Earth's crust melts easier than previously thought

March 18, 2009
Mt. Rushmore granite crystallized from a magma that was generated 1.7 billion years ago during collision of smaller tectonic plates that together produced the nucleus of the North American continent. Reduced heat diffusion in colliding and deforming tectonic plates, as reported in the paper, contributed to melting of crustal rocks in the ancient mountain belt, in a manner analogous to granite production in the active Himalayan continental collision. Photo courtesy of Peter Nabelek.

A University of Missouri study published in Nature this week has found that the Earth's crust melts easier than previously thought. In the study, researchers measured how well rocks conduct heat at different temperatures and found that as rocks get hotter in the Earth's crust, they become better insulators and poorer conductors. This finding provides insight into how magmas are formed and will lead to better models of continental collision and the formation of mountain belts.

"In the presence of external heat sources, rocks will heat up more efficiently than previously thought," said Alan Whittington, professor of geological sciences in the MU College of Arts and Science. "We applied our findings to computer models that predict what happens to rocks when they get buried and heat up in mountain belts, such as the Himalayas today or the Black Hills in South Dakota in the geologic past. We found that strain heating, caused by during mountain belt formation, quite easily triggers crustal melting."

In the study, researchers used a laser-based technique to determine how long it took heat to conduct through different samples. In all of the samples, , or how well a material conducts heat, decreased rapidly with increasing temperatures. Researchers found the thermal diffusivity of hot rocks and magmas to be half that of what had been previously assumed.

"Most crustal melting on the Earth comes from intrusions of hot from the Earth's mantle," said Peter Nabelek, professor of geological sciences in the MU College of Arts and Science. "The problem is that during , we don't see intrusions of basaltic magma into continental crust. These experiments suggest that because of low thermal diffusivity, strain heating is much faster and more efficient, and once rocks get heated, they stay hotter for much longer. Of course, these processes take millions of years to occur and we can only simulate them on a computer. This new data will allow us to create computer models that more accurately represent processes that occur during continental collisions."

More information: The study, "Temperature-dependent thermal diffusivity of the Earth's crust and implications for magmatism," was published in this week's Nature and was co-authored by Whittington, Nabelek and Anne Hofmeister, a professor at Washington University.

Source: University of Missouri-Columbia (news : web)

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1 / 5 (6) Mar 18, 2009
2.3 / 5 (3) Mar 18, 2009
^No, no I think you're wrong.
1.5 / 5 (4) Mar 18, 2009
Now we'll have to study 'human induced global melting' ;-)
1 / 5 (2) Mar 19, 2009
Stress and strain heating caused by subduction zones and faulting, are both factors.
not rated yet Apr 29, 2009
You're getting closer!
Now can you imagine what might happen if you eliminated magma wholly from the equation. It is always 'assumed' that the source of heat must tie back to magma. What if...

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