阜平—五台幔枝构造的时空结构及其对区域岩浆与金属成矿的控制作用  

The Spatio-temporal Structure of Fuping—Wutai Mantle Branch Structure and Its Control on Regional Magmatism and Metal Mineralization

作　　者：张聚全 陈超 张福祥 王晨光 郭海全 张才龙 范起超 邢欢 ZHANG Ju-quan;CHEN Chao;ZHANG Fu-xiang;WANG Chen-guang;GUO Hai-quan;ZHANG Cai-long;FAN Qi-chao;XING Huan(Postdoctoral Research Station of Hebei Bureau of Geology and Mineral Resources Exploration and Development,Shijiazhuang 050051,China;Hebei GEO University,Shijiazhuang 050031,China;Hebei Bureau of Geology and Mineral Resources Exploration and Development,Shijiazhuang 050051,China)

机构地区：[1]河北省地质矿产勘查开发局博士后科研工作站,河北石家庄050051 [2]河北地质大学地球科学学院,河北石家庄050031 [3]河北省地质矿产勘查开发局,河北石家庄050051

出　　处：《河北地质大学学报》2023年第4期72-79,共8页Journal of Hebei Geo University

基　　金：河北省地质矿产勘查开发局博士后项目(13000023P00F664100037);河北地质矿产勘查开发局科研项目(13000022P00329410103R);河北科技厅重点研发项目(22374201D);河北省自然科学基金资助项目(D2021403028,D2015403013)。

摘　　要：幔枝构造是牛树银团队提出的地幔热柱的第三级构造单元,很好地解释了华北地区内生金属矿床的时空分布规律,并在地质找矿中得到进一步的实践和证明。对位于太行山中—北段和五台山—恒山地区的阜平—五台幔枝构造的三维空间、形成时代、成矿特征与控矿作用进行讨论,并建立了其成矿系统模型,为区域找矿勘查提供技术支撑。The mantle branch structure is the third-level structural unit of the mantle plume,proposed by the team of Niu Shuyin,which well explains the temporal and spatial distribution of endogenous metal deposits in North China,and has been further practiced and proved in geological prospecting.In this paper,the three-dimensional space,formation age,metallogenic characteristics and mineralization control of the Fuping—Wutai mantle branch structure located in the middle—northern section of the Taihang Mountains and the Wutaishan—Hengshan area are discussed,and a model of its mineralization system is established,which provide technical support for regional mineral exploration.

关 键 词：幔枝构造 金矿成矿 地幔热柱 成矿规律 

分 类 号：P611[天文地球—矿床学]