Origin of Fe-Mn ± Si layers associated with the Permian volcanic-hosted massive sulphide deposits in the Tasik Chini district, Peninsular Malaysia

Mohd Basril Iswadi Basori,Khin Zaw,Garry J. Davidson,Sebastien Meffre,Ross R. Large

Journal of Asian Earth Sciences（2020）

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摘要

•The Fe-Mn ± Si layers at the VHMS deposits in Tasik Chini were formed by chemical precipitation.•Sources of such layers were mainly chemical components with minor detrital materials.•These layers were formed due to the seafloor-hydrothermal activity associated with hydrothermal vents.

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Tasik Chini,VHMS,Fe-Mn±Si layers,Geochemistry,Peninsular Malaysia

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Origin of Fe-Mn ± Si layers associated with the Permian volcanic-hosted massive sulphide deposits in the Tasik Chini district, Peninsular Malaysia

Origin of Fe-Mn ± Si layers associated with the Permian volcanic-hosted massive sulphide deposits in the Tasik Chini district, Peninsular Malaysia