吉林大学学报(地球科学版) ›› 2021, Vol. 51 ›› Issue (6): 1613-1635.doi: 10.13278/j.cnki.jjuese.20200248
• 地质与资源 • 下一篇
刘建民1,2, 赵国春3, 徐刚1,2, 邱海成4, 李建锋1,2, 肖昌浩1,2, 沙德铭5, 刘福兴6, 毕广源3, 房兴1,2,3, 张家奇3, 郭祺3, 于婳3
Liu Jianmin1,2, Zhao Guochun3, Xu Gang1,2, Qiu Haicheng4, Li Jianfeng1,2, Xiao Changhao1,2, Sha Deming5, Liu Fuxing6, Bi Guangyuan3, Fang Xing1,2,3, Zhang Jiaqi3, Guo Qi3, Yu Hua3
摘要: 辽东半岛地处华北克拉通东北部、胶-辽台隆北段,是我国东部重要的金矿资源产区之一。区内先后发现五龙、白云、猫岭等大中型金矿床,探明储量超过300 t。鉴于辽东半岛与胶东半岛处于相似的构造背景,辽东半岛金矿成矿及找矿潜力一直广受关注,相关的地质研究及矿产勘查工作也持续进行。总体看,已有研究更多聚焦于金矿床本身的描述及矿床成因等方面的工作,但缺乏对区域成矿背景及成矿过程的全面梳理,在一定程度上制约了深部资源勘查工作的方向及部署。作者根据2016-2019年间的野外地质调查,结合区域成矿地质背景、含矿岩石显微构造变形和年代学等方面的分析,系统总结了辽东半岛金矿的成矿条件和控矿因素,并就深部资源勘查方向提出了建议。研究表明:辽东半岛已发现金矿化分属于晚三叠世和早白垩世两期构造-岩浆成矿系统。宏观及微观上,构造对区内金矿的形成和分布均表现出明显的控制作用。两个时期的金矿都经历了早期的韧性变形和晚期的脆性变形,且金矿化都与晚期脆性构造环境下发育的超碎裂岩化及含矿热液蚀变作用有关。基于辽东半岛地壳结构、物质组成和金矿成矿地质条件的分析,本文认为辽东半岛的深部资源勘查应重点集中在3个方向:营口-宽甸台拱的南、北边界断裂带及其伴随的北东、北西向断裂构造的复合部位;营口-宽甸台拱的东、西两侧北东向(新华夏系)边界断裂带及其伴随的低级别、低序次构造系统;关注在现有含矿构造带下部是否存在与印支期、燕山期岩浆活动有关的斑岩型金矿化(床)。
中图分类号:
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