黑龙江省铁力地区钼（铜）矿床成矿地质条件及找矿潜力分析
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摘要
铁力地区位于伊春—延寿成矿带中部,西以逊克-铁力-尚志断裂为界,东临佳木斯地块。鹿鸣钼矿床是近年来新发现和正在勘查的Mo、Cu多金属矿床,矿床矿体产出于二长花岗岩、花岗斑岩岩体中,辉钼矿、黄铜矿等金属矿物呈浸染状、细脉浸染状赋存于蚀变二长岩(局部过渡为花岗斑岩)中,总体属于重要的斑岩型矿床,矿床规模达超大型(资源总量达60万吨);翠岭钼矿位于鹿鸣西侧3km,矿床矿体产出于花岗斑岩岩体中,矿床规模为小型。对区内钼铜矿床成矿地质条件与地质、地球物理、地球化学标志等研究表明,本区成矿地质条件优越,找矿标志明显,具备较好的找矿潜力。
本文从成矿地质背景分析入手,深入研究矿床地质特征、地球化学特征、成矿地质条件及其控矿机制,准确厘定了成矿岩体的形成时代,确定了该地区MoCu矿床的成因,建立成矿模式;根据成矿地质条件与地质、地球物理、地球化学测量结果研究,确定找矿标志,指明该区的找矿方向,确定后续找矿工作的预测靶区,研究成果对本地区的开展类似研究工作与部属钼铜多金属矿产勘查工作有重要指导意义。
Tieli area is located in the central south of the Yichun-Yanshou magma–structure belt which geostructure position is situated in the Songnen–Zhangguangcailing block and the Jiamusi–Xingkai block collisional belt. Its special tectonic setting and related activities of the intermediate-acid magmatic rocks provided conditions for the formation of molybdenum, copper, lead-zinc, gold and high-grade iron deposit in the study area.
Luming in the area molybdenum-copper deposit is a super large deposit which was recent discovered and investigated in recent years, the aspects of ore body was in the adamellite and the granite-porphyry, which belongs to the type of porphyry ore deposit. Cuiling in the area molybdenum-copper deposit was small, and it has the similar characteristics to those of Luming molybdenum-copper deposit, which is also belongs to the type of porphyry ore deposit. Studies on the granitic magmatic rock (monzonite, granite-porphyry) have shown the results that its generally belongs to the aluminium-oversaturated, high potassium calc-alkaline series I type granite. Based on the characteristics of major element, REE, trace element, isotope and regional geology, we believe that these molybdenum-copper deposits have been formed in a pull apart environment of the later syn-collision tectonic period. According to the measure of the age, The dateing of the La-ICP-MS zircon U-Pb indicates that these rock mass have been formed in the age of 174.0~178.3 Ma, and that belonged to the early period of mesozoic Yanshan Movement.
The exposed granite-porphyry of the northeastern study area has obvious differences with the fine porphyritic monzonitic-orthoclase granites of the south, and the former is associated with acidic volcanic rock, but the later has controlled the element anomalies such as Mo, Cu, Ag, Bi, Pb, As, Zn, etc. And also controlled the distribution of the molybdenum-copper deposit and molybdenum copperore occurrences in the regional. The research shows indicates that the metallogenic adamellite, adamellite and granite-porphyry have obvious geophysical field characteristics of high magnetic, high resistance and low polarization, and the molybdenum-copper mineralized and developed in the section with apparent polarizability(1.5%±)and apparent resistivity (1500—2000?·m)in low,which is anastomosis with the world typical porphyry Mo(Cu) ore deposit. Based on the studies mentioned above and combined with the deposit geological characteristics of the existed deposit and ore occurrences in the study area, we made comprehensive analysis and information extraction on geological, geophysical and geochemistry, then summarized the metallogenic regularity in the metallogenic belt,and delineated th
From existing research, we think that Tieli area has a good prospect in the explorion of Mo(Cu),W and Au, possiblely become an important mineral resource base for Mo(Cu), W, Au and nonferrous metals in the northeast China. From now on, We should made pay attention to the protection of the forest ecological environment, when we launching the mineral resources exploration and exploitation and promot the harmonious development between man and the nature and the human beings’sustainable development.
