内蒙古赤峰南部地区金矿综合信息矿产预测
|
摘要
研究区位于内蒙古自治区赤峰市的南部,在地质上位于华北地台北缘中东段,北邻天山-兴蒙地槽系。研究区内地质情况复杂,成矿条件极为优越,是贵金属、多金属矿产的成矿有利地段。
本文在充分搜集了区域以往地质、物探、化探、矿产勘查等资料的基础上,对研究区内的金矿成矿地质背景、地球物理条件、地球化学条件进行了全面、系统、完整的分析,获取了大量的有用信息。通过典型矿床研究,建立起与研究区地质环境相应的金矿成矿模式,以典型矿床为目标研究了各种信息的关联关系,进而建立起该区的综合信息找矿模型。以成矿规律、成矿控制和找矿模型为指导,在区内过行了统计地质单元的划分,划分出44个统计单元;在找矿模型定量转换的基础上,选用了多种预测方法构建了金矿资源的定位、定量评价模型,并进行了科学预测。通过预测结果的解释,在研究内确定了一级找矿远景区3个,二级找矿远景区5个,分布在3个成矿带中,预测全区金矿资源潜力153吨。编制赤南地区的金矿资源分布图,并对一、二级找矿远景区提出工作布署建议。研究成果对赤峰南部地区今后找矿勘探工作具有重要的参考价值。
Northern margin of north china platform is an important metallogenic belt for non-ferrous metals and precious metals, and one of 16 key minerogenic belts for solid mineral resource in China. South of Chifeng is the important component in this mineralization belt.This area occupies the connection spot of northern margin of north china platform with the Mongolian geosyncline orogenic zone.Geological structure in the area is complex,the activity of magmatic is frequent,the deterioration distortion function is obvious.The mining history is glorious,the geological condition of mineralizing is superior,where is the advantageous sector for precious metal,and polymetallic minerals. besides, the gold ore is the superiority ore to plant.
This article taking the modern metallogenic theory as the instruction, conducts the research for the first time in the area using the synthesis information minerals prediction technique. We will use the synthesis information minerals prediction technique to analyze the regional geology, the geophysical prospecting, the geochemical exploration and the minerals investigation material, thus will get some new knowledge form the excavation and the connection from the information. the next step will Conduct the research and the appraisal to the region minerals resource,finally,for the units selected, we will make geological interpretation and put forward the proposal to deployment the prospecting work.
1、Fundamental geology
This area has the glorious gold mining history, in addition to,new metallogenic theory and new method has been used widely in recent years.which has led the mineralization analysis more and more detailed.There are many kinds of mineralization concepts in a long period,which has made tremendous contribution to the metallogenic theory's consummation.But the fundamental of mineralization has not changed obviously.The first source bed unification understanding was the Pre-Cambrian Period antique generation of deterioration rock mass,The second source bed was the Paleozoic Era later period to the Mesozoic Era early time original rock restoration activation magmatic rock;the metallogenic model can been unified for the original rock restoration and the superimposition concentrates function.In view of the minerals forecast,the metallogenic model will be called as compound endogenous model.
The tectonic framework in south of Chifeng area are mainly controlled by the Chifeng-Kaiyuan breaks and the Nenjiang-Qinglonghe breaks these two first-level structure.These two first-level structures are the basic tectonic element in the area.These structures is controlling the distribution of second-level structure and the fluctuation of fault block in the area,and which is in charge of the Heilihe-Yebaishou breaks,the Xiaoniuqun-Jiefangyingzi break and the Jinshan-Chifeng break and so on,these secondary breaks were controlling the Paleozoic Era to the Mesozoic Era intrusive rockthe alteration beltthe deterioration distortion belt's spatial distribution and the spreed form in the area.Gold deposits in the area is mainly affected by the spatial distribution of cross-cutting between NE and EW faults,thus the EW faults and NE faults and the intersection location is the most potential ore-forming tectonic environment.
2、Geochemical conclusions
Studies 39 kinds of elements in the region,pick up 14 kinds of elements related with the gold mineralization after the geochemistry research.Studies 14 kinds of element statistical parameter characteristic,which pointed out that the region elements are deficients primarily,but the discreteness of these elements is big enough,which noted that the regional metallogenic Events is dramatic,so the enrichment of ore-forming element makes it possible for mineralization.The multivariate statistical analysis shows that the area with the characteristics of multiple phases of superimposed mineralization.Based on the analysis for geochemical field,the study area will be divided into three types of geochemical field,the geochemical element of I-type are related with mineralization.Other two kinds are element related with mineralization and tracer element.The combination anomaly are divided into three types,the combination anomaly of Au-As;the combination anomaly of Au-Ag and the simple combination anomaly,The research for the combination of abnormal suggest that those area where the content of Au is high in background and the discreteness is strong are favorable position for mineralization.Au-As type combination anomaly and Au-Ag type combination anomalies has certain relationship with gold deposits.
