Fragmentation in kimberlite: products and intensity of explosive eruption |
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| Authors: | Stephen Moss J K Russell |
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| Institution: | (1) Volcanology and Petrology Laboratory, Department of Earth and Ocean Sciences, The University of British Columbia, 6339 Stores Road, Vancouver, BC, V6T 1Z4, Canada;(2) Mineral Services Canada Inc., 205-930 Harbourside Drive, North Vancouver, BC, V7P 3S7, Canada;(3) Mineral Deposit Research Unit, Department of Earth and Ocean Sciences, The University of British Columbia, 6339 Stores Road, Vancouver, BC, V6T 1Z4, Canada |
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| Abstract: | The explosive eruption of kimberlite magma is capable of producing a variety of pyroclast sizes, shapes, and textures. However,
all pyroclastic deposits of kimberlite comprise two main types of pyroclasts: (1) pyroclasts of kimberlite with or without
enclosed olivine crystals and (2) olivine crystals which lack coatings of kimberlite. Here, we propose two hypotheses for
how kimberlite magmas are modified due to explosive eruption: (1) olivine crystals break during kimberlite eruption, and (2)
kimberlite melt can be efficiently separated from crystals during eruption. These ideas are tested against data collected
from field study and image analysis of coherent kimberlite and fragmental kimberlite from kimberlite pipes at Diavik, NT.
Olivines are expected to break because of rapid pressure changes during the explosive eruption. Disruption of kimberlite magma,
and pyroclast production, is driven by ductile deformation processes, rather than by brittle fragmentation. The extent to
which melt separates from olivine crystals to produce kimberlite-free crystals is a direct consequence of the relative proportions
of gas, melt and crystals. Lastly, the properties of juvenile pyroclasts in deposits of pyroclastic kimberlite are used to
index the relative intensity of kimberlite eruptions. A fragmentation index is proposed for kimberlite eruption based on:
(a) crystal size distributions of olivine and on (b) ratios of selvage-free olivine pyroclasts to pyroclasts of kimberlite
with or without olivine crystals. |
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