Geochemical Characteristics of Lamprophyre from the TaoyuanXiaotongjiapuzi Gold Ore Belt and Their Geological Significance;
辽宁桃源-小佟家堡子金矿带煌斑岩的地球化学特征及地质意义
The Xiaotongjiapuzi gold deposit is hosted in Dashiqiao Formation of Liaohe Group.
小佟家堡子金矿床产于辽河群大石桥组三段第四、五层之间的互层带和大石桥组三段五层与盖县组地层的接触面上。
The Xiaotongjiapuzi gold deposit is hosted in the interlayered horizon of Upper Dashiqiao Formation marble and its overlying Lower Gaixian Formation schist of Liaohe Group.
小佟家堡子金矿床产于辽河群大石桥组顶部薄层大理岩与上覆盖县组底部片岩的“互层带”内，属原始沉积、变质富集、岩浆改造型多因复成矿床。
Located in gold concentration area of eastern Liaoning Province, the Xiaotongjapuzi gold deposit is hosted by fine-grained leptite and marble of Paleoproterozoic metamorphosed sequence.
小佟家堡子金矿床位于辽东金矿集中区 ,为产于古元古代变质岩系中的微细粒浸染型金矿 ,矿床类型独特。