本文从成矿地质背景分析入手,深入研究矿床地质特征、地球化学特征、成矿地质条件及其控矿机制,准确厘定了成矿岩体的形成时代,确定了该地区MoCu矿床的成因,建立成矿模式;根据成矿地质条件与地质、地球物理、地球化学测量结果研究,确定找矿标志,指明该区的找矿方向,确定后续找矿工作的预测靶区,研究成果对本地区的开展类似研究工作与部属钼铜多金属矿产勘查工作有重要指导意义。
Tieli area is located in the central south of the Yichun-Yanshou magma–structure belt which geostructure position is situated in the Songnen–Zhangguangcailing block and the Jiamusi–Xingkai block collisional belt. Its special tectonic setting and related activities of the intermediate-acid magmatic rocks provided conditions for the formation of molybdenum, copper, lead-zinc, gold and high-grade iron deposit in the study area.
Luming in the area molybdenum-copper deposit is a super large deposit which was recent discovered and investigated in recent years, the aspects of ore body was in the adamellite and the granite-porphyry, which belongs to the type of porphyry ore deposit. Cuiling in the area molybdenum-copper deposit was small, and it has the similar characteristics to those of Luming molybdenum-copper deposit, which is also belongs to the type of porphyry ore deposit. Studies on the granitic magmatic rock (monzonite, granite-porphyry) have shown the results that its generally belongs to the aluminium-oversaturated, high potassium calc-alkaline series I type granite. Based on the characteristics of major element, REE, trace element, isotope and regional geology, we believe that these molybdenum-copper deposits have been formed in a pull apart environment of the later syn-collision tectonic period. According to the measure of the age, The dateing of the La-ICP-MS zircon U-Pb indicates that these rock mass have been formed in the age of 174.0~178.3 Ma, and that belonged to the early period of mesozoic Yanshan Movement.
The exposed granite-porphyry of the northeastern study area has obvious differences with the fine porphyritic monzonitic-orthoclase granites of the south, and the former is associated with acidic volcanic rock, but the later has controlled the element anomalies such as Mo, Cu, Ag, Bi, Pb, As, Zn, etc. And also controlled the distribution of the molybdenum-copper deposit and molybdenum copperore occurrences in the regional. The research shows indicates that the metallogenic adamellite, adamellite and granite-porphyry have obvious geophysical field characteristics of high magnetic, high resistance and low polarization, and the molybdenum-copper mineralized and developed in the section with apparent polarizability(1.5%±)and apparent resistivity (1500—2000?·m)in low,which is anastomosis with the world typical porphyry Mo(Cu) ore deposit. Based on the studies mentioned above and combined with the deposit geological characteristics of the existed deposit and ore occurrences in the study area, we made comprehensive analysis and information extraction on geological, geophysical and geochemistry, then summarized the metallogenic regularity in the metallogenic belt,and delineated th
From existing research, we think that Tieli area has a good prospect in the explorion of Mo(Cu),W and Au, possiblely become an important mineral resource base for Mo(Cu), W, Au and nonferrous metals in the northeast China. From now on, We should made pay attention to the protection of the forest ecological environment, when we launching the mineral resources exploration and exploitation and promot the harmonious development between man and the nature and the human beings’sustainable development.
