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suggested that the NE-trending Jiaojia-Xincheng fault (JXF) experienced normal faulting from 135 Ma to 120 Ma, and a sinistral slip from 120–110 Ma, which was followed by normal displacement at ca. From 80–60 Ma, the fault acted as a normal fault, followed by a dextral reactivation at ca. Maps showing the location (a) and general geology (b) of Jiaodong; Geologic maps showing the Sanshandao-Cangshang belt (c) and sampling localities (d); CN: China, NK: North Korea, SK: South Korea, SCF: Sanshandao-Cangshang fault, JXF: Jiaojia-Xincheng fault, ZPF: Zhaoyuan-Pingdu fault, UHP: ultra-high pressure; the paleostress directions in Fig. Numbers in the parentheses after the sample number represent sampling depth. The Sanshandao Au deposit is hosted by the Sanshandao-Cangshang fault (SCF), and to its south are two mining camps (Xinli and Cangshang) (Fig. To its north, the fault extends into Bohai Bay, and recent exploration drilling discovered large orebodies with 470 tons Au resource in the undersea region. The ore bodies are commonly several meters thick and localized only in the footwall rocks.… continue reading »