首页|期刊导航|世界有色金属|陕西省石泉县柿子沟金矿地质特征及控矿因素浅析

陕西省石泉县柿子沟金矿地质特征及控矿因素浅析OA

Geological Characteristics and Ore Controlling Factors of Shizigou Gold Deposit in Shiquan County,Shaanxi Province

中文摘要英文摘要

石泉县柿子沟金矿位于陕西省石泉县北西,大地构造位置位于扬子板块舟曲-安康早古生代裂谷(O-S)(III12),属于石泉~安康金锰成矿小区,具有有利的成矿条件.通过地质、化探、探矿工程等工作方法和手段,初步查明了矿区的成矿地质条件.在下志留系梅子垭组炭质片岩段内圈定了两条矿化蚀变带,并在带内圈定多条金矿(化)体;矿化蚀变带、矿(化)体受中下志留统梅子垭组地层、F5 韧性剪切构造控制.地球化学异常与地层、构造等分布位置耦合显著,具备韧性剪切带控制的沉积-变质热液型矿床成矿潜力.

The Shizigou gold deposit in Shiquan County,Shaanxi Province,is located in the northwest of the county.Its tectonic position is in the early Paleozoic rift(O-S)(III12)of the Yangtze Plate,from Zhouqu to Ankang.It belongs to the Shiquan Ankang gold manganese mineralization zone and has favorable mineralization conditions.Through geological,geochemical,and exploration engineering methods and means,the ore-forming geological conditions of the mining area have been preliminarily identified.Two mineralized alteration zones have been identified within the carbonaceous schist section of the Meiziya Formation in the Lower Silurian,and multiple gold(mineralized)bodies have been identified within these zones;The mineralized alteration zone and mineralized body are controlled by the Lower Silurian Meiziya Formation and F5 ductile shear structure.The coupling of geochemical anomalies with the distribution of strata,structures,and other factors is significant,indicating the potential for mineralization of sedimentary metamorphic hydrothermal deposits controlled by ductile shear zones.

付银攀;马国华;袁贇斐

中国冶金地质总局西北地质勘查院,陕西 西安 710119中国冶金地质总局西北地质勘查院,陕西 西安 710119中国冶金地质总局西北地质勘查院,陕西 西安 710119

天文与地球科学

柿子沟金矿地质特征控矿因素沉积-变质热液型矿床

Shizigou Gold MineGeological featuresMineral control factorsSedimentary metamorphic hydrothermal deposit

《世界有色金属》 2026 (14)

92-94,3

陕西省地质勘查基金项目《陕西省石泉县柿子沟一带金矿普查》(编号:61202110397).

评论