3、Geophysical conclusions
In this paper,we collect the regional physical information, based on the comparative analysis of those data set up the basic understanding for regional geophysical interpretation,which pointed out that there are big difference in regional rock (ore) on the physical properties,magnetic characteristics.Take the natural material as the foundation,carries on the analysis and infer the conditions related with the gold mineralization, such as tectonics,stratigraphyintrusive rocks.We make the interpretation to the regional tectonic using synthesis information interpretation principle and the method.The result shows that EW faults,NW faults and NE faults is extremely widespread,particular emphasis is the development situation of EW structures and the NW structures is relatively weak,which assumes off and on be in charge of the NE structure,these reflect the characteristics of multi-phase transformation,all the works consummate the system of regional tectonic.Through the analysis of the aeromagnetic field which reduced to the pole,the aeromagnetic field will be divided into 8 magnetic body,which we had make the geological explaination carefully.
4、Research on typical deposit
In this section,we summarized the ore-forming background,geological features,metallogeny and ore-forming characteristics about Mesozoic hydrothermal gold deposits and sub-volcanic rock-type gold deposit in south of Chifeng.The conclusion indicates that gold ore-controlling condition was mainly the Archean Metamorphic rockstectonic fracture systems and Yanshanian-hercynian intrusive rocks system.the analysis indicates that the uplift zone with distribution of Archean stratigraphic and volcanic activity Mesozoic basin and the edge of its interaction spot are the best parts for mineralization. Fracture NW direction and the intersection with the NE fracture and its associated secondary-fault zone are the best mineralization spots.The intersection spot of EW faults with the NW or SN faults and its vicinity with deep fault and shallow fault is the best parts for mineralization.The intermediate-acid intrusive rock in Mesozoic or Paleozoic period are favorable factors for mineralization.some ultra hypabyssal rock region where the intermediate-acid vein rocks is the main body,especially these ultra-hypabyssal porphyry vein with higher Au-Ag-Cu-Pb-Zn contents at Yanshanian to be more advantageous to the mineralization.At the same time,some region with wall-rock alteration,surface of the "burning skin" and the "face sesame",are the important spots for mineralization.
This paper take the typical deposit research as the foundation,refer to the the system of tectonic evolution,has established a compound endogenous-type gold mineralization model which related with Archean metamorphic in south of Chifeng,the author has mapped the regional metallogenic model finally.
5、Mineral prediction results
Based on the research about metallogenic regularity and metallogenic model in south of Chifeng, a comprehensive prospecting model.is established Altogether selects statistical unit 44,in which the statistics unit with accurate reserves data is 13,unknown statistical unit is 31.
While it carries on the regional prospecting work, established a set of method systematically according to the characteristic about mid-small scale synthesis information prospecting:the unit mineralization probability→the unit scale→the unit amount of resources→an entire area amount of resources.
①Location prediction
Carries on the resources localization forecast according to the synthesis information mineralization prediction theory in the research area,the choice method include the characteristic analysis,the Q cluster analysis,the correspondence analysis and the quantification theory IV.Using these methods calculats the probability of mineralization separately,the statistical units will be divided into 4 level after analysed synthetically.In considered fully the structural environment and the unit distribution which has gold deposits or the probability of mineralization above B level,south of Chifeng is divided into three metallogenic belt.Three metallogenic belts respectively are Xiaoniuqun-Jiefangyingzi,Jinshan-Malan and Heilihe-Tianyi mineralization belt.
②Quantitative prediction
In this section the author establish the forecast model for south of Chifeng using the logic information law,test the model with the verification units,get the confirmation rate of accuracy is 71%,it indicates that this method can be used for prediction on the unknown units,finally calculate the amount of resources 69.25 tons using the method.In the next section the author use the collection of ore unit with reserves to set up the multivariate linear regression equation,then test the regressioin equation with the significance test,finally forecast the amount of resource 153 tons.In the third section the author,set up regional resource prediction probability model: resource extent=number of deposits×ore reserves×ore grade with the Monte-Carlo law,then collect the ore reserves-grade data in Chifeng and its peripheral region,in final,calculat the amount of resources 215 tons with random sampling method.Through many kinds of methods and take care of adaption,we point out the resources of south of Chifeng is 153 tons.It noted that the area has potential for mineralization,there will continue to be an important areas for prospecting.
