The collision between the Indian subcontinent and the Asian landmass resulted in the formation of the Himalayan Mountains and the rise of the Tibetan Plateau, with consequent major climatic and environmental changes around our planet.
Placing precise constraints on the timing of the India-Asia continental collision is essential to understand the subsequent geological and topographic evolution of the orogenic belt as well as the tectonic uplift of the Tibetan Plateau and their effects on climate, environment, and life.
A recent study has constrained precisely the timing of the initial India-Asia continental collision by the accurate analysis of the sedimentary record preserved along the collision zone.
Based on the detailed study of fossils and detrital minerals contained in strata exposed along both sides of the Yarlung-Zangbo suture zone in Tibet, a team of Chinese and Italian researchers has determined with unprecedented accuracy the time when India and Asia first came into contact by pin-pointing major changes of sedimentary style and in provenance of detritus.
A variety of approaches have been followed to date such a major tectonic event, including paleomagnetism and biostratigraphic or radiometric dating of sedimentary, magmatic and metamorphic rocks coupled with structural, stratigraphic and sedimentological observations. A fierce debate ensued often because different research teams used different indicators and criteria to define continental collision and tentatively assess the chronological sequence of progressing orogeny.
This new research starts from a clear definition of collision onset as the timing of first contact between the opposite edges of the Indian and Asian continental crusts following complete consumption of intervening Neo-Tethyan oceanic lithosphere at a point.
By accurately dating with multiple methods the turbiditic deep-sea sediments derived from both India and Asia and deposited in the trench just south of the zone of initial collision, the researchers have constrained precisely the India-Asia collision onset as middle Palaeocene (59±1 million years ago). Initial continent-continent collision preceded by 20 million years the final disappearance of marine seaways from the Himalayas, and by 30 million years the accumulation of massive fluvial gravel and sand deposits in the Indo-Gangetic plain of northern India.
Researchers also showed that there was no major diachroneity of collision onset from the central to the western Himalaya.
This study represents a major contribution to understand plate tectonics and continental dynamics, and is of great significance not only as far as the India-Asia collision, Himalayan orogeny, Tibetan-Plateau uplift and consequent Cenozoic climatic change are concerned, but also because it provides a reference standard useful to investigate the process of continental collision and to reconstruct its progress in time resulting in the full growth of huge mountain belts.
The study appears in Science China: Earth Sciences.
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