Supplemental Material: Early to middle Eocene (50–43 Ma) Xianqian Basin in central Tibet: Archives of arid paleoenvironments and a southward plateau uplift trend

Anlin Ma; et al.

doi:10.1130/gsab.s.30359200

October 14, 2025Open Access

Supplemental Material: Early to middle Eocene (50–43 Ma) Xianqian Basin in central Tibet: Archives of arid paleoenvironments and a southward plateau uplift trend

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Key Points

The research highlights a trend of plateau uplift during the Eocene, impacting climate and ecosystems.
Analysis of paleoenvironments in the Xianqian Basin indicates significant aridity around 50–43 Ma.
Findings contribute to understanding the geological history of central Tibet and its climatic evolution.
Understanding these trends is essential for insights into past environmental conditions and landscape evolution.

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Implication

This analysis identifies arid paleoenvironments and shows trends of plateau uplift in the Eocene Xianqian Basin, highlighting significant geological changes in Tibet.

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Cite This Study

Ma et al. (2025) studied this question.

synapsesocial.com/papers/68f04935e559138a1a06e3a5 https://doi.org/10.1130/gsab.s.30359200

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Supplemental Material: Early to middle Eocene (50–43 Ma) Xianqian Basin in central Tibet: Archives of arid paleoenvironments and a southward plateau uplift trend

Key Points

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Implication

Abstract

Discussion

Cite This Study

Supplemental Material: Early to middle Eocene (50–43 Ma) Xianqian Basin in central Tibet: Archives of arid paleoenvironments and a southward plateau uplift trend

Key Points

No abstract yet

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Implication

Abstract

Discussion

Cite This Study

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