Earths crust melts easier than previously thoughtMarch 19th, 2009 - 11:59 am ICT by ANI
Washington, March 19 (ANI): In a new research, geologists have determined that Earths crust melts easier than previously thought, because rocks in the region become better insulators and poorer conductors as they get hotter.
According to the scientists, the findings provide insights into how magmas are formed, and will lead to better models of continental collision and the formation of mountain belts.
These results shed important light on a geologic question: how large bodies of granite magma can be formed in Earths crust, said Sonia Esperanca, a program director in the National Science Foundation (NSF)s Division of Earth Sciences, which funded the research.
In the presence of external heat sources, rocks heat up more efficiently than previously thought, said geologist Alan Whittington of the University of Missouri.
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, he added.
We found that strain heating, caused by tectonic movements during mountain belt formation, easily triggers crustal melting, he explained.
In the study, the researchers used a laser-based technique to determine how long it took heat to conduct through different rock samples.
In all their samples, thermal diffusivity, or how well a material conducts heat, decreased rapidly with increasing temperatures.
The thermal diffusivity of hot rocks and magmas was half that of what had been previously assumed .
Most crustal melting on Earth comes from intrusions of hot basaltic magma from the Earths mantle, said Peter Nabelek, also a geologist at the University of Missouri. The problem is that during continental collisions, we dont see intrusions of basaltic magma into continental crust, he added.
These experiments suggest that because of low thermal diffusivity, strain heating is much faster and more efficient.
Once rocks get heated, they stay hotter for much longer, Nabelek said.
The new data will allow scientists to create computer models that more accurately represent processes that occur during continental collisions. (ANI)
Tags: basaltic magma, black hills, computer models, continental collision, continental collisions, continental crust, earth sciences, earths mantle, external heat, geologist, heat sources, hot rocks, insulators, intrusions, mountain belts, national science foundation, rock samples, tectonic movements, thermal diffusivity, whittington