U of T news
  • Follow U of T News


U of T geophysicists uncover new evidence for an alternative style of plate tectonics

A cave city in volcanic rocks of uplifted Central Anatolian plateau (photo by Russell Pysklywec)

Canadian-Turkish collaboration reveals an event of active “drip” tectonics

When renowned University of Toronto geophysicist J. Tuzo Wilson cemented concepts in the emerging field of plate tectonics in the 1960s, he revolutionized the study of Earth’s physical characteristics and behaviours. Decades later, successor researchers at U of T and Istanbul Technical University have determined that a series of volcanoes and a mountain plateau across central Turkey formed not solely by the collision of tectonic plates, but instead by a massive drip and then detachment of the lower tectonic plate beneath Earth’s surface.

“Plate tectonics has stood for more than 50 years as the fundamental model for understanding activity that shapes our planet’s rock surface, though gaps in understanding how this activity is connected with processes below the surface have remained,” said Russell Pysklywec, chair of the department of Earth sciences at U of T and co-author of a study published this month in Nature Communications.

“One thing that is certain, however, is that Earth is always active and we are just beginning to understand how it works.”

Interested in publicly funded research in Canada? Learn more at UofT’s #supportthereport advocacy campaign

The researchers propose that the reason the Central Anatolian (Turkish) Plateau has risen by as much as one kilometre over the past 10 million years is because the planet’s crust and upper mantle – the lithosphere – has thickened and dripped below the region. As the lithosphere sank into the lower mantle, it first formed a basin at the surface, which later sprang up when the weight below broke off and sank further into the deeper depths of the mantle.

“It seems the heavy base of the tectonic plate has ‘dripped’ off into the mantle, leaving a massive gap in the plate beneath Central Anatolia. Essentially, by dropping this dense lithospheric anchor, there has been an upward bobbing of the entire land mass across hundreds of kilometres,” said Oğuz H. Gӧğüş of the Eurasia Institute of Earth Sciences at Istanbul Technical University (ITU), lead author of  the study.

It’s a new idea where plate shortening initially squeezed and folded a mountain belt, triggering the thickening and dripping of the deep lithosphere, and then increasing the elevation of most of central Turkey. Puzzled by the presence of such a process at a significant distance away from regular plate tectonic boundaries, the research team set about identifying why, in an area of high heating and high elevation, is the lithosphere below completely gone – something that was recently discovered from seismology.

Time slices of the computational geodynamic model showing dripping continental root and eventual surface uplift over a 4.5 million year period (U of T handout)

They tested high-performance computational models against known geological and geophysical observations of the Central Anatolian Plateau, and demonstrated that a drip of lithospheric material below the surface can account for the measured elevation changes across the region.

“It’s a new variation on the fundamental concepts of plate tectonics,” said Pysklywec. “It gives us some insight into the connection between the slow circulation of near-solid rock in Earth’s mantle caused by convection currents carrying heat upwards from the planet’s interior, and observed active plate tectonics at the surface.

“This is part of the holy grail of plate tectonics – linking the two processes to understand how the crust responds to the mantle thermal engine of the planet.”

Pysklywec carried out the study with Gӧğüş, who received his PhD from U of T in 2010, and fellow researchers at ITU including Professor A. M. C. Şengӧr, and Erkan Gün of the Eurasia Institute of Earth Sciences at Istanbul Technical Institute. Gün is also now a current graduate student at U of T, supervised by Pysklywec. The research adds to decades of groundbreaking work in plate tectonics at U of T, and builds on Wilson’s seminal work.

Read the research in Nature Communications

“Tuzo Wilson is a towering figure in geophysics internationally and the person most responsible for pioneering the ideas of plate tectonics in the 1960s,” said Pysklywec. “I am pleased that we are continuing his legacy in geophysics with our work.”

While Pysklywec notes there are many locations on Earth missing its lithosphere below, he is quick to reassure that no place is in imminent danger of sinking into the mantle or boosting upwards overnight. “Our results show that the Central Anatolian Plateau rose over a period of millions of years. We’re talking about mantle fluid motions and uplift at the pace at which fingernails grow.”

Gӧğüş highlights the links of the tectonics with human history saying, “The findings are exciting also because of the link with the remarkable historical human activity of Central Anatolia where some of the earliest known civilizations have existed. For example, Central Anatolia is described as an elevated, dry, cold plain of Lycaonia in Strabo’s Geographica in 7 BC, and even cave paintings in the region dating to approximately 7000 BC record active volcanic eruptions on the plateau.”

The study, titled Drip Tectonics and the enigmatic uplift of the Central Anatolian Plateau, was published Nov. 16 in Nature Communications. The research was made possible with support from the Scientific and Technological Research Council of Turkey (TUBITAK), Istanbul Technical University, and the Natural Sciences and Engineering Research Council of Canada (NSERC).