Metallogenesis of the Zhibo and Chagangnuoer volcanic iron oxide deposits in the Awulale Iron Metallogenic Belt, Western Tianshan orogen, China
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文摘

Two iron deposits were generated in a continental arc-setting.

We favor a magmatic origin for the iron oxide mineralization.

The mineralization is related to the magmatic evolution of the same volcano.

The mineralization of both deposits occurred between ca. 350 and 330 Ma.

Both deposits were hydrothermally overprinted between ca. 319 and 313 Ma.

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