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新立金矿床地处渤海莱州湾畔，含矿蚀变带隐伏于海水之下，矿床位于三山岛断裂带（主要控矿断裂）由ＮＥ向转为ＮＥＥ向的拐弯部位。三山岛、仓上金矿床也分布在该断裂带拐弯地段。根据胶东地区金矿主要受ＮＥ向断裂控制，构造产状变化或构造交汇部位易于成矿，以及金矿床具有等距分布的特点，今后找矿的重点地段应是仓上金矿床北部和芙蓉岛—潘家屋子一带。
The Xinli gold deposit is located at the bank of Laizhou Bay in the Bohai Sea. The ore-bearing alteration zone is hidden under sea water. The deposit is located at the turning point from NE to NEE in the Sanshan Island fault zone (the main ore-controlling fault). Sanshandao, Cangshang gold deposits are also distributed in the corner of the fault zone. According to the fact that the gold deposits in Jiaodong area are mainly controlled by the NE-trending faults, structural tectonic changes or structural metallogenetic intersections are easy to be formed and the gold deposits are equidistantly distributed, the key areas for prospecting in the future should be the northern part of Cangshang Gold Deposit and Huron Island - Panjia house area.