甘肃省柳园镇辉铜山铜矿地质特征及外围潜力评价区评价
|
摘要
通过对辉铜山铜矿成矿地质特征、构造控矿特征及矿区外围潜力评价区地质特征的对比研究,总结了辉铜山铜矿的地质特征、成矿规律、矿床成因及找矿标志等。同时运用相似类比理论将评价区与辉铜山铜矿的大地构造位置、地球化学异常、地层、构造、围岩蚀变等地质特征进行对比,发现评价区的一系列地质特征均与辉铜山铜矿床的地质特征有很多相同或相似性,显示出评价区具有极大的找矿潜力。
Through the comparative study of the geological characteristic-s of mineralization,characteristics of structural ore-control of Huitongshan copper mine and the geological characteristics of peripheral potential assessment area,the geological characteristics,mineralization law and ore genesis of Huitongshan copper mine are concluded. By comparing the geological characteristics including geotectonic location,geochemical anomaly,stratum,structure and wall rock alteration between the assessment area and Huitongshan copper mine applying the analog theory of similarity,we found there existed many similarities,which proved that the evaluation area has great prospecting potential.
Through the comparative study of the geological characteristic-s of mineralization,characteristics of structural ore-control of Huitongshan copper mine and the geological characteristics of peripheral potential assessment area,the geological characteristics,mineralization law and ore genesis of Huitongshan copper mine are concluded. By comparing the geological characteristics including geotectonic location,geochemical anomaly,stratum,structure and wall rock alteration between the assessment area and Huitongshan copper mine applying the analog theory of similarity,we found there existed many similarities,which proved that the evaluation area has great prospecting potential.
引文
[1]龚全胜,刘明强,李海林等.2002.甘肃北山造山带类型及基本特征.西北地质,35(3):28-34
[2]龚全胜,刘明强,梁明宏等.2003.北山造山带大地构造相及构造演化.西北地质,36(1):11-17
[3]江思宏,聂凤军,陈文等.2003.甘肃辉铜山铜矿床燕山期钾长花岗岩的发现及其地质意义.矿床地质,22(2):185-194
[4]江思宏,聂凤军.2006.北山地区花岗岩类的40Ar/39Ar同位素年代学研究.岩石学报,22(11):2719-2732
[5]梅华林,李惠民,陆松年等.1999.甘肃柳园地区花岗质岩石时代及成因.岩石矿物学杂志,18(1):14-17
[6]穆治国,刘驰,黄宝玲,等.1992.甘肃北山地区同位素定年与构造岩浆热事件.北京大学学报(自然科学版),28(4):486-497
[7]聂凤军,江思宏,白大明,王新亮,苏新旭,李景春,刘妍,赵省民.2002.北山地区金属矿床成矿规律及找矿方向.北京:地质出版社,1-408
[8]张新虎.1993.甘、青、蒙祁连山、北山造山带构造地层演化史.甘肃地质学报,8(1):80-86
[9]邱林林,李雪涛.甘肃省瓜州县辉铜山铜矿矿床成因及找矿潜力分析[J].世界有色金属,2018(01):82-83.
[10]左国朝,何国琦.1990.北山板块构造及成矿规律.北京:北京大学出版社,1-209
[11]曹新志,王燕.成矿预测方法的理论基础及分类(J).地质科技情报,1993,12(1):69-72.
[12]梁祥济.中国矽卡岩和矽卡岩矿床形成机理的试验研究(M).北京:学苑出版社,2000:91-116.
[13]路凤香,桑隆康.岩石学(M).北京地质出版社,2002:285-287
[14]马生明,朱立新.甘肃北山辉铜山铜矿地球化学异常结构研究.(J).32(4):405-412
[15]徐明钻.北山地区典型Cu矿中元素地球化学分布规律及成矿预测方法技术研究[D].中国地质科学院,2011.
[2]龚全胜,刘明强,梁明宏等.2003.北山造山带大地构造相及构造演化.西北地质,36(1):11-17
[3]江思宏,聂凤军,陈文等.2003.甘肃辉铜山铜矿床燕山期钾长花岗岩的发现及其地质意义.矿床地质,22(2):185-194
[4]江思宏,聂凤军.2006.北山地区花岗岩类的40Ar/39Ar同位素年代学研究.岩石学报,22(11):2719-2732
[5]梅华林,李惠民,陆松年等.1999.甘肃柳园地区花岗质岩石时代及成因.岩石矿物学杂志,18(1):14-17
[6]穆治国,刘驰,黄宝玲,等.1992.甘肃北山地区同位素定年与构造岩浆热事件.北京大学学报(自然科学版),28(4):486-497
[7]聂凤军,江思宏,白大明,王新亮,苏新旭,李景春,刘妍,赵省民.2002.北山地区金属矿床成矿规律及找矿方向.北京:地质出版社,1-408
[8]张新虎.1993.甘、青、蒙祁连山、北山造山带构造地层演化史.甘肃地质学报,8(1):80-86
[9]邱林林,李雪涛.甘肃省瓜州县辉铜山铜矿矿床成因及找矿潜力分析[J].世界有色金属,2018(01):82-83.
[10]左国朝,何国琦.1990.北山板块构造及成矿规律.北京:北京大学出版社,1-209
[11]曹新志,王燕.成矿预测方法的理论基础及分类(J).地质科技情报,1993,12(1):69-72.
[12]梁祥济.中国矽卡岩和矽卡岩矿床形成机理的试验研究(M).北京:学苑出版社,2000:91-116.
[13]路凤香,桑隆康.岩石学(M).北京地质出版社,2002:285-287
[14]马生明,朱立新.甘肃北山辉铜山铜矿地球化学异常结构研究.(J).32(4):405-412
[15]徐明钻.北山地区典型Cu矿中元素地球化学分布规律及成矿预测方法技术研究[D].中国地质科学院,2011.