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华北板块接触交代型铁矿成矿规律及成矿预测
引用本文:丁俊德.华北板块接触交代型铁矿成矿规律及成矿预测[J].地质找矿论丛,1986(3):18-28.
作者姓名:丁俊德
作者单位:华北有色地质勘探公司
摘    要:接触交代型铁矿在我国铁矿床类型中占有较重要的地位。华北板块区接触交代型铁矿在我国该类型铁矿中,不论在探明储量和研究程度上均取得很大进展。目前本区该类型矿床的地质研究及找矿工作已近尾声,但仍有很多问题尚待进一步深入,新区的找矿工作有待于老区工作经验的借鉴。因此,进一步总结和提高认识仍有必要。本文将着重从区域和矿床成矿规律及预测成矿有望地区略加探讨。不正之处,请予指正。一、控矿围岩


THE METALLOGENIC REGULARITY AND PROGNOSIS OF THE CONTACT METASOMATICTYPE IRON ORE DEPOSITS IN NORTH CHINA PLATE AREA
Ding Junde.THE METALLOGENIC REGULARITY AND PROGNOSIS OF THE CONTACT METASOMATICTYPE IRON ORE DEPOSITS IN NORTH CHINA PLATE AREA[J].Contributions to Geology and Mineral Resources Research,1986(3):18-28.
Authors:Ding Junde
Abstract:This paper deals with ore-controlling country rock, ore field structure, ore deposit distribution regularity, metallogenic models and metalloge nic prognosis of the contact metasomatic-type iron deposits in western Shandong, both sides of Taihang mountain and Yanshan metageosynclinal district in North China plate area, placing an emphasis on the ore-con trolling function of the country rocks.The ore field is situated in the rift basin at the side of the rift valley belt.Yanshanian magmatic rocks are ore-forming parent rocks and the original magma is related to basic rocks or ultrabasic rocks.Three stages might be classified according to the intrusive sequence.Iron ores are associated with inter mediate-acidic(with some basic) rocks or intermediate-acidic (with some alkaline) rocks of early-middle stage, and Mo-, Cu-, Au-bearing hy-drothermal vein deposits commonly associated with alkaline rocks of late stage.Old latitudinal structures in basement might function as channels for magma.Neocathaysian tectonics of upper cover is rock-controlling structure.It is believed that the interlayer weak zone within the cover provides favourable space for magmatic intrusion.Magmatic body appears as a laccolith.The equidistant or grating distribution of the cover bed structure resulted from wavy transmission of the stress provides a helpful indication for the prognosis of ore deposits, and six prospects for exploration are thus suggested by the auther.
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