In the overall evaluation localization forecast and under the quantitative forecasting result's premise,we take into account the conditions of ore-forming unit,choose 3 first-level prospecting area and 5 second-level prospecting area from 13 B-level unit,this work will provide some clues to geological exploration afterwards.
本文在充分搜集了区域以往地质、物探、化探、矿产勘查等资料的基础上,对研究区内的金矿成矿地质背景、地球物理条件、地球化学条件进行了全面、系统、完整的分析,获取了大量的有用信息。通过典型矿床研究,建立起与研究区地质环境相应的金矿成矿模式,以典型矿床为目标研究了各种信息的关联关系,进而建立起该区的综合信息找矿模型。以成矿规律、成矿控制和找矿模型为指导,在区内过行了统计地质单元的划分,划分出44个统计单元;在找矿模型定量转换的基础上,选用了多种预测方法构建了金矿资源的定位、定量评价模型,并进行了科学预测。通过预测结果的解释,在研究内确定了一级找矿远景区3个,二级找矿远景区5个,分布在3个成矿带中,预测全区金矿资源潜力153吨。编制赤南地区的金矿资源分布图,并对一、二级找矿远景区提出工作布署建议。研究成果对赤峰南部地区今后找矿勘探工作具有重要的参考价值。
Northern margin of north china platform is an important metallogenic belt for non-ferrous metals and precious metals, and one of 16 key minerogenic belts for solid mineral resource in China. South of Chifeng is the important component in this mineralization belt.This area occupies the connection spot of northern margin of north china platform with the Mongolian geosyncline orogenic zone.Geological structure in the area is complex,the activity of magmatic is frequent,the deterioration distortion function is obvious.The mining history is glorious,the geological condition of mineralizing is superior,where is the advantageous sector for precious metal,and polymetallic minerals. besides, the gold ore is the superiority ore to plant.
This article taking the modern metallogenic theory as the instruction, conducts the research for the first time in the area using the synthesis information minerals prediction technique. We will use the synthesis information minerals prediction technique to analyze the regional geology, the geophysical prospecting, the geochemical exploration and the minerals investigation material, thus will get some new knowledge form the excavation and the connection from the information. the next step will Conduct the research and the appraisal to the region minerals resource,finally,for the units selected, we will make geological interpretation and put forward the proposal to deployment the prospecting work.
1、Fundamental geology
This area has the glorious gold mining history, in addition to,new metallogenic theory and new method has been used widely in recent years.which has led the mineralization analysis more and more detailed.There are many kinds of mineralization concepts in a long period,which has made tremendous contribution to the metallogenic theory's consummation.But the fundamental of mineralization has not changed obviously.The first source bed unification understanding was the Pre-Cambrian Period antique generation of deterioration rock mass,The second source bed was the Paleozoic Era later period to the Mesozoic Era early time original rock restoration activation magmatic rock;the metallogenic model can been unified for the original rock restoration and the superimposition concentrates function.In view of the minerals forecast,the metallogenic model will be called as compound endogenous model.
The tectonic framework in south of Chifeng area are mainly controlled by the Chifeng-Kaiyuan breaks and the Nenjiang-Qinglonghe breaks these two first-level structure.These two first-level structures are the basic tectonic element in the area.These structures is controlling the distribution of second-level structure and the fluctuation of fault block in the area,and which is in charge of the Heilihe-Yebaishou breaks,the Xiaoniuqun-Jiefangyingzi break and the Jinshan-Chifeng break and so on,these secondary breaks were controlling the Paleozoic Era to the Mesozoic Era intrusive rockthe alteration beltthe deterioration distortion belt's spatial distribution and the spreed form in the area.Gold deposits in the area is mainly affected by the spatial distribution of cross-cutting between NE and EW faults,thus the EW faults and NE faults and the intersection location is the most potential ore-forming tectonic environment.
2、Geochemical conclusions
Studies 39 kinds of elements in the region,pick up 14 kinds of elements related with the gold mineralization after the geochemistry research.Studies 14 kinds of element statistical parameter characteristic,which pointed out that the region elements are deficients primarily,but the discreteness of these elements is big enough,which noted that the regional metallogenic Events is dramatic,so the enrichment of ore-forming element makes it possible for mineralization.The multivariate statistical analysis shows that the area with the characteristics of multiple phases of superimposed mineralization.Based on the analysis for geochemical field,the study area will be divided into three types of geochemical field,the geochemical element of I-type are related with mineralization.Other two kinds are element related with mineralization and tracer element.The combination anomaly are divided into three types,the combination anomaly of Au-As;the combination anomaly of Au-Ag and the simple combination anomaly,The research for the combination of abnormal suggest that those area where the content of Au is high in background and the discreteness is strong are favorable position for mineralization.Au-As type combination anomaly and Au-Ag type combination anomalies has certain relationship with gold deposits.
