辽东半岛金矿成矿作用与深部资源勘查

doi:10.13278/j.cnki.jjuese.20200248

Abstract

Abstract: Located in the northeast of North China craton and the northern part of Jiao-Liao uplift, Liaodong Peninsula is one of the important gold resource producing areas in East China, where several large and medium sized gold deposits are developed including those occurred in Wulong, Baiyun, and Maoling areas with proven reserves up to more than 300 t. Because of the similarity of the geological and tectonic settings between Jiaodong Peninsula and Liaodong Peninsula, the gold mineralization and prospecting potential in Liaodong Peninsula has received attention, and the research on the mineralization settings and typical gold deposits has been going on. However, the lack of a systematic understanding of the relationship between the regional metallogenic geological settings and mineralization process restricts the deployment of deep resource exploration. Based on the investigation over the years of 2016-2019 on the geology and geochronology of the gold deposits, as well as the comprehensive analysis of the microstructural deformation and geochronology of the ore-related rocks, we discussed the ore-forming geological conditions of the gold deposits in Liaodong Peninsula. The results show that the discovered gold deposits in Liaodong Peninsula may be related to the two episodes of tectono-magmatic-ore forming systems in the Late Triassic and Early Cretaceous. The two kinds of gold mineralization are controlled by different structural patterns, macro-and microscopically. The gold ores are mainly formed under the brittle or brittle-shear deformation conditions with the extensive occurrences of ore-bearing clastic flows, caused by both a repetitive sequence of brittle or brittle-shear failure along the major fault systems and the related magmatic hydrothermal activities in the Late Triassic and Early Cretaceous. This genetic origin of the gold mineralization and ore-bearing clastic flows may support the idea of flashing vaporization by earthquakes in the mesothermal gold-bearing systems. We suggest that the exploration of the deep resources should target three regions:The north and south boundary fault zones of the Yingkou-Kuandian uplift and the structural composite sites between the north and south boundary fault zones and the accompanying NE or NW-trending fault zones;The main NE-trending fault zones and the accompanying lower or secondary structural systems along the east and west boundary of the Yingkou-Kuandian uplift; deep in the existing ore-bearing structural belt,where it is necessary to pay attention to the existence of porphyry-type gold mineralization (deposit) which is related to the magmatic activities of Indosinian and Yanshanian periods.

Key words: metallogenisis of gold deposits, structural control on gold mineralization, chronology for ore-forming, exploration for the deep resources, Liaodong Peninsula

CLC Number:

P613

Liu Jianmin, Zhao Guochun, Xu Gang, Qiu Haicheng, Li Jianfeng, Xiao Changhao, Sha Deming, Liu Fuxing, Bi Guangyuan, Fang Xing, Zhang Jiaqi, Guo Qi, Yu Hua. Metallogenesis of Gold Deposits and Deep Exploration in Liaodong Peninsula[J].Journal of Jilin University(Earth Science Edition), 2021, 51(6): 1613-1635.

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Metallogenesis of Gold Deposits and Deep Exploration in Liaodong Peninsula

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