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| A view of the bends of the fracture zones on the Southwest Indian Ridge caused by the slowdown of Africa in response to the Reunion plume head. The image shows the gravity field. |
SAN DIEGO — Bringing fresh insight into long-standing debates about how powerful
geological forces shape the planet, from earthquake ruptures to mountain
formations, scientists at Scripps Institution of Oceanography at UC San
Diego have identified a new mechanism driving Earth's massive tectonic
plates.
Scientists who study tectonic motions have known for decades that the
ongoing "pull" and "push" movements of the plates are responsible for
sculpting continental features around the planet. Volcanoes, for
example, are generally located at areas where plates are moving apart or
coming together. Scripps scientists Steve Cande and Dave Stegman have
now discovered a new force that drives plate tectonics: plumes of hot
magma pushing up from Earth's deep interior. Their research is published
in Thursday's (July 7) issue of the journal Nature.
Using analytical methods to track plate motions through Earth's history, Cande and Stegman's research provides evidence that such mantle plume "hot spots," which can last for tens of millions of years and are active today at locations such as Hawaii, Iceland and the Galapagos, may work as an additional tectonic driver, along with push-pull forces.
Their new results describe a clear connection between the arrival of a
powerful mantle plume head around 70 million years ago and the rapid
motion of the Indian plate that was pushed as a consequence of overlying
the plume's location. The arrival of the plume also created immense
formations of volcanic rock now called the "Deccan flood basalts" in
western India, which erupted just prior to the mass extinction of
dinosaurs. The Indian continent has since drifted north and collided
with Asia, but the original location of the plume's arrival has remained
volcanically active to this day, most recently having formed Réunion
island near Madagascar.
The team also recognized that this "plume-push" force acted on other
tectonic plates, and pushed on Africa as well but in the opposite
direction.
"Prior to the plume's arrival, the African plate was slowly drifting but then stops altogether, at the same time the Indian speeds up," explains Stegman, an assistant professor of geophysics in Scripps' Cecil H. and Ida M. Green Institute of Geophysics and Planetary Physics. "It became clear the motion of the Indian and African plates were synchronized and the Réunion hotspot was the common link."
After the force of the plume had waned, the African plate's motion
gradually returned to its previous speed while India slowed down.
"There is a dramatic slow down in the northwards motion of the Indian
plate around 50 million years ago that has long been attributed to the
initial collision of India with the Eurasian plate," said Cande, a
professor of marine geophysics in the Geosciences Research Division at
Scripps. "An implication of our study is that the slow down might just
reflect the waning of the mantle plume-the actual collision might have
occurred a little later."
Funding for the research was provided by the National Science Foundation.
About Scripps Institution of Oceanography
Scripps Institution of Oceanography at University of California, San Diego, is one of the oldest, largest and most important centers for global science research and education in the world. Now in its second century of discovery, the scientific scope of the institution has grown to include biological, physical, chemical, geological, geophysical and atmospheric studies of the earth as a system. Hundreds of research programs covering a wide range of scientific areas are under way today in 65 countries. The institution has a staff of about 1,400, and annual expenditures of approximately $170 million from federal, state and private sources. Scripps operates robotic networks, and one of the largest U.S. academic fleets with four oceanographic research ships and one research platform for worldwide exploration. Learn more at scripps.ucsd.edu. Scripps News: scrippsnews.ucsd.edu

