南金山金矿是在化探基础上,经过初步普查和详细普查后发现和肯定的。现已具中型规模,据目前情况看,该矿床还有一定潜力。南金山金矿床。位于甘肃北山肃北县的北部,交通方便。大地构造位置属天山地穹系东端。矿区地层主要为下石炭统柳园组碎屑—火山碎屑岩建造;该区金元素背景值特高,由于断裂构造、变质热液的作用。使金元素发生迁移、富集,形成了金矿床。甘肃北山区地洼期的主要特点之一,是断裂构造非常发育,因而形成一系列断陷小盆地和古生代、前古生代构造层的隆起和错位。根据地洼学成矿理论分析,本区应当是有利的多 The South Jinshan Gold Mine was discovered and affirmed on the basis of geochemical exploration after preliminary census and detailed census. Now with a medium-sized, according to the current situation, the deposit has some potential. South Jinshan gold deposit. Located in the northern part of Gansu Beishan Subei County, accessibility. The structure of the earth belongs to the eastern end of the dome of the Tianshan Mountains. The strata of the mining area are mainly composed of the Lower Carboniferous Liyuan Formation clastic-pyroclastic rocks. The gold background in this area is extremely high due to the fault structure and metamorphic hydrothermal fluids. The migration of gold elements, enrichment, formed a gold deposit. One of the main features of the diwa period in the Beishan area of ​​Gansu is that the fault structure is very well developed, thus forming a series of uplift and dislocation of a series of fault depression small basins and Paleozoic and pre-Paleozoic structural strata. According to the study of depression and study of mineralization, the district should be more favorable