Sources and mechanisms for two mineralization stages at Chaihulanzi, North China Craton: constraints from mineralogy, trace elements, and in situ sulfur isotopes

2026/07/30 by Qing-fei Sun, Ju-xing Tang, Chen-guang Zhao +3

paper · doi:10.1016/j.oregeorev.2026.107471

crossref created 2026/07/30 · crossref deposited 2026/08/06 · crossref indexed 2026/08/06 · crossref issued 2026/09/01 · crossref published 2026/09/01 · crossref published-print 2026/09/01

Citations

• Geological, fluid inclusion, and O–C–S–Pb–He–Ar isotopic constraints on the genesis of the Honghuagou lode gold deposit, northern North China Craton
• Remobilization of metasomatized mantle lithosphere: a new model for the Jiaodong gold province, eastern China
• Mineralogy and He–Ar isotopic compositions of pyrites in the Paishanlou Au deposit on the northern margin of North China Craton
• A rare Phanerozoic amphibolite-hosted gold deposit at Danba, Yangtze Craton, China: significance to fluid and metal sources for orogenic gold systems
• Trace Element Content of Sedimentary Pyrite in Black Shales
• Trace-element characteristics of different pyrite types in Mesoarchaean to Palaeoproterozoic placer deposits
• Gold and Trace Element Zonation in Pyrite Using a Laser Imaging Technique: Implications for the Timing of Gold in Orogenic and Carlin-Style Sediment-Hosted Deposits
• Orogenic gold deposits: A proposed classification in the context of their crustal distribution and relationship to other gold deposit types
• A revaluation of the Co/Ni ratio in pyrite as geochemical tool in ore genesis problems
• Revised effective ionic radii and systematic studies of interatomic distances in halides and chalcogenides
• Systematics of Sulfur and Carbon Isotopes in Hydrothermal Ore Deposits
• Cobalt, nickel and selenium in sulphides as indicators of ore genesis