松辽盆地西南部钱家店矿山地质条件及成矿作用分析OA
Analysis on metallogenic geological conditions and mineralization of Qianjiadian sandstone type in southwest Songliao Basin
钱家店矿床位于松辽盆地西南部的钱家店凹陷以内,是我国在东部地区发现的首个超大型矿床.但是,关于钱家店矿床的成矿地质条件及成矿作用模式一直存在争论,因此,理清控制成矿因素,明确成矿作用模式,将有效地指导同类型矿床的勘查,有利于在松辽盆地西南部更好地进行矿床研究.本文通过对钱家店矿床的构造、古气候环境、沉积相和砂体等进行研究,探索其与钱家店成矿的关系,理清了其对成矿的影响,明确了钱家店矿床的成矿地质条件及成矿作用,由此相应建立了多成因多阶段的"沉积成矿预富集-层间氧化下渗成矿-富集成矿-还原护矿"四阶段成矿模式.
The Qianjiadian deposit is located in the Qianjiadian sag in the southwest of Songliao Basin.It is the first super large sandstone type deposit found in the eastern part of our country.However,the metallogenic geological conditions and metallogenic mode of Qianjiadian deposit have been controversial.Therefore,clarifying the controlling factors of mineralization and clarifying the metallogenic mode will effectively guide the exploration of similar sandstone deposits,which is conducive to better study of sandstone deposits in the southwest of Songliao Basin.In this paper,the structure,paleoclimatological environment,sedimentary facies and sand body of the Qianjiadian deposit are studied to explore its relationship with the Qianjiadian sandstone type mineralization,clarify its influence on mineralization,and clarify the metallogenic geological conditions and mineralization of the Qianjiadian deposit.Accordingly,the four-stage ore-forming model of"sedimentary and diagenetic preenrichment-interlayer oxidation infiltration mineralization-oil-gas modification enrichment-oil-gas reduction protection"was established.
吴修俣
东华理工大学地球科学学院,江西 南昌 330013
地质学
松辽盆地钱家店矿床成矿地质条件
Songliao BasinQianjiadian depositMetallogenic geological condition
《世界有色金属》 2024 (7)
61-63,3
评论