引文
[1]张彦龙,葛文春,柳小明,张吉衡.大兴安岭新林镇岩体的同位素特征及其地质意义[J].吉林大学学报.2008,38(2):177-186
[2]范蔚茗,郭锋,高晓峰,李超文.东北地区中生代火成岩Sr-Nd同位素区划及其大地构造意义[J].地球化学.2008,37(4):361-372
[3]韩振哲,赵海玲,苏士杰,郎海涛,于荣文,尹志刚.小兴安岭东南金山屯一带晚三叠世二长花岗岩成因及其地质意义[J].现代地质.2008,22(2):197-206
[4]周金平,吴峰,贾木欣.伊春鹿鸣钼矿工艺矿物学研究[J].矿治. 2008,17(2):111-119
[5]韩振哲,张海,赵长青.黑龙江省铁力市翠岭铜钼多金属矿普查06-07年度普查阶段性报告[R].项目报告.2008
[6]张显.黑龙江省东部早中生代火成岩构造组合及其大地构造演化[D].中国地质大学博士学位论文.2008
[7]陈雪.黑龙江省鸡东金场沟铜钼矿控矿条件与成矿预测[D].吉林大学硕士学位论文.2008
[8]时永明,崔彬,贾维林.黑龙江省铁力市鹿鸣钼矿床地质特征[J].地质与勘探. 2007,43(2):20-22
[9]刘宝山,任凤和,李仰春,赵焕力.伊春地区晚印支期I型花岗岩带特征及其构造背景[J].地质与勘探.2007,43(1):74-78
[10]唐文龙,杨言辰,李骞,毛向军.伊春前进地区岩浆岩的地球化学特征及其对成矿的制约[J].吉林大学学报.2007,37(1):41-47
[11]吴福元,李献华,杨进辉,郑永飞.花岗岩成因研究的若干问题[J].岩石学报.2007,23(6):1217-1238
[12]葛文春,隋振民,吴福元等.大兴安岭东北部早古生代花岗岩锆石U-Pb年龄、Hf同位素特征及地质意义[J].岩石学报.2007,23(2):423-440
[13]隋振民,吴福元,葛文春等.大兴安岭东北部侏罗纪花岗质岩石的锆石U-Pb年龄、地球化学特征及成因[J].岩石学报.2007,23(2):461-480
[14]胡永达.青海东昆仑乌兰乌珠尔铜矿地质特征及成矿远景评价[D].吉林大学硕士学位论文.2007
[15]赵院冬.东宁地区早中生代花岗岩地球化学特征及大地构造背景[D].吉林大学硕士学位论文.2007
[16]谢海东.珲春柳树河子—马滴达金及多金属矿化集中区控矿地质条件及找矿靶区预测[D].吉林大学硕士学位论文.2007
[17]臧兴运.吉林省桦甸市板庙子金矿及外围控矿地质条件与靶区预测[D].吉林大学硕士学位论文.2007
[18]艾国栋.福建省龙岩市学堂坑钼矿地质特征及找矿预测研究[D].中南大学硕士学位论文.2007
[19]芮宗瑶,张洪涛,陈仁义,王志良,王龙生,王义天.斑岩铜矿研究中若干问题探讨[J].矿床地质.2006,25(4):491-500
[20] Zheng. you-ye. Ore-forming fluid controlling minerallzation in Qulong super-large porphyry copper deposit, Tibet [J].Diqiu Kexue–Zhongguo Dizhida Daxue Xuebao /Earth Science-jlurnal of China University of Geosciences .2006,31(3):349-354.
[21] Han. Chunming. Geological characteristics and genesis of the Tuwu porphyry copper deposit, Hami, Xinjiang , central Asia[J]. Ore Geology Reviews.v .2006,29(1) :77-94.
[22]程瑞玉,吴福元,葛文春,孙德有,柳小明,杨进辉.黑龙江省东部饶河杂岩的就位时代与东北东部中生代构造演化[J].岩石学报2006,22(2):353-376
[23]赵焕利,刘宝山,李仰春.岩石密度测量在黑龙江伊春地区花岗岩体就位机制研究中的应用[J].华南地质与矿产.2006,2:6-12
[24]杨言辰.鹿鸣-前进地区多金属矿床成矿规律与成矿预测[R].项目报告.2006
[25]程瑞玉.黑龙江省东部饶河地区花岗岩时代及其成因[D].吉林大学硕士学位论文.2006
[26]张海心.内蒙古乌奴格吐山铜钼矿床地质特征及成矿模式[D].吉林大学硕士学位文.2006
[27]葛文春,吴福元,周长勇,张吉衡.大兴安岭中部乌兰浩特地区中生代花岗岩的锆石U-Pb年龄及地质意义[J].岩石学报.2005,21(3):749-762
[28]刘宝山,马永强,吕军等.伊春地区上游新村晚三叠世二长花岗岩体成因及就位机制[J].地质与资源.2005,14(3):170-175
[29]孙德有,吴福元,高山.吉林中部晚三叠世和早侏罗世两期铝质A型花岗岩的厘定及对吉黑东部构造格局的制约[J].地学前缘.2005,12(2):263-275
[30]杨言辰.黑龙江小兴安岭-张广才岭成矿带金、多金属矿床成矿规律与成矿预测[R].项目报告.2005
[31]杨言辰,王可勇,冯本智.大横路式钴(铜)矿床地质特征及成因探讨[J].地质与勘探. 2004,40(1):7-11
[32]孙德有,吴福元,高山.小兴安岭东部清水岩体的锆石激光U-Pb年龄测定[J].地球学报2004,25(2):213-218
[33]林强,葛文春,吴福元,孙德有,曹林.大兴安岭中生代花岗岩类的地球化学[J].岩石学报.2004,20(3):403-412
[34]侯增谦.斑岩Cu-Mo-Au矿床[J]:新认识与新进展. 2004,11(1):131-144
[35]韩振新,徐衍强,郑庆道.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
[35] Dengjun,Liuwei, S unzhongshi,et al.Evidence of mantle-rooted fluid and multi-level circulation ore-formingdynamics:A case study from the Xiadian gold deposit,Shangdong province,China. [J].Science in China(series D): 2003,46:123-134.
