Weiduo Hao

Latest

• The Kaolinite Shuttle Links the Great Oxidation and Lomagundi Events
• Depositional and environmental constraints on the late Neoarchean Dagushan deposit (Anshan-Benxi area, North China Craton): An Algoma-type banded iron formation
• Trace Elemental Partitioning on Clays Derived from Hydrothermal Muds of the El Tatio Geyser Field, Chile
• Hydrothermally induced $^{34}$S enrichment in pyrite as an alternative explanation of the Late-Devonian sulfur isotope excursion in South China
• New constraints on the onset age of the Emeishan LIP volcanism and implications for the Guadalupian mass extinction