某矽卡岩型銅矿床是在一比二万五千的金属量测量、磁法普查中发現的。在地质勘探过程中,进行了一比二千的綜合物、化探詳查工作。使用原生暈、磁法、激发电位、自然电場等方法均取得一定的地质效果。本文着重探討对地表和钻孔原生暈的初步研究的效果。一矿区位于一个地塹型复式向斜盆地的北西翼。黄銅矿体賦存于由矽卡岩組成之低山丘陵地带。其北部以海拔一千多米的中、高山为 A skarn-type copper deposit was found in a magnetometry survey of a metal volume of 25,000. In the geological exploration process, carried out a complex of 2,000, geochemical exploration work. Using primary halo, magnetic method, excitation potential, natural electric field and other methods have achieved some geological results. This article focuses on the effect of primary studies on surface and borehole primary halo. The first mine is located on the north west wing of a graben syncline basin. Chalcopyrite occurs in the hilly region of skarn. Its northern elevation of more than 1000 meters in the mountains