[37] Dengjun,Sunzhongshi,Wangqingfei,et al. Crust mantle structure and gold enrichment mechanismof mantle fluid system[J].Chinese journal of geochemistry, 2003,22(3):263-270.
[38]潘贵,刘宝山,李仰春.伊春地区晚奥陶世花岗质岩石中闪长质包体的成因[J].中国地质.2002,29(4):364-368
[39] Dengjun,Wangqingfei,Sunzhongshi. Origin of gold bearing fluid and its initiative localization mechanism in Xiadian gold deposit,Shandong province[J].Chinese Journal of geochemistry. 2002,21(3):282-288.
[40]涂绍雄,汪雄武.20世纪90年代国外花岗岩类研究的某些重大进展[J].岩石矿物学杂志. 2002,21(2):107-118
[41]陈文明.论斑岩铜矿的成因[J].现代地质. 2002,16(1):1-8
[42]杨言辰,马志红,杨宝俊.中国北方古元古代成矿带矿床成矿系列研究[M].吉林人民出版社.2002
[43]刘宗秀.金厂沟梁金矿床地质地球化学特征及东矿区金矿的预测[D].吉林大学硕士学位论文.2002
[44]郭峰,范蔚茗等.大兴安岭南段晚中生带双峰式火山作用[J].岩石学报. 2001,17(1):161-168
[45]孙德有.张广才岭中生代花岗岩成因及其地球动力学意义[D].吉林大学博士学位论文.2001
[46]王京彬,王玉往,王莉娟.大兴安岭中南段铜矿成矿背景及找矿潜力[J].地质与勘探. 2000,36(5):1-4
[47]赵明玉.张广才岭成矿带铁力-玉泉有色金属、贵金属矿带成矿特征分析[J].矿产与地质. 2000,14(78):225-229
[48]李朝阳等著.中国铜矿主要类型特征及其成矿远景[ M].地质出版社.2000
[49]孙加鹏,张兴洲,杨宝俊.张广才岭岩石圈结构及盆岭构造[J].长春科技大学学报.1999,29(1):25-28
[50]吴福元,曹林.东北亚地区的若干重要基础地质问题[J].世界地质.1999,18(2):1-13
[51]吴福元,孙德有,林强.东北地区显生宙花岗岩的成因与地壳增生[J].岩石学报.1999,15(2):181-189
[52]姜宝龙,吴延之.黑龙江省小西林铅锌矿床同生沉积成扩特征与找扩方向[J].有色金属矿产与勘查.1999,8(23):107-108.
