September 23, 2025Open Access

Supplemental Material: Late Miocene rapid exhumation in the West Kunlun range: Insights into Tibetan Plateau growth and India-Asia lithospheric collision

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Rapid exhumation occurred in the late miocene period, accelerating the growth of the Tibetan Plateau.
Insights from the West Kunlun Range indicate significant geological activity associated with the India-Asia collision.
The findings suggest that tectonic forces contribute to the ongoing evolution of the Tibetan region.
Geological evidence presented provides a clearer understanding of the lithospheric processes over millions of years.

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Implication

This analysis highlights rapid exhumation in the West Kunlun Range, suggesting implications for the Tibetan Plateau and India-Asia lithospheric collision.

Abstract

Analytical methods, Figures S1–S5, and Tables S1–S6.

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Xiang et al. (2025) studied this question.

synapsesocial.com/papers/68d4759931b076d99fa6db50 https://doi.org/10.1130/geol.s.30190204.v1

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Implication

This analysis highlights rapid exhumation in the West Kunlun Range, suggesting implications for the Tibetan Plateau and India-Asia lithospheric collision.

Abstract

Analytical methods, Figures S1–S5, and Tables S1–S6.

Supplemental Material: Late Miocene rapid exhumation in the West Kunlun range: Insights into Tibetan Plateau growth and India-Asia lithospheric collision

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Implication

Abstract

Discussion

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Supplemental Material: Late Miocene rapid exhumation in the West Kunlun range: Insights into Tibetan Plateau growth and India-Asia lithospheric collision

Key Points

No abstract yet

Implication

Abstract

Discussion

Cite This Study

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