乌伊岭地区铜金多金属矿床特征及成矿规律研究
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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.
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.
引文
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[2]曲关生,浦全生,韩松山.黑龙江省岩石地层[M].中国地质大学出版社,2008.
[3]杨林楠,杨巍然.中国区域大地构造学[M].地质出版社,1985.
[4]任纪舜,黄汲清.中国大地构造及其演化[M].科学出版社,1980.
[5]韩振新,徐衍强,等.黑龙江省重要金属和非金属矿产的成矿系列及其演化[M].黑龙江人民出版社,2004.
[6]陶奎元.火山岩相构造学[M].江苏科学技术出版社,1991.
[7]赵春荆,彭玉鲸,党增欣,等.吉黑东部构造格架及地壳演化[M].辽宁大学出版社,1996.
[8]韩振新,郝正平,等.黑龙江省主要成矿带矿床成矿系列[M].哈尔滨工程大学出版社,1996.
[9]刘志逊,赵寒冬,马丽玲,等.小兴安岭晚石炭世花岗岩岩浆混合作用的岩相学证据及其地质意义[J].地质通报,2007:26(3):289~298.
[10]祁近平,陈衍景.东北地区浅成低温热液矿床的地质特征和构造背景[J].矿物岩石,2005,25(2):47~59.
[11]谭成印.黑龙江省主要金属矿产构造—成矿系统基本特征[D].北京中国地质大学,2009.