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Paleoenvironmental conditions of the Huayacocotla basin, mexico during the Late Jurassic: Implications for Mn accumulation
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DOI：10.1016/j.gexplo.2026.108095.png)
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Abstract
En 中文
• Sediment hosted manganese carbonate deposit. • Manganese accumulation occurred under anoxic conditions from terrestrial and hydrothermal sources. • Diagenetic formation of manganese carbonates within a semi restricted redox stratified basin. • Deposition was significantly influenced by both local and global environmental factors
Keywords:
Manganese carbonate
Anoxic conditions
Diagenesis
Redox stratification
Paleoenvironmental conditions
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