地幔亚热柱-幔枝构造演化及其对金的成矿控矿作用模式OACHSSCD
The Structural Evolution of Submantle Plume-Mantle Branch Structures and Its Role in Gold Mineralization and Ore Control Mechanisms
为揭示深部成矿规律,文章建立了幔枝构造背景下的成矿控矿模式,系统分析了金的物质来源与运移通道、构造控矿作用及岩浆活动对成矿的影响.该模式清晰展示了幔枝构造从地球深部到浅部分阶段、分类型形成不同金矿床的过程,具有重要理论研究价值;同时为断裂构造带及岩浆接触带等有利区域的找矿提供指导,助力深部矿产资源发现.此外,银矿及铜、铅、锌多金属矿的成矿特点与金相似,可为其他多金属矿床成矿模式研究提供参考.
To elucidate the deep mineralization mechanisms,this study establishes a metallogenic control model within the context of mantle branch structures,systematically analyzing the influence of gold's material sources and migration pathways,tectonic control,and magmatic activity on mineralization.The model clearly illustrates how mantle branch structures form distinct gold deposits in stages and across different types from the Earth's deep to shallow regions,holding significant theoretical value;it also provides guidance for prospecting in favorable areas such as fault zones and magmatic contact zones,facilitating the discovery of deep mineral resources.Furthermore,the mineralization characteristics of silver deposits and polymetallic deposits(copper,lead,zinc)are similar to those of gold,offering insights for studying the metallogenic patterns of other polymetallic deposits.
牛树银;张建珍;宋明春;陈超;陶光活;李杰;马宝军
河北地质大学,河北 石家庄 052161河北地质大学,河北 石家庄 052161河北地质大学,河北 石家庄 052161河北地质大学,河北 石家庄 052161河北省地质调查院,河北 石家庄 050000河北地质大学,河北 石家庄 052161河北地质大学,河北 石家庄 052161
天文与地球科学
幔枝构造成矿控矿模式金矿床银及多金属矿深部成矿规律
mantle branch structuresmineralization control modelgold depositssilver and polymetallic depositsdeep mineralization patterns
《河北地质大学学报》 2026 (4)
56-59,4
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