陕西省镇坪县红阳萤石矿成矿模式

红阳萤石矿主要受构造及岩浆岩控制,工作区位于秦岭构造带南部北大巴山构造带,通过探讨区域地层岩性、岩浆岩条件和构造控制作用等,结合工作成果,归纳总结该地区控矿地质因素,通过对区域上闹阳坪萤石矿典型矿床成矿模式的分析研究,有助于更好的掌握工作区的成矿地质背景和控矿条件,进而提高找矿效率,实现找矿突破。

Hongyang fluorite mine is mainly controlled by structure and magmatic rock.The working area is located in the southern part of the Qinling Orogenic Belt.By discussing the lithology of regional strata,magmatic rock conditions and tectonic control,based on work results,the ore-controlling geological factors in this area are summarized.The metallogenic model of typical fluorite deposit in upper Naoyangping fluorite mine is analyzed.It is helpful to more effectively grasp the ore-forming geological background and ore-controlling conditions of the working area,so as to improve the efficiency of prospecting and achieve a breakthrough in prospecting.