Evolving mantle convection from bottom up to top down.

Ross N Mitchell, Michael Brown, Thomas M Gernon, Christopher J Spencer
Author Information
  1. Ross N Mitchell: State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China.
  2. Michael Brown: Laboratory for Crustal Petrology, Department of Geology, University of Maryland, College Park, MD 20742, USA.
  3. Thomas M Gernon: School of Ocean and Earth Science, University of Southampton, Southampton SO22 4JR, UK.
  4. Christopher J Spencer: Department of Geological Sciences and Geological Engineering, Queen's University, Kingston, ON K7L 2N8, Canada.

Abstract

When it comes to convection, what goes up must come down. Or is it, what goes down must come up? The truth is it depends. Although convection must be mass balanced, there is no reason that it must be force balanced: the positive and negative buoyancy forces driving convection up and down, respectively, do not necessarily need to be balanced. The balance, or imbalance, all depends on the top and bottom boundary layers. Thus, convection in Earth's mantle depends on the temperature differences across the core-mantle boundary below and the lithosphere-asthenosphere boundary above. Convective asymmetry predominated by positive buoyancy, or bottom-up convection, would be driven by plume ascent, whereas if it were predominated by negative buoyancy, or top-down convection, it would be driven by plate subduction. Symmetric convection would balance plume ascent and plate subduction. Is mantle convection on Earth balanced, dominantly top down or bottom up, or time dependent?

Word Cloud

Created with Highcharts 10.0.0convectionmustdependsbalancedbuoyancytopbottomboundarymantlegoescomepositivenegativebalancepredominateddrivenplumeascentplatesubductioncomesup?truthAlthoughmassreasonforcebalanced:forcesdrivingrespectivelynecessarilyneedimbalancelayersThusEarth'stemperaturedifferencesacrosscore-mantlelithosphere-asthenosphereConvectiveasymmetrybottom-upwhereastop-downSymmetricEarthdominantlytimedependent?Evolvingdown

Similar Articles

Cited By (1)