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Gold deposits in the Himalayas formed through hydrothermal fluid circulation driven by crustal thickening

the verdict
SUPPORTED
the evidence backs this
Recorded sources
5 sources for · 0 against

Counts group repeated records of the same source within each side. They do not measure evidence strength or source independence.

Scientific studies and geological literature support the claim that gold deposits in the Himalayas formed through hydrothermal and metamorphic fluid processes associated with orogenic crustal deformation and thickening.

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Judged against reference works: claims of this kind are settled by the historical reference record, not journal abstracts.

Evidence for · 5
sciencedirect.com: Tectonically driven fluid flow and gold mineralisation in active collisional orogenic belts: comparison between New Zealand and western Himalaya
Recorded source metadata

sciencedirect.com: Tectonically driven fluid flow and gold mineralisation in active collisional orogenic belts: comparison between New Zealand and western Himalaya. sciencedirect.com. https://www.sciencedirect.com/science/article/abs/pii/S0040195101002530

Explicitly connects tectonically driven fluid flow and gold mineralization in collisional orogenic belts like the Himalayas.

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More for · 4
doi.org: Control of crustal deformation on orogenic Au mineralization in Himalaya: A case study from Buzhu
Recorded source metadata

doi.org: Control of crustal deformation on orogenic Au mineralization in Himalaya: A case study from Buzhu. doi.org. https://doi.org/10.1016/j.jsg.2024.105269

Examines crustal deformation control on orogenic gold mineralization in the Himalayas.

doi.org: The role of deep-sourced metamorphic fluids in Au enrichment: A case study of the Bangbu Au deposit, southern Tibet (Western China)
Recorded source metadata

doi.org: The role of deep-sourced metamorphic fluids in Au enrichment: A case study of the Bangbu Au deposit, southern Tibet (Western China). doi.org. https://doi.org/10.1016/j.oregeorev.2025.106699

Discusses deep-sourced metamorphic fluids driving gold enrichment in the Tibetan Himalayan region.

sciencedirect.com: Genesis of the Mingsai Au deposit, southern Tibet: Constraints from geology, fluid inclusions, 40Ar/39Ar geochronology, H–O isotopes, and in situ sulfur isotope compositions of pyrite - ScienceDirect
Recorded source metadata

sciencedirect.com: Genesis of the Mingsai Au deposit, southern Tibet: Constraints from geology, fluid inclusions, 40Ar/39Ar geochronology, H–O isotopes, and in situ sulfur isotope compositions of pyrite - ScienceDirect. sciencedirect.com. https://www.sciencedirect.com/science/article/abs/pii/S0169136819310492

Identifies southern Tibet Himalayan deposits as orogenic-type gold linked to deep-source fluids.

doi.org: Mechanism and age of gold remobilization in orogenic gold deposit from primary laminated ore to the high-grade ore: A case study from Cenozoic Bangbu gold deposit, Tethyan Himalaya
Recorded source metadata

doi.org: Mechanism and age of gold remobilization in orogenic gold deposit from primary laminated ore to the high-grade ore: A case study from Cenozoic Bangbu gold deposit, Tethyan Himalaya. doi.org. https://doi.org/10.1016/j.oregeorev.2023.105464

Analyzes hydrothermal fluid processes in Cenozoic orogenic gold deposits within the Tethyan Himalaya.

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first checked31 Jul 2026
judged → SUPPORTED · 7531 Jul 2026
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