India-Asia convergence driven by the subduction of the Greater Indian continent

Fabio Capitanio, Gabriele Morra, Saskia Goes, Roberto Weinberg, Louis-Noel Moresi

Research output: Contribution to journalArticleResearchpeer-review

99 Citations (Scopus)

Abstract

The most spectacular example of a plate convergence event on Earth is the motion of the Indian plate towards Eurasia at speeds in excess of 18 cm yr(-1) (ref. 1), and the subsequent collision. Continental buoyancy usually stalls subduction shortly after collision, as is seen in most sections of the Alpine-Himalayan chain. However, in the Indian section of this chain, plate velocities were merely reduced by a factor of about three when the Indian continental margin impinged on the Eurasian trench about 50 million years ago. Plate convergence, accompanied by Eurasian indentation, persisted throughout the Cenozoic era(1-3), suggesting that the driving forces of convergence did not vanish on continental collision. Here we estimate the density of the Greater Indian continent, after its upper crust is scraped off at the Himalayan front, and find that the continental plate is readily subductable. Using numerical models, we show that subduction of such a dense continent reduces convergence by a factor similar to that observed. In addition, an imbalance between ridge push and slab pull can develop and cause trench advance and indentation. We conclude that the subduction of the dense Indian continental slab provides a significant driving force for the current India-Asia convergence and explains the documented evolution of plate velocities following continental collision.
Original languageEnglish
Pages (from-to)136 - 139
Number of pages4
JournalNature Geoscience
Volume3
Issue number2
DOIs
Publication statusPublished - 2010

Cite this

Capitanio, Fabio ; Morra, Gabriele ; Goes, Saskia ; Weinberg, Roberto ; Moresi, Louis-Noel. / India-Asia convergence driven by the subduction of the Greater Indian continent. In: Nature Geoscience. 2010 ; Vol. 3, No. 2. pp. 136 - 139.
@article{565c3e45feb64d1498913c79508c4235,
title = "India-Asia convergence driven by the subduction of the Greater Indian continent",
abstract = "The most spectacular example of a plate convergence event on Earth is the motion of the Indian plate towards Eurasia at speeds in excess of 18 cm yr(-1) (ref. 1), and the subsequent collision. Continental buoyancy usually stalls subduction shortly after collision, as is seen in most sections of the Alpine-Himalayan chain. However, in the Indian section of this chain, plate velocities were merely reduced by a factor of about three when the Indian continental margin impinged on the Eurasian trench about 50 million years ago. Plate convergence, accompanied by Eurasian indentation, persisted throughout the Cenozoic era(1-3), suggesting that the driving forces of convergence did not vanish on continental collision. Here we estimate the density of the Greater Indian continent, after its upper crust is scraped off at the Himalayan front, and find that the continental plate is readily subductable. Using numerical models, we show that subduction of such a dense continent reduces convergence by a factor similar to that observed. In addition, an imbalance between ridge push and slab pull can develop and cause trench advance and indentation. We conclude that the subduction of the dense Indian continental slab provides a significant driving force for the current India-Asia convergence and explains the documented evolution of plate velocities following continental collision.",
author = "Fabio Capitanio and Gabriele Morra and Saskia Goes and Roberto Weinberg and Louis-Noel Moresi",
year = "2010",
doi = "10.1038/NGEO725",
language = "English",
volume = "3",
pages = "136 -- 139",
journal = "Nature Geoscience",
issn = "1752-0894",
publisher = "Nature Publishing Group",
number = "2",

}

India-Asia convergence driven by the subduction of the Greater Indian continent. / Capitanio, Fabio; Morra, Gabriele; Goes, Saskia; Weinberg, Roberto; Moresi, Louis-Noel.

In: Nature Geoscience, Vol. 3, No. 2, 2010, p. 136 - 139.

Research output: Contribution to journalArticleResearchpeer-review

TY - JOUR

T1 - India-Asia convergence driven by the subduction of the Greater Indian continent

AU - Capitanio, Fabio

AU - Morra, Gabriele

AU - Goes, Saskia

AU - Weinberg, Roberto

AU - Moresi, Louis-Noel

PY - 2010

Y1 - 2010

N2 - The most spectacular example of a plate convergence event on Earth is the motion of the Indian plate towards Eurasia at speeds in excess of 18 cm yr(-1) (ref. 1), and the subsequent collision. Continental buoyancy usually stalls subduction shortly after collision, as is seen in most sections of the Alpine-Himalayan chain. However, in the Indian section of this chain, plate velocities were merely reduced by a factor of about three when the Indian continental margin impinged on the Eurasian trench about 50 million years ago. Plate convergence, accompanied by Eurasian indentation, persisted throughout the Cenozoic era(1-3), suggesting that the driving forces of convergence did not vanish on continental collision. Here we estimate the density of the Greater Indian continent, after its upper crust is scraped off at the Himalayan front, and find that the continental plate is readily subductable. Using numerical models, we show that subduction of such a dense continent reduces convergence by a factor similar to that observed. In addition, an imbalance between ridge push and slab pull can develop and cause trench advance and indentation. We conclude that the subduction of the dense Indian continental slab provides a significant driving force for the current India-Asia convergence and explains the documented evolution of plate velocities following continental collision.

AB - The most spectacular example of a plate convergence event on Earth is the motion of the Indian plate towards Eurasia at speeds in excess of 18 cm yr(-1) (ref. 1), and the subsequent collision. Continental buoyancy usually stalls subduction shortly after collision, as is seen in most sections of the Alpine-Himalayan chain. However, in the Indian section of this chain, plate velocities were merely reduced by a factor of about three when the Indian continental margin impinged on the Eurasian trench about 50 million years ago. Plate convergence, accompanied by Eurasian indentation, persisted throughout the Cenozoic era(1-3), suggesting that the driving forces of convergence did not vanish on continental collision. Here we estimate the density of the Greater Indian continent, after its upper crust is scraped off at the Himalayan front, and find that the continental plate is readily subductable. Using numerical models, we show that subduction of such a dense continent reduces convergence by a factor similar to that observed. In addition, an imbalance between ridge push and slab pull can develop and cause trench advance and indentation. We conclude that the subduction of the dense Indian continental slab provides a significant driving force for the current India-Asia convergence and explains the documented evolution of plate velocities following continental collision.

UR - http://www.nature.com/ngeo/journal/v3/n2/pdf/ngeo725.pdf

U2 - 10.1038/NGEO725

DO - 10.1038/NGEO725

M3 - Article

VL - 3

SP - 136

EP - 139

JO - Nature Geoscience

JF - Nature Geoscience

SN - 1752-0894

IS - 2

ER -