对内华达杰里谷地区金矿床的地质、地球化学、流体包裹体和稳定同位素的综合研究表明:该类矿床的金是通过流体混合及主岩中铁的硫化作用而沉淀的.这些矿床矿石沉淀过程中的化学反应途径模式表明,借助于流体混合,(包括矿液的同时冷却、稀释、氧化和与围岩反应)以及主岩中活性铁的硫化作用,可以解释在杰里谷地区及其他许多沉积岩中浸染型金矿床内所见到的自然金的浸染状产出状态,微细的颗粒、蚀变分带、矿物学和地球化学等现象. A comprehensive study of the geology, geochemistry, fluid inclusions and stable isotopes of the gold deposits in the Jelili Valley, Nevada shows that the gold in this deposit is precipitated by fluid mixing and sulfidation of iron in the host rock, The chemical reaction pathway model shows that the fluid-mixing (including the simultaneous cooling, dilution, oxidation and reaction of surrounding rock) and the sulfidation of active iron in the host rock can be explained by the fluid mixing in the Jilli Valley and many other sedimentary rocks Disseminated gold deposits seen in the natural gold disseminated output state, fine particles, alteration zoning, mineralogy and geochemistry and so on.