[53]侯敏,杜恒芳.小兴安岭南段-张广才岭成矿带主要金属矿床成矿系列的划分及区域成矿规律[J].黑龙江地质.1998,9(3):10-16
[54]吴福元,江博明,林强.中国北方造山带造山后花岗岩的同位素特点与地壳生长意义[J].科学通报.1997,42(20):2188-2192
[55]尹冰川,冉清昌.小兴安岭—张广才岭地区区域成矿演化矿床地质[J].1997,16(3):237-242
[56]韩振新,赫正平等.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
[57]韩振新,郝政平,侯敏.小兴安岭地区与加里东期花岗岩类有关的矿床成矿系列[J].矿床地质.1995,14(4):293-302
[58]黑龙江省地质矿产局.黑龙江省区域地质志[M ].地质出版社.1993
[59]邱家骧,林景仟.岩石化学[M].北京:地质出版社.1991
[60]王中刚,于学元,赵振华等.稀土元素地球化学[M].北京:科学出版社.1989,223-224
[61] Li. Peilan. Yu. Xingzhen. Experimental Study Of The Principle Of Geochemical Potential Conservation Based On The Mineralization Of Duobaoshan Porphyry Copper Deposit[J]. Zhongnan Kuangye Xueyuan Xuebao/Journal of Central-South Institute of Mining and Metallurgy. 1987,18(4):384-384
[62]冶金工业部地质研究所.中国斑岩铜矿[ M].科学出版社.1984
[63]邱家骧.岩浆岩岩石学[ M].北京:地质出版社.1983
[64]南京大学地质系矿物岩石教研室.火成岩岩石学[ M].北京:地质出版社.1979
[65]路远发.Geokit软件.长江大学地球化学系.2008
[66]唐文龙.黑龙江省前进地区岩浆岩地球化学特征与成矿预测[D].吉林大学硕士学位论文. 2007
[67]刘红霞.黑龙江省伊春-延寿成矿带成矿系统分析与成矿预测[D].吉林大学硕士学位论文.2007
[68]吴小军.黑龙江省前进东山铅锌矿床地质特征及成因[D].吉林大学硕士学位论文.2008
[2]范蔚茗,郭锋,高晓峰,李超文.东北地区中生代火成岩Sr-Nd同位素区划及其大地构造意义[J].地球化学.2008,37(4):361-372
[3]韩振哲,赵海玲,苏士杰,郎海涛,于荣文,尹志刚.小兴安岭东南金山屯一带晚三叠世二长花岗岩成因及其地质意义[J].现代地质.2008,22(2):197-206
[4]周金平,吴峰,贾木欣.伊春鹿鸣钼矿工艺矿物学研究[J].矿治. 2008,17(2):111-119
[5]韩振哲,张海,赵长青.黑龙江省铁力市翠岭铜钼多金属矿普查06-07年度普查阶段性报告[R].项目报告.2008
[6]张显.黑龙江省东部早中生代火成岩构造组合及其大地构造演化[D].中国地质大学博士学位论文.2008
[7]陈雪.黑龙江省鸡东金场沟铜钼矿控矿条件与成矿预测[D].吉林大学硕士学位论文.2008
[8]时永明,崔彬,贾维林.黑龙江省铁力市鹿鸣钼矿床地质特征[J].地质与勘探. 2007,43(2):20-22
[9]刘宝山,任凤和,李仰春,赵焕力.伊春地区晚印支期I型花岗岩带特征及其构造背景[J].地质与勘探.2007,43(1):74-78
[10]唐文龙,杨言辰,李骞,毛向军.伊春前进地区岩浆岩的地球化学特征及其对成矿的制约[J].吉林大学学报.2007,37(1):41-47
[11]吴福元,李献华,杨进辉,郑永飞.花岗岩成因研究的若干问题[J].岩石学报.2007,23(6):1217-1238
[12]葛文春,隋振民,吴福元等.大兴安岭东北部早古生代花岗岩锆石U-Pb年龄、Hf同位素特征及地质意义[J].岩石学报.2007,23(2):423-440
[13]隋振民,吴福元,葛文春等.大兴安岭东北部侏罗纪花岗质岩石的锆石U-Pb年龄、地球化学特征及成因[J].岩石学报.2007,23(2):461-480
[14]胡永达.青海东昆仑乌兰乌珠尔铜矿地质特征及成矿远景评价[D].吉林大学硕士学位论文.2007
[15]赵院冬.东宁地区早中生代花岗岩地球化学特征及大地构造背景[D].吉林大学硕士学位论文.2007
[16]谢海东.珲春柳树河子—马滴达金及多金属矿化集中区控矿地质条件及找矿靶区预测[D].吉林大学硕士学位论文.2007
[17]臧兴运.吉林省桦甸市板庙子金矿及外围控矿地质条件与靶区预测[D].吉林大学硕士学位论文.2007
[18]艾国栋.福建省龙岩市学堂坑钼矿地质特征及找矿预测研究[D].中南大学硕士学位论文.2007
[19]芮宗瑶,张洪涛,陈仁义,王志良,王龙生,王义天.斑岩铜矿研究中若干问题探讨[J].矿床地质.2006,25(4):491-500
[20] Zheng. you-ye. Ore-forming fluid controlling minerallzation in Qulong super-large porphyry copper deposit, Tibet [J].Diqiu Kexue–Zhongguo Dizhida Daxue Xuebao /Earth Science-jlurnal of China University of Geosciences .2006,31(3):349-354.
