Scientists discover how tectonic plates collide

September 9, 2015 by Charlotte Anscombe, University of Nottingham
Scientists discover how tectonic plates collide

Researchers have discovered how tectonic plates first collided in one of the world's largest deep sea trenches.

One of the biggest questions yet to be answered about plate tectonics is how do start? A subduction zone is a deep trough cut across the ocean floor. They form when two tectonic plates collide and one of the plates is pushed under another as they move towards each other, creating an ocean trench.

When the collide the underlying plate is consumed into the Earth's mantle, creating a hot magma that erupts from volcanoes on the surface of the overlying plate. These volcanoes form a volcanic arc.

The Izu-Bonin-Mariana Arc

There are examples of this kind of natural occurrence all across the globe. One is the Izu-Bonin-Mariana Arc (IBM), an extinct arc bordering a trench zone south of Japan.

In a new paper published in Nature Geoscience, a team of 30 scientists from across the globe travelled to the Philippine Sea during the summer of 2014 on a large drillship called the JOIDES Resolution operated by the International Ocean Discovery Programme, to drill into the of the IBM arc and to try to find out what had caused the plates to collide.

Dr Sev Kender a Research Fellow in the School of Geography at The University of Nottingham, was one of the team of 30 who went out on the trip.

Dr Kender says: "Plate tectonics and seafloor spreading was a ground-breaking theory discovered in the mid-20th-Century that explained much of geology, and started our modern discipline today. Before it there was no single accepted theory of why oceans and mountains formed, and why continents look like they used to be linked together. This latest discovery addresses one of the last links in the theory that explains how geology works – which is a really significant find."

Leading models

There are two leading models that exist to explain how subduction zones may start - 'spontaneous', where one side sinks because it is more dense, and 'induced' where the plates are forced together by pressure from other distant locations.

These ideas are not easy to test, because the process cannot be observed happening today. Subduction zones are created over many millions of years, and the initiation period happened millions of years ago in most cases.

One way to understand the process is when scientists drill a long borehole into the on the overlying plate, to test the make-up and age of the crust and to see how it behaved before the subduction started. The problem with this method however, is that in the millions of years since the initiation, a large amount of sediment has piled up on top of the crust, obscuring it.

Significant discovery

Dr Kender said: "During our expedition to the IBM Arc, we successfully collected 1.5km of borehole through the overlying sediments and into the crust itself, dating the rocks with microscopic fossils and magnetic field reversals that took place throughout Earth's history.

"We found the crust to be much younger than expected, a stunning discovery indicating that we needed to readjust our ideas of how the subduction zone formed. The crust has chemical characteristics indicating it was formed at the time the subduction zone started, rather than much earlier. The crust may have formed in an extensional setting through seafloor spreading, in some ways similar to that formed at mid-ocean ridges today, although in this case near the newly-formed subduction zone."

Mid-ocean ridges, which are found in all ocean basins, are where fresh new oceanic crust is formed and are the opposite of subduction zones. There are numerous 'transform faults' near ridges today, enormous fractures through the crust that form due to the spreading plates interaction with the curvature of the earth.

"One idea is that the subduction zone formed along a previous line of weakness in one of these fracture zones, although it is not proven. Our new records show that the initiation was probably 'spontaneous' rather than 'induced', as the crust was formed in an extensional setting and did not become uplifted before formation. This finding really takes us one step closer to discovering how plate tectonics really works."

Co-author Kara Bogus of Texas A&M University's International Ocean Discovery Program (IODP), who served as the expedition project manager, adds: "This discovery is significant because one of the biggest questions remaining in plate tectonics is how subduction zones initiate. It's half the story in . We understand well the other half (how the plates move apart from each other and create new crust), but we are just beginning to understand this half. Overall, our results mean that we need to modify our subduction inception models."

Explore further: The downs and ups of mountain building

More information: "A record of spontaneous subduction initiation in the Izu–Bonin–Mariana arc." Nature Geoscience 8, 728–733 (2015) DOI: 10.1038/ngeo2515

Related Stories

The downs and ups of mountain building

August 20, 2015

In the D'Entrecasteaux Islands off Papua New Guinea, the rocks are giving rise to new ideas about the ways in which mountain chains form. A new scientific model inspired by data from the islands shows how the seemingly opposite ...

Is there an ocean beneath our feet?

January 27, 2014

(Phys.org) —Scientists at the University of Liverpool have shown that deep sea fault zones could transport much larger amounts of water from the Earth's oceans to the upper mantle than previously thought.

Studying ancient Earth's geochemistry

January 18, 2013

Researchers still have much to learn about the volcanism that shaped our planet's early history. New evidence from a team led by Carnegie's Frances Jenner demonstrates that some of the tectonic processes driving volcanic ...

Recommended for you

Weather anomalies accelerate the melting of sea ice

January 16, 2018

In the winter of 2015/16, something happened that had never before been seen on this scale: at the end of December, temperatures rose above zero degrees Celsius for several days in parts of the Arctic. Temperatures of up ...

2 comments

Adjust slider to filter visible comments by rank

Display comments: newest first

Nik_2213
3 / 5 (2) Sep 10, 2015
Another piece in the jigsaw, perhaps ? For most of the Pacific, the early evidence has long-since been subducted. They've done well finding this 'fossil' !!
docile
Sep 10, 2015
This comment has been removed by a moderator.

Please sign in to add a comment. Registration is free, and takes less than a minute. Read more

Click here to reset your password.
Sign in to get notified via email when new comments are made.