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On thermochemical mantle plumes with an intermediate thermal power that erupt on the Earth’s surface

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Abstract

The relative plume thermal power Ka = N/N 1 is used (N is the thermal power transferred from the plume base to its conduit and N 1 is the thermal power transferred from the plume conduit into the surrounding mantle in the steady-state heat conduction regime). Thermochemical mantle plumes with small (Ka < 1.15) and intermediate (1.15 < Ka < 1.9) thermal powers are formed at the core–mantle boundary beneath cratons in the absence of horizontal free-convection mantle flows beneath them, or in the presence of weak horizontal mantle flows. Thermochemical plumes reach the Earth’s surface when their relative thermal power is Ka > 1.15. The thermal and hydrodynamical structure of the plume conduit ascending from the core–mantle interface to the level from which the magmatic melt erupts on the Earth’s surface is presented. The model of two-stage eruption of the melt from the plume conduit to the surface is considered. The critical height of the massif above the plume roof, at which the eruption conduit supplying magmatic melt to the surface forms, is determined. The volume of melt erupting through the eruption conduit to the surface is estimated. The dependence of depth Δx from which the melt is transported to the surface on the plume diameter for a kinematic viscosity of ν = 0.5–2 m2/s is presented. In the case when the value Δx is larger than the depth starting from which diamond is stable (150 km), the melt from the plume conduit can transport diamonds to the Earth’s surface. The melt flow in the eruption conduit is considered as a turbulent flow in a cylindrical duct. The velocity of the melt flow in the eruption conduit and the time for the melt to be transported to the surface from a depth of Δx = 150 km for a kinematic viscosity of the melt in the eruption conduit ν v = 0.01–1 m2/s are determined. Tangential stress on the eruption conduit sidewall is estimated in cases of melt flow both in smooth and rough conduits.

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Authors and Affiliations

  1. Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences, pr. Akademika Koptyuga 3, Novosibirsk, Russia

    A. A. Kirdyashkin & A. G. Kirdyashkin

  2. Novosibirsk State University, ul. Pirogova 2, Novosibirsk, Russia

    A. A. Kirdyashkin

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Original Russian Text © A.A. Kirdyashkin, A.G. Kirdyashkin, 2016, published in Geotektonika, 2016, No. 2, pp. 78–92.

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Kirdyashkin, A.A., Kirdyashkin, A.G. On thermochemical mantle plumes with an intermediate thermal power that erupt on the Earth’s surface. Geotecton. 50, 209–222 (2016). https://doi.org/10.1134/S0016852116020059

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