Research from China University of Geosciences (Beijing) provides new insights into the India–Asia collision in the Western Himalayas dating back to circa 55 million years and the extent of Greater India

Hundreds of millions of years ago, the surface of the Earth looked very different from how we see it today. There were just two continents: Laurasia and Gondwanaland. The present Indian subcontinent was part of Gondwanaland, which broke up about 150 million years ago. A part of the Indian Plate that broke away from the Gondwana supercontinent is now subducted under the Himalayas and the Tibetan Plateau. Understanding the original extent of the ‘lost’ part of this continent, called Greater India, is therefore important to resolve several key questions surrounding the age of the India–Asia collision and answer how and when the Tibetan Plateau got built.

However, estimates of the extent of Greater India have remained uncertain, varying from 100’s to more than 2,000 km. The Sangdanlin section lying between the Indian and Asian plates in southern Tibet represents a geologic Rosetta stone to constrain the initiation of the India–Asia collision; however, divergent evidence regarding its age and paleomagnetic record has made the estimation challenging.

Providing key answers, researchers from China University of Geosciences (Beijing) (CUGB) along with colleagues from other institutions, including Ludwig Maximilians University and Chinese Academy of Sciences, have now clarified that Greater India was a single plate of 2,000 to 3,000 km before it subducted under Asia. Professor Jun Meng from the School of Earth Sciences and Resources, CUGB, the first author of the study that was published in Proceedings of the National Academy of Sciences of the USA on August 8, 2023, explains, “There are two primary models for the India–Asia collision. The first is a multistage collision model that subdivides the oceanic basin at the leading edge of India into smaller plates that were later incorporated into the Asian plate. The second model says that India and Greater India existed as a single plate in the Early Cretaceous period, with the upper crust of the northern margin of Greater India forming the Himalayan thrust belt and the lower crust being subducted under Asia.” His colleague from CUGB, Professor Chengshan Wang adds, “Our goal was to understand which of these models was more accurate.”

The researchers resolved several questions surrounding these issues through a combined geologic, paleontologic, and paleomagnetic study of the infamous Sangdanlin section. The paleomagnetism of the Cretaceous rocks allowed the researchers to track the geographical position of the northern sector of the Indian Plate through time and calculate a minimum size for Greater India. The data obtained in the study showed that the lithosphere— the rocky outer shell of the Earth—consumed by subduction since the onset of the collision 55 mya was larger than the area of the Indian subcontinent today and originally extended ~2,000 to 3,000 km to the north. Consequently, almost 5 million km² of lithosphere has been subducted under the Asian Plate, which must have contributed to the rise of the Tibetan Plateau.

These findings represent a tectonic shift in our understanding of the India–Asia collision and the emergence of various geological structures in these regions.  Prof. Stuart A. Gilder from Ludwig Maximilians University observes, “Our findings challenge established notions of the formation of Asia’s southern margin through the coalescence of independent tectonic blocks in the Tethys Ocean. They could help us fill the gap in the knowledge regarding the size of the Indian plate in a Gondwanaland configuration and the tectonic history of India up until its collision with Asia.”

Disruptive discoveries advance human knowledge in leaps and bounds. Kudos to the research team for contributing to such a discovery!

For a quick animated version of this research story, check out this video, here.

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Reference

DOI: https://doi.org/10.1073/pnas.2305928120

Authors: Jun Meng^a, Stuart A. Gilder^b, Xiaodong Tan^c, Xin Li^d, Yalin Li^a, Hui Luo^d, Noritoshi Suzuki^e, Zihao Wang^a, Yuchen Chi^b, Chunyang Zhang^a, and Chengshan Wang^a

Affiliations      

^aState Key Laboratory of Biogeology and Environmental Geology, School of Earth Sciences and Resources, China University of Geosciences Beijing, Beijing 100083, China

^bDepartment of Earth and Environmental Sciences, Ludwig Maximilians University, 80333 Munich, Germany

^cKey Laboratory of Ocean and Marginal Sea Geology, South China; Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China

^dState Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China;

^eDepartment of Earth Science, Graduate School of Science, Tohoku University, Sendai City 980-8578, Japan

About Professor Chengshan Wang

Chengshan Wang is a Professor at the School of Earth Sciences and Resources

at China University of Geosciences (Beijing). He is a member of the Chinese Academy of Sciences and the President of the Executive Committee of the Deep-time Digital Earth (DDE) Big Science Program. His research interests include the Cretaceous paleoenvironment and paleoclimate, tectonic uplift and sedimentary response, and analysis of petroliferous basins. With over 19,000 citations, he is a leader in the field of uplift of mountain ranges and has extensively studied the Tibetan Plateau and the Himalayan range. He has received The Li Siguang Geological Science Award and the National Award of Natural Sciences.

About Professor Jun Meng

Dr. Jun Meng is a professor at the School of Earth Sciences and Resources at the China University of Geosciences, Beijing, China. Prof. Meng’s research interests include paleomagnetism and tectonics. He has authored over 20 research papers in reputed scientific journals and has over 1,000 citations to his credit.