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作 者:杜远生[1,2,3] 余文超 张亚冠[1] Du Yuan-Sheng;Yu Wen-Chao;Zhang Ya-Guan(School of Earth Sciences,China University of Geosciences(Wuhan),Wuhan 430074,China;State Key Laboratory of Biogeology and Environmental Geology,Wuhan 430074,China;Engineering Technology Innovate center of Resource Exploration in basement area of China Ministry of Natural Resources,Guiyang 550004,China)
机构地区:[1]中国地质大学(武汉)地球科学学院,湖北武汉430074 [2]生物地质与环境地质国家重点实验室,湖北武汉430074 [3]自然资源部基岩区矿产资源勘查工程技术创新中心,贵州贵阳550004
出 处:《古地理学报》2020年第4期601-619,共19页Journal of Palaeogeography:Chinese Edition
基 金:国家自然科学基金项目(编号:U1812402);中国地调局项目(编号:12120114016501和12120114016701);国土资源部公益类项目(编号:201411051);贵州省锰矿资源预测评价科技创新人才团队等项目联合资助。
摘 要:矿产沉积学是一个沉积学与矿床学交叉而形成的新的学科方向。矿产沉积学属于应用基础学科,主要任务是应用沉积学(沉积动力学、流体动力学、物理化学、微生物沉积学等)的基本原理,探讨成矿元素的迁移-聚集机理和成矿颗粒的风化-搬运-沉积过程,从而恢复沉积矿产的古环境(沉积环境、古盐度、古碱度、古氧化还原条件)和形成背景(沉积盆地、古地理、古气候等),最终目的是确定矿床成因、成矿规律,建立成矿模式和找矿模型,进行成矿预测,为沉积矿产的找矿勘探提供科学依据。同时将成矿事件与重大地质事件相结合,揭示重大地质事件与成矿事件的耦合关系。Ore sedimentology is a new interdisciplinary research direction based on the combination of sedimentology and ore deposit geology.Ore sedimentology belongs to applied fundamental research and its main task is to apply the basic principles of applied sedimentology(sedimentation dynamics,fluid dynamics,physics,chemistry,and microbial sedimentology)to explore the transfer and accumulation of ore-forming elements and the weathering-transportation-deposition process of ore-forming particles.After obtaining above-mentioned information,we can reconstruct the palaeoenvironment factors of sedimentary ore deposits(e.g.,sedimentary environment,palaeosalinity,palaeo-alkalinity,palaeo-redox)and their forming background(e.g.,sedimentary basin,palaeogeography,palaeoclimate).This research aims at providing scientific basis for prospecting of sedimentary ore deposits.To achieve this goal,we need to constrain the origin of ore deposits,summarize the ore-forming rules,build the ore depositional and the prospecting model.Our study cases indicate that there were couplings between the sedimentary ore-forming events and important key geological events.
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