You may have heard that the Earth’s tectonic plates slide around, but, how do these hard rocks do that?
Scientists from the Scripps Institution of Oceanography discovered a layer of magma in the Earth’s mantle which may be acting as a lubricant to facilitate the slide of tectonic plates. They imaged a 15.5-mile thick layer of partially melted mantle rock below the edge of the Cocos plate where it moves under Central America.
There are two main layers of the mantle. The upper mantle, and the lower mantle. The upper mantle is mostly solid, and the lower mantle is partially molten (extremely viscous/barely liquid).
This lubricant discovery was made at the Middle America trench using electromagnetic imaging technology pioneered at Scripps as part of the SERPENT project.
Scripps Institution of Oceanography / University of California, San Diego
Scientists at Scripps Institution of Oceanography at UC San Diego have found a layer of liquefied molten rock in Earth’s mantle that may be acting as a lubricant for the sliding motions of the planet’s massive tectonic plates. The discovery may carry far-reaching implications, from solving basic geological functions of the planet to a better understanding of volcanism and earthquakes.
The scientists discovered the magma layer at the Middle America trench offshore Nicaragua. Using advanced seafloor electromagnetic imaging technology pioneered at Scripps, the scientists imaged a 25-kilometer- (15.5-mile-) thick layer of partially melted mantle rock below the edge of the Cocos plate where it moves underneath Central America.
The discovery is reported in the March 21 issue of the journal Nature by Samer Naif, Kerry Key, and Steven Constable of Scripps, and Rob Evans of Woods Hole Oceanographic Institution.
The new images of magma were captured during a 2010 expedition aboard the U.S. Navy-owned and Scripps-operated research vessel Melville. After deploying a vast array of seafloor instruments that recorded natural electromagnetic signals to map features of the crust and mantle, the scientists realized they found magma in a surprising place.
“This was completely unexpected,” said Key, an associate research geophysicist in the Cecil H. and Ida M. Green Institute of Geophysics and Planetary Physics at Scripps. “We went out looking to get an idea of how fluids are interacting with plate subduction, but we discovered a melt layer we weren’t expecting to find at all-it was pretty surprising.”
For decades scientists have debated the forces and circumstances that allow the planet’s tectonic plates to slide across the earth’s mantle. Studies have shown that dissolved water in mantle minerals results in a more ductile mantle that would facilitate tectonic plate motions, but for many years clear images and data required to confirm or deny this idea were lacking.
“Our data tell us that water can’t accommodate the features we are seeing,” said Naif, a Scripps graduate student and lead author of the paper. “The information from the new images confirms the idea that there needs to be some amount of melt in the upper mantle and that’s really what’s creating this ductile behavior for plates to slide.”
“This new image greatly enhances our understanding of the role that fluids, both seawater and deep subsurface melts, play in controlling tectonic and volcanic processes,” said Bil Haq, program director in the National Science Foundation’s Division of Ocean Sciences.
The marine electromagnetic technology employed in the study was originated by Charles “Chip” Cox, an emeritus professor of oceanography at Scripps, and in recent years further advanced by Constable and Key. Since 2000 they have been working with the energy industry to apply this technology to map offshore oil and gas reservoirs.
The researchers say their results will help geologists better understand the structure of the tectonic plate boundary and how that impacts earthquakes and volcanism.
“One of the longer-term implications of our results is that we are going to understand more about the plate boundary, which could lead to a better understanding of earthquakes,” said Key.
The researchers are now seeking to find the source that supplies the magma in the newly discovered layer.
The National Science Foundation and the Seafloor Electromagnetic Methods Consortium at Scripps supported the research.
More information about this project and the Scripps Marine Electromagnetics Laboratory is available at:
http://marineemlab.ucsd.edu/Projects/SERPENT