[21] Han. Chunming. Geological characteristics and genesis of the Tuwu porphyry copper deposit, Hami, Xinjiang , central Asia[J]. Ore Geology Reviews.v .2006,29(1) :77-94.
[22]程瑞玉,吴福元,葛文春,孙德有,柳小明,杨进辉.黑龙江省东部饶河杂岩的就位时代与东北东部中生代构造演化[J].岩石学报2006,22(2):353-376
[23]赵焕利,刘宝山,李仰春.岩石密度测量在黑龙江伊春地区花岗岩体就位机制研究中的应用[J].华南地质与矿产.2006,2:6-12
[24]杨言辰.鹿鸣-前进地区多金属矿床成矿规律与成矿预测[R].项目报告.2006
[25]程瑞玉.黑龙江省东部饶河地区花岗岩时代及其成因[D].吉林大学硕士学位论文.2006
[26]张海心.内蒙古乌奴格吐山铜钼矿床地质特征及成矿模式[D].吉林大学硕士学位文.2006
[27]葛文春,吴福元,周长勇,张吉衡.大兴安岭中部乌兰浩特地区中生代花岗岩的锆石U-Pb年龄及地质意义[J].岩石学报.2005,21(3):749-762
[28]刘宝山,马永强,吕军等.伊春地区上游新村晚三叠世二长花岗岩体成因及就位机制[J].地质与资源.2005,14(3):170-175
[29]孙德有,吴福元,高山.吉林中部晚三叠世和早侏罗世两期铝质A型花岗岩的厘定及对吉黑东部构造格局的制约[J].地学前缘.2005,12(2):263-275
[30]杨言辰.黑龙江小兴安岭-张广才岭成矿带金、多金属矿床成矿规律与成矿预测[R].项目报告.2005
[31]杨言辰,王可勇,冯本智.大横路式钴(铜)矿床地质特征及成因探讨[J].地质与勘探. 2004,40(1):7-11
[32]孙德有,吴福元,高山.小兴安岭东部清水岩体的锆石激光U-Pb年龄测定[J].地球学报2004,25(2):213-218
[33]林强,葛文春,吴福元,孙德有,曹林.大兴安岭中生代花岗岩类的地球化学[J].岩石学报.2004,20(3):403-412
[34]侯增谦.斑岩Cu-Mo-Au矿床[J]:新认识与新进展. 2004,11(1):131-144
[35]韩振新,徐衍强,郑庆道.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
[35] Dengjun,Liuwei, S unzhongshi,et al.Evidence of mantle-rooted fluid and multi-level circulation ore-formingdynamics:A case study from the Xiadian gold deposit,Shangdong province,China. [J].Science in China(series D): 2003,46:123-134.
[37] Dengjun,Sunzhongshi,Wangqingfei,et al. Crust mantle structure and gold enrichment mechanismof mantle fluid system[J].Chinese journal of geochemistry, 2003,22(3):263-270.
[38]潘贵,刘宝山,李仰春.伊春地区晚奥陶世花岗质岩石中闪长质包体的成因[J].中国地质.2002,29(4):364-368
[39] Dengjun,Wangqingfei,Sunzhongshi. Origin of gold bearing fluid and its initiative localization mechanism in Xiadian gold deposit,Shandong province[J].Chinese Journal of geochemistry. 2002,21(3):282-288.
