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山西省灵丘县马坡—山神庙锰银矿床是一个以锰银为主,伴生有铅锌的多金属矿床。矿床地处燕辽台褶带西端,受燕山期火山活动和断裂构造控制明显,矿体赋存呈似层状、透镜状或脉状产出。矿体富集规律显示,矿体中的锰银铅锌等矿源来自长城系高于庄组的白云岩地层,经中生代火山活动使矿质富集于火山构造周围的断裂带中,属于沉积—热液改造型锰银矿床。锰银矿是我国的稀缺矿种,用途广泛。通过对马坡—山神庙锰银矿床的市场分析、资源分析和建矿条件分析,均表明马坡—山神庙锰银矿具有广阔的市场前景、良好的资源保障和有利的建矿条件,其资源开发前景良好。
Lingqiu County, Shanxi Province, Ma slope - Temple of the Shan-Shan Manganese silver deposit is a manganese-based, accompanied by lead-zinc polymetallic deposits. The deposit is located at the western end of the Yanliaotai fold belt. It is obviously controlled by the volcanic activity and fault structure of the Yanshan Period. The ore bodies are layered and lenticular or vein-shaped. The ore body enrichment law shows that the manganese, silver, lead, zinc and other ore bodies in the orebody come from the dolomite formation of the Gaozhuangzhuang Formation of the Great Wall and are enriched by the Mesozoic volcanic activity in the fault zone around the volcano structure. Liquid modified manganese silver deposit. Manganese silver mine is China’s scarce minerals, a wide range of uses. Based on the market analysis, resource analysis and construction conditions analysis of the Magup-Shanmianmiao manganese-silver deposit, it is indicated that the Magup-Shanmusi manganese silver deposit has broad market prospects, good resource guarantee and favorable conditions for the construction of ore , Its resource development prospects are good.