Abstract
Stratabound ore deposits in China commonly occur in organic-rich formations (TOC > 1%, up to 19%), including black shales which are host rocks for stratabound U, Ni, V and Cu ore deposits, and source beds for Pb-Zn, Hg, Sb, Au and Sn ore deposits. Spatially, some stratabound ore deposits are adjacent to oilfields, or associated with oil traps.
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