Iron transport and deposition mechanisms in the Taochong iron-rich skarn deposit, Middle-Lower Yangtze Valley, Eastern China
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Two types of ores (type 1 and 2 ore) in this deposit were recognized.

We estimate the fluid composition and physico-chemical conditions of ore deposition.

The type 1 ore deposition took place by filling, probably induced by fluid boiling.

The type 2 ore deposition caused by replacement and induced by fluid-rock interactions and mixing.

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