Anomaly in Atlantic Ocean May Be First Detection of a Tectonic Plate Peeling Aside

Scientists have recognized what they are saying might be the primary proof of a tectonic plate peeling into two separate layers beneath the ocean.

This epic however nonetheless hypothetical division phenomenon – to the extent we will detect it in laptop modelling – might be answerable for the beginning of a brand new subduction zone, the place one in every of Earth’s tectonic plates is pushed forcefully beneath one other.


Marine geologist João Duarte from the College of Lisbon in Portugal has been learning the seismic historical past of his house metropolis for years, most famously characterised by the Nice Lisbon earthquake of 1755: a large catastrophic quake and tsunami that successfully wiped Lisbon out, killing as much as an estimated 100,000 folks within the course of.

Centuries later, a a lot milder occasion in 1969 in the identical area was additionally famous by seismologists, however luckily claimed no human lives.

But what’s unusual is that these violent quakes are taking place in any respect, because the area the place they’re emanating from is a sparse, abyssal plain on the seafloor alongside the Iberian Peninsula, a great distance from any energetic tectonic faults.

015 iberia subduction tectonic plate portugal 1(Duarte et al., Geology, 2013)

However far under this flat, unremarkable seabed panorama, one thing else is occurring, Duarte says: one thing seismic.

“This seismicity is situated under a seismically silent layer, interpreted as a serpentinisation entrance propagating down by the lithospheric higher mantle,” Duarte and his workforce write in an summary for brand new analysis offered final month on the EGU Normal Meeting 2019 in Vienna.


Serpentinisation is a geological course of the place rock constructions take up water, and in accordance with the researchers, it might be answerable for the oceanic lithosphere off the coast of Portugal peeling in two, probably triggering quakes because it rips aside.

“A number of tomographic fashions have constantly imaged a fast-velocity anomaly extending as much as a depth of 250 kilometres, proper under this seismicity cluster,” the researchers write.

“We interpret this anomaly as a lithospheric drip brought on by the delamination of oceanic lithosphere. If so, it’s the first time that delamination of oceanic lithosphere is recognized.”

Testing their speculation with laptop fashions, the researchers’ early work – which as but has not been peer-reviewed – suggests serpentinisation layer in previous oceanic lithosphere may generate “horizontal decoupling zones” by the oceanic plate, main the decrease, softer rock layer to ‘delaminate’ (tear away) from the higher layer.

In the event that they’re proper – and that is an enormous if for now – the researchers suggest that this phenomenon might be serving to to create a subduction zone within the area, the place one tectonic plate finally ends up being pushed beneath one other.


“Immediately, we all know that the Southwest Iberian Margin is certainly being reactivated,” Duarte defined in a weblog publish final 12 months.

“Whether or not it will result in the nucleation of a brand new subduction zone remains to be a matter of debate, and we’ll most likely by no means know for positive. Nonetheless, subduction initiation is among the main unsolved issues in earth sciences, and the coasts off Lisbon would possibly represent an ideal pure laboratory to research this drawback.”

Taken to at least one excessive, this subduction initiation course of may hypothetically assist underlay the foundations of a completely new supercontinent.

In analysis revealed in 2016, Duarte and fellow researchers proposed a brand new conceptual mannequin primarily based round previous, unstable oceanic lithosphere, through which “each the Pacific and the Atlantic oceans shut concurrently, resulting in the termination of the current Earth’s supercycle and to the formation of a brand new supercontinent, which we identify Aurica”.

That distant future – if it ever involves go – is many hundreds of thousands of years away, however Duarte for one is happy by the probabilities.

“It is a large assertion,” Duarte instructed Nationwide Geographic. “Perhaps this isn’t the answer to all the issues. However I believe we have now one thing new right here.”

The findings had been offered at on the EGU Normal Meeting 2019 held in Vienna in April.


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