黑龙江洋灰洞子铜多金属矿床地处兴蒙造山带东段、吉黑褶皱带北部太平岭隆起带与老黑山断陷复合部位。为了揭示其成矿规律和成矿潜力,开展了区域成矿规律与成矿预测的研究工作。在分析洋灰洞子铜多金属矿床成矿地质背景和矿床地质特征的基础上,发现区内元素的区域分布规律为:区内北部以寻找Sn、Mo矿为主,南部则寻找Cu、Pb、Zn矿为主。在此基础上,初步确定了3个重点普查找矿靶区:二段林场Cu、Pb、Zn多金属普查靶区,杨木林Pb、Zn矿普查靶区和路明山Sn、Mo多金属普查靶区。
Yanghuidongzi copper-polymetallic deposit in the province is located in anoverlapped area where three regions ,the eastern part of the Xingmeng orogenic belt ,Taipingling uplift in the north of Jihei fold belt and the Laohe-ishan depression meet .In order to reveal its metallogenic regularity and mineralization potentiality ,research on regional mineralization regularity and mineralization prediction is on the move .The regional distribution pattern of elements through the analysis of the metallogenic geological background and geological characteristics of Yanghuidongzi copper -polymetallic deposit is studied and the results show that the northern area is mainly for Sn ,Mo ore and the southern ar-ea for Cu,Pb,Zn ore.Based on this evidence it will make three prospecting targets:Cu,Pb,Zn polymetallicgeneral sur-vey target at Erduan forest area ,Pb,Zn general survey target at Yangmulin area and Lumingshan Sn ,Mo polymetallic-general survey target .
参考文献
[1] | 杨增武,董传统,夏统元,余友.黑龙江省洋灰洞子铜矿床地质特征及成因探讨[J].地质与勘探,2005(02):27-29. |
[2] | 孟兆贤.黑龙江省东宁县洋灰洞子铜矿床的成因探讨[D].长春:吉林大学地球科学学院,2012.,2012. |
[3] | 韩振新,徐衍强,郑庆道.黑龙江省重要金属和非金属矿产的矿床成矿系列及其演化[M].哈尔滨:黑龙江人民出版社,2003.,2003. |
[4] | 黑龙江省地质矿产局.黑龙江省区域地质志[M].北京:地质出版社,1993.,1993. |
[5] | 李光辉.黑龙江完达山-太平岭成矿带成矿系列与找矿预测[D].北京:中国地质大学(北京),2011.,2011. |
[6] | 芮宗瑶,施林道,方如恒.华北陆块北缘及邻区有色金属矿床地质[M].北京:地震出版社,1994:1-24.,1994. |
[7] | 祁进平,陈衍景,Franco PIRAJNO.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(02):47-59. |
[8] | 吕俊超,杨言辰,韩世炯,闫文强,张国宾,张本臣,赵清泉.黑龙江洋灰洞子铜矿床花岗闪长斑岩地球化学、锆石U-Pb定年及地质意义[J].世界地质,2014(01):59-75. |
[9] | 王恒亮,杨继权.黑龙江省东宁县桦木林场等四幅1:5万区域地质矿产调查报告[R].哈尔滨:黑龙江省区域地质调查所,2011.,2011. |
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