Origin and genesis of intracontinental orogens
Peer-Reviewed Publication
Updates every hour. Last Updated: 13-Dec-2025 22:11 ET (14-Dec-2025 03:11 GMT/UTC)
In an article published in Science China Earth Sciences, two senior scientists at China University of Geosciences (Beijing) and University of Science and Technology of China present comprehensive arguments for the past and present of intracontinental orogens, developing a holistic model of mountain building from intracontinental reworking of fossil plate margins. The intracontinental orogeny involves dual dynamic mechanisms via either far-field compressional stress transmission from remote plate margins or near-field extensional stress focus from local plate bottom. This provides new insights into the formation and evolution of continental tectonics with respect to inheritance and development in both structure and composition from preceding plate margins.
A recent study published in National Science Review revealed detailed crustal structures of the Eastern Himalayas, showing a local stress field of dominantly north-south horizontal compression, low-angle subduction of the crust-mantle boundary and flat-ramp geometry of the Indian plate beneath the Eurasian plate. These results have important implications for understanding the regional tectonics, the broad uplift of the mountains and generation of thrust and strike-slip earthquakes in this continental collision zone.
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