New model reveals rips in Earth's mantle layer below southern Tibet

July 30, 2018 by Lois Yoksoulian, University of Illinois at Urbana-Champaign
Illinois geology professor Xiaodong Song is a co-author of a new study that suggests rips in the upper mantle layer of the Indian tectonic plate are responsible for the locations of earthquakes and the surface deformation seen in southern Tibet. Credit: L. Brian Stauffer

Seismic waves are helping researchers uncover the mysterious subsurface history of the Tibetan Plateau, possibly lending insight to future earthquake activity in the region.

The specifics of the deep geologic processes that occurred roughly 50 million years ago, when the Indian and Asian tectonics plates collided, have remained elusive. By collecting high-resolution data, geologists have generated a model that provides the clearest picture so far of the geology below the surface of the Tibetan Plateau. They report their findings in the Proceedings of the National Academy of Sciences.

"The continental collision between the Indian and Asian tectonic plates shaped the landscape of East Asia, producing some of the deadliest earthquakes in the world," said Xiaodong Song, a geology professor at the University of Illinois and co-author of the new study. "However, the vast high is largely inaccessible to geological and geophysical studies."

Song and his colleagues reveal that the upper mantle layer of the Indian tectonic plate appears to be torn into four pieces that dive under Asia—each at a different angle and distance from the origin of the tear.

The team gathered geophysical data from various sources to generate seismic wave tomographic images of Tibet that extend roughly 160 kilometers deep. They found that these newly modeled images match well with historic earthquake activity and with geological and geochemical observations.

Seismic wave velocity images of the Tibetan Plateau in image a (map view) and image b (cross-section view). In image b, T1, T2 and T3 mark mantle tears, the circles indicate earthquakes deeper than 40 kilometers and the white contours show earthquake density. Credit: Graphic courtesy Xiaodong Song
"The presence of these tears helps give a unified explanation as to why mantle-deep earthquakes occur in some parts of southern and central Tibet and not others," Song said.

The intact regions of crust between the tears are strong enough to accumulate strain to generate earthquakes. The crustal areas above the torn regions are exposed to more of the heat from the mantle and are therefore more ductile, the researchers said. That ductile flexibility makes warmer crust less susceptible to earthquakes.

"What were previously thought of as unusual locations for some of the intercontinental earthquakes in the southern Tibetan Plateau seem to make more sense now after looking at this model," said graduate student and co-author Jiangtao Li. "There is a striking correlation with the location of the earthquakes and the orientation of the fragmented Indian upper mantle."

The model also explains some of the deformation patterns seen at the surface, including a series of unusual north-south rifts. Together, the earthquake locations and deformation patterns are evidence of a strongly coupled crust and upper in southern Tibet, the researchers said.

Armed with this new information, geoscientists now have a clearer picture of what role the Indian plays in shaping the Tibetan Plateau and why earthquakes happen where they do in this region. This could help assess earthquake risk, the researchers said.

"Overall, our new research suggests that we need to take a deeper view to understand the Himalayan-Tibetan continental deformation and evolution," Song said.

Explore further: Strength of tectonic plates may explain shape of the Tibetan Plateau, study finds

More information: Jiangtao Li et al, Tearing of Indian mantle lithosphere from high-resolution seismic images and its implications for lithosphere coupling in southern Tibet, Proceedings of the National Academy of Sciences (2018). DOI: 10.1073/pnas.1717258115

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