Do tectonic plates move because of movement in the Earth’s mantle, or is the mantle driven by the movement of the plates?

Image of the numerical solution at the moment when a supercontinent begins to break up. Source: Nicolas Coltice

International scientists: its both forces at different parts of the planet’s surface and this balance of forces changes over geological time

Which forces drive tectonic plates? This has remained an open question ever since the advent of plate tectonic theory 50 years ago. Do the cold edges of plates slowly sinking into the Earth’s mantle at subduction zones cause the motion observed at the Earth’s surface? Or alternatively, does the mantle, with its convection currents, drive the plates? For geologists, this is rather like the problem of the chicken and the egg: the mantle apparently causes the plates to move, while they in turn drive the mantle…

To shed light on the forces at work, scientists from the Geology Laboratory of the École Normale Supérieure (CNRS/ENS – PSL), the Institute of Earth Sciences (CNRS/Universities Grenoble Alpes and Savoie Mont Blanc/IRD/Ifsttar) and the University of Rome 3 treated the solid Earth as a single indivisible system and carried out the most comprehensive modelling to date of the evolution of a fictional planet very similar to the Earth. The scientists first had to find the appropriate parameters, and then spend some 9 months solving a set of equations with a supercomputer, reconstructing the evolution of the planet over a period of 1.5 billion years.

In the image on the left, the modelled fictional planet looks much like the Earth: its surface and mantle move spontaneously, at speeds close to those observed on Earth. The distribution of the plates (some of which are large, while many are small) is also similar, as is the topography: red hues represent shallow regions of the ocean (ridges), while blue indicates the deep seafloor. The deepest blue areas correspond to subduction trenches (where a plate is sinking into the mantle). The continents are shown in translucent white (and therefore appear purplish grey). The image on the right shows warm currents (plumes) rising from the bottom of the mantle. Source: Nicolas Coltice

Using this model, the team showed that 2 thirds of the Earth’s surface moves faster than the underlying mantle, in other words it is the surface that drags the interior, while the roles are reversed for the remaining third. This balance of forces changes over geological time, especially for the continents.

The latter are mainly dragged by deep motion within the mantle during the construction phases of a supercontinent, as in the ongoing collision between India and Asia: in such cases, the motion observed at the surface can provide information about the dynamics of the deep mantle. Conversely, when a supercontinent breaks up, the motion is mainly driven by that of the plates as they sink down into the mantle.

The computation contains a wealth of data that remains largely unexploited. The data obtained could help us to understand how mid-ocean ridges form and disappear, how subduction is triggered, or what determines the location of the plumes that cause vast volcanic outpourings.

Source: Science Advances

* Formation of a supercontinent
* Breakup of a supercontinent

(12.11.2019, USA: 11.12.2019)