Gold deposits in the Himalayas formed through hydrothermal fluid circulation driven by crustal thickening
the verdict
SUPPORTED
the evidence backs this
confidence 75/100
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.
Evidence for · 5
sciencedirect.com: Tectonically driven fluid flow and gold mineralisation in active collisional orogenic belts: comparison between New Zealand and western Himalaya
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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
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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)
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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
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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
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Analyzes hydrothermal fluid processes in Cenozoic orogenic gold deposits within the Tethyan Himalaya.