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乌伊岭地区铜金多金属矿床特征及成矿规律研究

Characteristics and Metallogenic Regularity of Copper-Gold Polymetallic Deposits in Wuyiling,Heilongjiang Province
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摘要 研究区处于黑龙江省小兴安岭-张广才岭成矿带北端与佳木斯隆起成矿带北端之结合部位,但以前者为主,具备两大成矿带的成矿特征。由于多期次的构造运动、频繁的岩浆活动,使本带成为我省最主要的铜、金、铁、钨、钼等贵金属—多金属共生的成矿带。本文将通过对研究区的地层、岩浆岩、构造以及区域矿产特征等方面的研究,基以研究其成矿规律、控矿因素,建立找矿模型,希望对未来的找矿工作略尽绵力。 The study area is in xiaoxinganling - far north ZhangGuangCaiLing metallogenic belt and jiamusi uplift metallogenic belt of combining site, but is given priority to with the former, with two metallogenic characteristics of metallogenic belt. Because many times of tectonic movement, frequent magmatic activity, make this belt in our province's main copper, gold, iron, tungsten, molybdenum and other precious metals - polymetallic metallogenic belt of symbiosis. This article through the study on the strata, magmatic rocks, structure and regional mineral characteristics and so on, to study the metallogenic regularities, ore controlling factors, prospecting model is set up, in the hope of making minor contributions for future prospecting work.
作者 吕澜清 LV Lanqing(College of Earth Sciences, Chengdu University of Technology, Chengdu 610059, China)
出处 《四川有色金属》 2019年第1期35-37,共3页 Sichuan Nonferrous Metals
关键词 地质构造 热液成因 成矿规律 控矿因素 找矿模型 Geological structure Hydrothermal genesis Metallogenic regularity Ore-controlling factors Pros-pecting model
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