3、Geophysical conclusions
In this paper,we collect the regional physical information, based on the comparative analysis of those data set up the basic understanding for regional geophysical interpretation,which pointed out that there are big difference in regional rock (ore) on the physical properties,magnetic characteristics.Take the natural material as the foundation,carries on the analysis and infer the conditions related with the gold mineralization, such as tectonics,stratigraphyintrusive rocks.We make the interpretation to the regional tectonic using synthesis information interpretation principle and the method.The result shows that EW faults,NW faults and NE faults is extremely widespread,particular emphasis is the development situation of EW structures and the NW structures is relatively weak,which assumes off and on be in charge of the NE structure,these reflect the characteristics of multi-phase transformation,all the works consummate the system of regional tectonic.Through the analysis of the aeromagnetic field which reduced to the pole,the aeromagnetic field will be divided into 8 magnetic body,which we had make the geological explaination carefully.
4、Research on typical deposit
In this section,we summarized the ore-forming background,geological features,metallogeny and ore-forming characteristics about Mesozoic hydrothermal gold deposits and sub-volcanic rock-type gold deposit in south of Chifeng.The conclusion indicates that gold ore-controlling condition was mainly the Archean Metamorphic rockstectonic fracture systems and Yanshanian-hercynian intrusive rocks system.the analysis indicates that the uplift zone with distribution of Archean stratigraphic and volcanic activity Mesozoic basin and the edge of its interaction spot are the best parts for mineralization. Fracture NW direction and the intersection with the NE fracture and its associated secondary-fault zone are the best mineralization spots.The intersection spot of EW faults with the NW or SN faults and its vicinity with deep fault and shallow fault is the best parts for mineralization.The intermediate-acid intrusive rock in Mesozoic or Paleozoic period are favorable factors for mineralization.some ultra hypabyssal rock region where the intermediate-acid vein rocks is the main body,especially these ultra-hypabyssal porphyry vein with higher Au-Ag-Cu-Pb-Zn contents at Yanshanian to be more advantageous to the mineralization.At the same time,some region with wall-rock alteration,surface of the "burning skin" and the "face sesame",are the important spots for mineralization.
This paper take the typical deposit research as the foundation,refer to the the system of tectonic evolution,has established a compound endogenous-type gold mineralization model which related with Archean metamorphic in south of Chifeng,the author has mapped the regional metallogenic model finally.
5、Mineral prediction results
Based on the research about metallogenic regularity and metallogenic model in south of Chifeng, a comprehensive prospecting model.is established Altogether selects statistical unit 44,in which the statistics unit with accurate reserves data is 13,unknown statistical unit is 31.
While it carries on the regional prospecting work, established a set of method systematically according to the characteristic about mid-small scale synthesis information prospecting:the unit mineralization probability→the unit scale→the unit amount of resources→an entire area amount of resources.
①Location prediction
Carries on the resources localization forecast according to the synthesis information mineralization prediction theory in the research area,the choice method include the characteristic analysis,the Q cluster analysis,the correspondence analysis and the quantification theory IV.Using these methods calculats the probability of mineralization separately,the statistical units will be divided into 4 level after analysed synthetically.In considered fully the structural environment and the unit distribution which has gold deposits or the probability of mineralization above B level,south of Chifeng is divided into three metallogenic belt.Three metallogenic belts respectively are Xiaoniuqun-Jiefangyingzi,Jinshan-Malan and Heilihe-Tianyi mineralization belt.
②Quantitative prediction
In this section the author establish the forecast model for south of Chifeng using the logic information law,test the model with the verification units,get the confirmation rate of accuracy is 71%,it indicates that this method can be used for prediction on the unknown units,finally calculate the amount of resources 69.25 tons using the method.In the next section the author use the collection of ore unit with reserves to set up the multivariate linear regression equation,then test the regressioin equation with the significance test,finally forecast the amount of resource 153 tons.In the third section the author,set up regional resource prediction probability model: resource extent=number of deposits×ore reserves×ore grade with the Monte-Carlo law,then collect the ore reserves-grade data in Chifeng and its peripheral region,in final,calculat the amount of resources 215 tons with random sampling method.Through many kinds of methods and take care of adaption,we point out the resources of south of Chifeng is 153 tons.It noted that the area has potential for mineralization,there will continue to be an important areas for prospecting.
