Tectonic Evolution and Mineralization of the Tibetan Plateau

Summary

The Tibetan Plateau represents the most extensive high-elevation orogenic system on Earth, shaped by successive episodes of terrane accretion, oceanic subduction and continental collision. During the Mesozoic, the Paleo-Tethys and Neo-Tethys oceans circulated between microcontinental blocks that now form the northern margin of the Indian plate. Subduction beneath Eurasia generated magmatic arcs, metamorphic belts and crustal shortening, culminating in the Cretaceous–Cenozoic collision with India. This collision induced intense crustal thickening, horizontal extrusion and uplift to elevations exceeding 4 km, while driving regional denudation and basin formation. Mineralization across the plateau spans porphyry Cu–Mo–Au systems, skarn and vein deposits, and rare-metal granites, all genetically linked to tectonic processes. Slab rollback and break-off episodes facilitated slab-derived melts and fluid release, triggering high-silica adakitic magmatism and hydrothermal circulation. Notable metallogenic provinces include the eastern Yidun arc, the Songpan-Ganzi belt and the North Qiangtang terrane, where crustal anatexis and mantle metasomatism produced fertile magmatic–hydrothermal systems. Understanding the spatio-temporal interplay of tectonics and mineralization informs exploration under rapid uplift and erosion, and underpins the global supply of critical metals such as copper, molybdenum, gold and rare earth elements.

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Tectonic Evolution and Mineralization of the Tibetan Plateau publication trend

The graph below shows the total number of articles in tectonic evolution and mineralization of the tibetan plateau across all publications each year (not limited to Nature Index journals).

Technical terms

Terrane: A fragment of crust with a distinct geological history accreted onto a continental margin.

Subduction: The process by which one tectonic plate descends beneath another into the mantle.

Porphyry deposit: A large, low-grade mineral system formed from magmatic-hydrothermal fluids near intrusive bodies.

Adakitic rock: A high-silica volcanic or plutonic rock derived from melting of a subducted basaltic slab.

Slab rollback: The retreat of a subducting plate hinge, causing mantle flow, crustal extension and magmatism.

References

  1. Whole-Rock and Apatite Geochemistry of Late Triassic Plutonic Rocks in the Eastern Songpan-Ganzi Orogenic Belt: Petrogenesis and Implications for Tectonic Evolution. Lithosphere (2024).
  2. Petrogenesis of late triassic high-silica granites in the North Qiangtang terrane, central Tibetan Plateau. Frontiers in Earth Science (2024).
  3. Metallogenic Chronology and Prospecting Indication of Tiechanghe Granite and Polymetallic Molybdenum Mineralization Types in Jiulong Area, Western Sichuan, China. Minerals (2024).
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