Continental crust thanks to the right mixture
For the first time, ETH scientists have successfully recreated the formation of continental crust in the Archean using a computer simulation. The model helps scientists to better understand processes that took place three to four billion years ago.
|Artistic representation of the Earth in the Archean. Stromatolites, the first signs of life, are present in the shallow water |
[Credit: Tim Bertelink/WikiCommons]
In the journal Nature, geophysicists led by Antoine Rozel, a senior assistant at the Institute of Geophysics at ETH Zurich, have now presented a computer model that is likely to add fuel to the scientific debate. With their model, they were able to recreate the origination of earlier continental crust for the first time, something which until now had proven particularly challenging.
Venus or Io?
For their computer model, the researchers took inspiration from two opposing explanatory approaches. One approach postulates that the Archean crustal material was built up through volcanic activity alone, as it has been suggested to happen on Jupiter's moon Io. The other approach, by contrast, assumes that new crust was formed by the accumulation of magma remaining warm in the crust might be the case on Venus.
|Venus, Earth and Io: different modes formed their crusts [Credit: NASA]|
Temperature and pressure narrowly defined
"The rocks of the original continental crust could only form under relatively narrowly defined temperature and pressure conditions. In both extremes, these conditions do not exist," explains Rozel. "If a new crust is formed solely by volcanoes, whereby the magma cools immediately on the Earth's surface, the crust would be too cold. Conversely, the crust in the other approach would be hotter than it should be."
|Archean crust could have been built by vulcanism and accumulation of magma remaining |
warm in the crust [Credit: Antoine Rozel/ETH Zurich]
Two-dimensional and global
For the researchers to calculate their model, however, they had to make some compromises. Although their model is global, it is only two-dimensional. "If we had wanted a high regional resolution and a three-dimensional model, we would have had to run the calculations on a supercomputer for ten years," says Rozel.
In their model, the researchers considered various quantities, such as temperature, pressure, water content of the rock and its viscosity, and simulated the processes up to 100 times to test the parameters with various values.
Author: Peter Rüegg | Source: ETH Zurich [May 10, 2017]