论文部分内容阅读
蓬家夼金矿赋存于中生界莱阳组和下元古界荆山群之间的剥离断层中，矿体产出严格受层间滑脱断层带控制，矿体的厚大部位产在层间滑脱断层产状由陡（４５°～５０°）变缓（１５°～２０°）处。通过对蓬家夼金矿田家矿区东西两翼成矿地质条件的研究，认为山西段和东井口段同样是成矿有利地段，应进行详细勘探。
The Pengjiajing gold deposit occurs in the peel faults between the Laiyang Formation and the Lower Proterozoic Jingshan Group in the Mesozoic. The ore body output is strictly controlled by the inter-strata detachment fault zone. The fault shape is steep (45 ° ~ 50 °) slowed down (15 ° ~ 20 °). Through the research on the geological conditions of the east and west flanks of the Pengjialuo gold orefield, it is considered that the Shanxi section and the Dongjingkou section are also the favorable metallogenic sections and should be explored in detail.