[40]涂绍雄,汪雄武.20世纪90年代国外花岗岩类研究的某些重大进展[J].岩石矿物学杂志. 2002,21(2):107-118
[41]陈文明.论斑岩铜矿的成因[J].现代地质. 2002,16(1):1-8
[42]杨言辰,马志红,杨宝俊.中国北方古元古代成矿带矿床成矿系列研究[M].吉林人民出版社.2002
[43]刘宗秀.金厂沟梁金矿床地质地球化学特征及东矿区金矿的预测[D].吉林大学硕士学位论文.2002
[44]郭峰,范蔚茗等.大兴安岭南段晚中生带双峰式火山作用[J].岩石学报. 2001,17(1):161-168
[45]孙德有.张广才岭中生代花岗岩成因及其地球动力学意义[D].吉林大学博士学位论文.2001
[46]王京彬,王玉往,王莉娟.大兴安岭中南段铜矿成矿背景及找矿潜力[J].地质与勘探. 2000,36(5):1-4
[47]赵明玉.张广才岭成矿带铁力-玉泉有色金属、贵金属矿带成矿特征分析[J].矿产与地质. 2000,14(78):225-229
[48]李朝阳等著.中国铜矿主要类型特征及其成矿远景[ M].地质出版社.2000
[49]孙加鹏,张兴洲,杨宝俊.张广才岭岩石圈结构及盆岭构造[J].长春科技大学学报.1999,29(1):25-28
[50]吴福元,曹林.东北亚地区的若干重要基础地质问题[J].世界地质.1999,18(2):1-13
[51]吴福元,孙德有,林强.东北地区显生宙花岗岩的成因与地壳增生[J].岩石学报.1999,15(2):181-189
[52]姜宝龙,吴延之.黑龙江省小西林铅锌矿床同生沉积成扩特征与找扩方向[J].有色金属矿产与勘查.1999,8(23):107-108.
[53]侯敏,杜恒芳.小兴安岭南段-张广才岭成矿带主要金属矿床成矿系列的划分及区域成矿规律[J].黑龙江地质.1998,9(3):10-16
[54]吴福元,江博明,林强.中国北方造山带造山后花岗岩的同位素特点与地壳生长意义[J].科学通报.1997,42(20):2188-2192
[55]尹冰川,冉清昌.小兴安岭—张广才岭地区区域成矿演化矿床地质[J].1997,16(3):237-242
[56]韩振新,赫正平等.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
[57]韩振新,郝政平,侯敏.小兴安岭地区与加里东期花岗岩类有关的矿床成矿系列[J].矿床地质.1995,14(4):293-302
[58]黑龙江省地质矿产局.黑龙江省区域地质志[M ].地质出版社.1993
[59]邱家骧,林景仟.岩石化学[M].北京:地质出版社.1991
[60]王中刚,于学元,赵振华等.稀土元素地球化学[M].北京:科学出版社.1989,223-224
[61] Li. Peilan. Yu. Xingzhen. Experimental Study Of The Principle Of Geochemical Potential Conservation Based On The Mineralization Of Duobaoshan Porphyry Copper Deposit[J]. Zhongnan Kuangye Xueyuan Xuebao/Journal of Central-South Institute of Mining and Metallurgy. 1987,18(4):384-384
[62]冶金工业部地质研究所.中国斑岩铜矿[ M].科学出版社.1984
[63]邱家骧.岩浆岩岩石学[ M].北京:地质出版社.1983
[64]南京大学地质系矿物岩石教研室.火成岩岩石学[ M].北京:地质出版社.1979
[65]路远发.Geokit软件.长江大学地球化学系.2008
[66]唐文龙.黑龙江省前进地区岩浆岩地球化学特征与成矿预测[D].吉林大学硕士学位论文. 2007
[67]刘红霞.黑龙江省伊春-延寿成矿带成矿系统分析与成矿预测[D].吉林大学硕士学位论文.2007
[68]吴小军.黑龙江省前进东山铅锌矿床地质特征及成因[D].吉林大学硕士学位论文.2008