    Xenolith
    Breccia
    Phenocryst
    Ultramafic rock
    Mineral redox buffer
    Diopside
    Citations (24)
    Statistical Comparison between Pyroxenes from Kimberlites and Their Associated Xenoliths
    The Journal of Geology (1977)
    W. E. StephensJ. B. Dawson
    Cluster analysis of 458 pyroxenes from kimberlites, associated xenoliths and diamonds has allowed recognition of 5 chemically distinct orthopyroxene groups and 10 distinct clinopyroxene groups from the $$TiO_{2}, Al_{2}O_{3}, Cr_{2}O_{3}$$, FeO, MgO, CaO, and $$Na_{2}O$$ contents. Names assigned to these groups convey their distinctive chemical features. Because many groups contain cases from both kimberlite and xenoliths, some kimberlite pyroxenes may derive from fragmented xenoliths. However from size alone, large discrete orthopyroxene crystals, discrete sub-calcic diopside nodules and low-Cr diopsides intergrown with ilmenite are apparently not xenolithic; nor are the minute diopside crystals growing in the kimberlite matrix. Pyroxene inclusions in diamonds and pyroxenes coexisting with diamond in eclogite and peridotite xenoliths range widely in chemical composition.
    Xenolith
    Diopside
    Pyroxene
    Ilmenite
    Peridotite
    Pyrope
    Citations (59)
    The geology and mineralogy of the Anuri kimberlite, Nunavut, Canada
    Lithos (2004)
    K MASUN
    Phlogopite
    Xenolith
    Lapilli
    Diatreme
    Country rock
    Citations (1)
    Constraints on kimberlite ascent mechanisms revealed by phlogopite compositions in kimberlites and mantle xenoliths
    Lithos (2015)
    Andrea GiulianiDavid PhillipsVadim S. KamenetskyKarsten Goemann
    Phlogopite
    Xenolith
    Citations (136)
    Kimberlite age in the Arkhangelsk Province, Russia: Isotopic geochronologic Rb–Sr and 40Ar/39Ar and mineralogical data on phlogopite
    Petrology (2016)
    Yu. О. LarionovaЛ. В. СазоноваNataliya LebedevaА. А. НосоваV.V. Tretyachenko
    Phlogopite
    Xenolith
    Phenocryst
    Diatreme
    Citations (39)
    Xenoliths of phlogopite-bearing rocks in kimberlites of Yakutia
    International Geology Review (1980)
    A. D. Khar'kivD. I. Savrasov
    Phlogopite
    Xenolith
    Citations (0)