Multistage Mantle Metasomatism during the Generation of Kimberlite Melts: Evidence from Mantle Xenoliths and Megacrysts of the Grib Kimberlite, Arkhangelsk, Russia
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Peridotite
Metasomatism
Xenolith
Phlogopite
Ultramafic rock
Primitive mantle
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Phlogopite
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In this study, we compare the major- and trace-element compositions of olivine, garnet, and clinopyroxene that occur as single crystals (142 grains), with those derived from xenoliths (51 samples) from six kimberlites in the Lucapa area, northeastern Angola: Tchiuzo, Anomaly 116, Catoca, Alto Cuilo-4, Alto Cuilo-63 and Cucumbi-79. The samples were analyzed using electron probe microanalysis (EPMA) and laser-ablation inductively coupled plasma-mass spectrometry (LA-ICP-MS). The results suggest different paragenetic associations for these kimberlites in the Lucapa area. Compositional overlap in some of the macrocryst and mantle xenolith samples indicates a xenocrystic origin for some of those macrocrysts. The presence of mantle xenocrysts suggests the possibility of finding diamond. Geothermobarometric calculations were carried out using EPMA data from xenoliths by applying the program PTEXL.XLT. Additional well calibrated single-clinopyroxene thermobarometric calculations were also applied. Results indicate the underlying mantle experienced different equilibration conditions. Subsequent metasomatic enrichment events also support a hypothesis of different sources for the kimberlites. These findings contribute to a better understanding of the petrogenetic evolution of the kimberlites in northeastern Angola and have important implications for diamond exploration.
Xenolith
Metasomatism
Trace element
Primitive mantle
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Metasomatism
Peridotite
Phlogopite
Xenolith
Trace element
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Phlogopite
Country rock
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Diatreme
Phlogopite
Xenolith
Breccia
Phenocryst
Ultramafic rock
Mineral redox buffer
Diopside
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Phlogopite
Xenolith
Lapilli
Diatreme
Country rock
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Phlogopite
Xenolith
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Metasomatism
Xenolith
Amphibole
Anhydrous
Lile
Primitive mantle
Peridotite
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Phlogopite
Xenolith
Phenocryst
Diatreme
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