Kshiroda Plate
| Kshiroda Plate | |
|---|---|
 The Kshiroda Plate to the south of the Eurasian Plate(>50 mya) | |
| Features | Tibetan Plateau, Tethys Ocean, Indian Ocean, Himalayas |
The Kshiroda Plate (Pronunciation:
Discovery
The Kshiroda Plate was discovered when geologists studying the boundary zone between the Indian and Eurasian Plates, noticed that the data supported the existence of two parallel
This was studied in detail in 2015 by Oliver Jagoutz, a geologist at the Massachusetts Institute of Technology, Cambridge, Massachusetts, and his team, who identified the possibilities of a hidden tectonic plate in the region.[3]
The usage of the term "Kshiroda Plate" began the same year 2015.
Subduction
Around 50 million years ago, the Indian Plate collided with the southern subduction zone of the Kshiroda oceanic plate causing the plate to shrink. It was pushed northwards and eventually collapsed more than 40 million years ago.[3] It was pushed below the crust of the Eurasian Plate and this led to the formation of the Tibetan Plateau and the Himalayas.
It is possible that the impact might have caused the delamination of the Indian Plate beneath the Tibetan Plateau, a process which is still continuing.[4]
Significance
The Kshiroda Plate has great significance in the geology of South Asia. The subduction of the plate, which occurred before 40 million years ago, caused the upliftment of the Tibetan Plateau.
The
See also
References
- ISSN 0084-6597.
- ISSN 0040-1951.
- ^ ISSN 1752-0908.
- doi:10.22541/e (inactive 2024-04-13).)
{{cite journal}}: CS1 maint: DOI inactive as of April 2024 (link - ^ fultonk (2011-02-11). "The Himalayas ~ Tectonic Motion: Making the Himalayas | Nature | PBS". Nature. Retrieved 2024-04-13.
