Collision-related tin metallogeny: Insight from a new discovery of the volcanic-subvolcanic-hosted Sn deposit in the western Gangdese, Xizang

Hao Chen , Xin Chen , Youye Zheng , Xian Che , Yuanping Lai , Xingkai Huang , Shunbao Gao , Bei Pang

Geoscience Frontiers ›› 2026, Vol. 17 ›› Issue (2) : 102216

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Geoscience Frontiers ›› 2026, Vol. 17 ›› Issue (2) :102216 DOI: 10.1016/j.gsf.2025.102216
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Collision-related tin metallogeny: Insight from a new discovery of the volcanic-subvolcanic-hosted Sn deposit in the western Gangdese, Xizang
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Abstract

The Gangdese metallogenic belt in Xizang, a world-class copper polymetallic province, has a poorly understood western segment due to extensive volcanic cover and limited historical exploration. The recent discovery of the Sangmoladong (SMLD) deposit, the first undocumented volcanic-subvolcanic-hosted, tin-dominant polymetallic system in western Gangdese, provides a unique opportunity to investigate collisional metallogeny. Through integrated LA-ICP-MS U-Pb geochronology of zircon and cassiterite, comprehensive whole-rock geochemistry, and Nd-Hf isotopes, this research establishes a genetic link between Paleocene magmatism and Sn-polymetallic mineralization. The mineralization is hosted within granite porphyry stocks and associated rhyolitic tuff breccias of a volcanic dome complex. It comprises two main stages: an early, disseminated cassiterite-sulphide stage with chloritic alteration, followed by later fluorite-cassiterite-tourmaline veins and veinlets. New LA-ICP-MS U-Pb dating constrains the timing of granite porphyry emplacement to 61.3 ± 0.2 Ma and rhyolitic tuff deposition to 61.8 ± 0.5 Ma. Cassiterite mineralization occurred between 61.0 ± 2.2 Ma and 59.3 ± 3.5 Ma, confirming that Sn metallogenesis was coeval with this Paleocene magmatic pulse during the Indo-Asian collision. The ore-forming granitic porphyries are highly evolved, A-type granites, characterized by high SiO2 (77.50 - 80.40 wt.%), elevated zircon saturation temperatures (831 - 870 °C), and high Ga/Al ratios (10,000 × Ga/Al = 5.75 - 6.51). Their Nd-Hf isotopic signatures (εNd(t) = −6.5 to −6.3; zircon εHf(t) = −5.2 to +2.1) indicate an origin from anatexis of ancient Lhasa terrane metapelites, likely triggered by lithospheric extension during Neo-Tethyan slab rollback. This generated a reduced, fluorine- and boron-rich magmatic-hydrothermal system highly efficient at mobilizing and concentrating tin. On a regional scale, a metallogenic framework is proposed where Fe-Cu mineralization is sourced from hybridized mantle-crust magmas, whereas Pb-Zn and Sn systems derive from similar crustal-dominated sources. This metallogenic divergence of Pb-Zn and Sn reflects contrasting thermal regimes and magma crystallization pathways during a transtensional setting with local extension in pull-apart and uplift structures. The formation of the SMLD tin deposit is attributed to prolonged fractional crystallization of a high-temperature, low fO2 magma within a subvolcanic dome complex. These conditions suppressed early cassiterite saturation and promoted extreme tin enrichment in the residual melt. This study makes two key contributions: (1) it identifies the first volcanic-hosted tin system in the western Gangdese, challenging traditional exploration models focused on porphyry skarn Cu-Pb-Zn deposits; and (2) it establishes a new tectono-metallogenic model that elucidates the spatiotemporal evolution of Paleocene mineralization (Fe-Cu → Pb-Zn → Sn) during orogenesis. These findings provide crucial insights into metallogeny in continental collision zones and pave the way for new exploration targets for tin resources throughout the central-western Tethyan metallogenic domain, especially in underexplored volcanic terrains with analogous geodynamic histories.

Keywords

Volcanic-Subvolcanic magma / Cassiterite / Tin-polymetallic mineralization / Slab rollback / Tectono-metallogenic model / Gangdese

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Hao Chen, Xin Chen, Youye Zheng, Xian Che, Yuanping Lai, Xingkai Huang, Shunbao Gao, Bei Pang. Collision-related tin metallogeny: Insight from a new discovery of the volcanic-subvolcanic-hosted Sn deposit in the western Gangdese, Xizang. Geoscience Frontiers, 2026, 17(2): 102216 DOI:10.1016/j.gsf.2025.102216

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CRediT authorship contribution statement

Hao Chen: Writing - review & editing, Writing - original draft, Software, Methodology, Investigation, Data curation. Xin Chen: Writing - review & editing, Writing - original draft, Software, Methodology, Data curation, Conceptualization. Youye Zheng: Writing - review & editing. Xian Che: Writing - review & editing, Software. Yuanping Lai: Writing - review & editing, Methodology. Xingkai Huang: Writing - review & editing, Software. Shunbao Gao: Writing - review & editing, Investigation, Funding acquisition. Bei Pang: Writing - review & editing, Software.

Declaration of competing interest

The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.

Acknowledgements

We extend our sincere appreciation to Associate Editor Prof. Qingfei Wang for his thorough review and valuable enhancements. We are especially indebted to the five anonymous reviewers for their expert evaluations, which greatly strengthened our manuscript. We also acknowledge the National Natural Science Foundation of China (U22A20572), Special Fund of Deep Earth Probe and Mineral Resources Exploration- National Science and Technology Major Project (No. 2025ZD1005904), the National Key R&D Program of Xizang (XZ202401ZY0026), and the Postdoctoral Science Foundation of China (BX20220277, 2022 M722938).

Appendix A. Supplementary data

Supplementary data to this article can be found online at https://doi.org/10.1016/j.gsf.2025.102216.

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