Earth: how to explain the astonishing speed of collision between India and Asia?

Earth how to explain the astonishing speed of collision between

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[EN VIDÉO] A billion years summarized in 40 seconds: plate tectonics
Researchers have modeled the movements of tectonic plates over the past billion years.

Among the manifestations of tectonic plates and the formidable migration of continents over time, the collision chains are certainly the most emblematic and the most visible in the landscape. The Himalayas, home to the highest peak in the world, are the result of the collision of the Indian continent with Asia. This event represents one of the major tectonic episodes of “recent” geological history. Because 200 million years ago, the situation was very different from that of today.

The analysis of movements continents, by through magnetic anomalies recorded by the ocean floor, teaches us that in the Triassic, India was located much further south, within the supercontinent Gondwana, which then began to fragment. Between the north of the Indian block and the Eurasian continent is a huge ocean that has now disappeared: the ocean Tethys.

The Himalayas, the result of India’s mad dash north

It is the double action of the opening of the current South-West Indian Ocean and the closing of the Tethys which will lead to the rapid migration of India towards the north. Fast is still an understatement. Because India will thus move to a speed quite exceptional at 20 cm/year! A mad race which brings him very quickly in contact with Asia. The violent collision that will lift the whole region and give birth to the Himalayas but more generally to the Hindu Kush-Himalaya area will thus begin about 60 million years ago.

For a long time, scientists have been interested to the engines of this dazzling continental migration. Among the proposed models, that of a double subduction. A hypothesis that has just been supported by a recent study, published in Science Advances.

Not one, but two successive subduction planes

The team of Chinese researchers has indeed highlighted the presence, in the coat upper located under the Myanmar region in the eastern range, remains of ancient slab. A slab represents the part of the plate which has entered into subduction, that is to say which has passed under the overlapping plate.

By accurately imaging the upper mantle in this region, thanks to seismic waves and the deployment of a new network of seismic stations, scientists were able to observe for the first time the presence of not one, but two parallel subduction planes, plunging into the depths of the mantle at the level of the suture of the ancient Tethys ocean.

The westernmost slab, which is characterized by a high velocity zone compared to that of the mantle rocks, was already identified by previous studies and represents the currently active subduction system. For India’s indentation into Eurasia is still ongoing, even though the speed of convergence is much lower than it was 60 million years ago.

But the Chinese researchers have just identified a second plane plunging towards the east, located in front of the first. The associated velocity anomaly is observable up to 300 km depth. For scientists, this is the signature of an ancient slab, now inactive, which would have participated in the closing of the Tethys ocean about 40 million years ago.

This new discovery naturally has implications for the tectonic models hitherto used to illustrate the convergence of India and Eurasia. In particular, it helps to explain the rapid migration from India to the north.

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