In the overall evaluation localization forecast and under the quantitative forecasting result's premise,we take into account the conditions of ore-forming unit,choose 3 first-level prospecting area and 5 second-level prospecting area from 13 B-level unit,this work will provide some clues to geological exploration afterwards.
引文
[1]尤瑟.未来15年我国矿产资源供需缺口将扩大[N].产经网-中国矿业报.2007-5-23.
[2]王世称,范继璋,杨永华.矿产资源评价[M].长春:吉林科学技术出版社,1990:21-28.
[3]王世称,成秋明,范继璋.金矿资源综合信息评价方法[M].长春:吉林科学技术出版社,1990:1-21.
[4]王世称,王於天.综合信息解译原理与矿产预测图编制方法[M].长春:吉林大学出版社,1989:3-18.
[5] De Verle Harris著,文世澂译.矿产资源评价—过去、现在的看法和对未来趋势的展望[C].矿产资源评价和矿业经济分析方法与实践.1997:9-19.
[6] Lesley Wyborn,etc.Using GIS for mineral potential evaluation in areas with few known mineral occurrences[J]. Second National forum on GIS in the Geosciences.1995:29-31.
[7]胡惠民等.大比例尺成矿预测方法[M].北京:地质出版社.1995:4-7.
[8] Agterberg F.P.Combining indicator patterns in weights of evidence for resource evaluation[J].Nonrenewable Resources.1992:1.
[9] Agterberg F.P,Bonham Carter G.F.Statistical pattern integration for mineral exploration,in G.Gaal and D.F.Merriam(eds.)-Computer Applications for Mineral Exploration in Resource Exploration[M].Oxford :Pergamon Press.1990
[10] Brinck,J.W.Critical parameters for the production,depletion and substitution of mineral resources-a horizon beyond the limits to growth.Ceol.en Mijnb.1976, V55(3–4):185-194.
[11] Donald A Singer著,张莓译,未发现矿产资源三阶段定量评价的基本原理[C].矿产资源评价与矿业经济分析方法与实践.1997:12-22.
[12]程裕淇,陈毓川等.再论矿床的成矿系列问题-兼论中生代某些矿床的成矿系列[J].地质论评.1983,V29(2):127-141.
[13]陈毓川,裴荣富,宋天锐.中国矿床成矿系列初论[M].北京:地质出版社.1998.
[14]孙启祯.论边缘成矿-关于金属矿床的时空分布及其成因联系[J].地质与勘探.1986(1):7-14.
[15]孙启祯.边缘成矿与成矿边缘效应[J].地学前缘.1994,V1(3-4):176-183.
[16]翟裕生,彭润民,邓军,王建平,区域成矿学与找矿新思路[J],现代地质,2001(2):151-156.
[17]涂光炽.超大型矿床的找矿和理论研究[J].矿产与地质.1989(1):1-3.
[18]曾庆丰.我国矿田构造(内生金属矿床)研究现状与展望[J],地质与勘探,1979,4:48-55.
[19]季克俭,王立本.热源研究的重要进展和"三源"交代热液成矿学说[J].地学前缘.1994,1(3-4):126-132.
[20]裴荣富.金属成矿省等级体制成矿[J].矿床地质.2004,5(28):131-141.
[21]裴荣富,梅燕雄.矿产勘查的双控论与合理域模型[J].矿床地质.2001,20(4):307-312.
[22]谢学锦,刘大文.地球化学块体-概念与方法学的发展[J].中国地质.2002,29(3):225-233.
[23]赵鹏大,胡旺亮.地质异常理论与矿产预测[J].新疆地质.1992,10(2):93-100.
[24]赵鹏大,池顺都.初论地质异常[J].地球科学.1991,16(3):241-248.
[25]赵鹏大,孟宪国.地质异常与矿产预测[J].地球科学.1993,18(1):39-47.
[26]王世称,陈永良,夏立显.综合信息矿产预测理论与方法[M].北京:科学出版社.2000:183-203
[27]王世称,杨毅恒,李景朝.综合信息矿产资源预测中的定性数据分析方法[M].长春:吉林大学出版社.
[28]肖克炎.应用综合信息法研究成矿规律及成矿预测的新进展[J].地球科学进展.1994,9(2):18-23.
[29]叶天竺.固体矿产预测评价方法技术[M].北京:中国大地出版社.2004:128-163.
[30]黄汲清.中国大地构造及其演化[M].科学出版社.1980:33-35,40-46.
[31]全国重要矿产成矿地质背景研究子项目组.全国大地构造分区划分方案[C].北京,2006.
[32]张伯声,王战.地壳波浪状镶嵌构造学说摘要[J].长安大学学报(地球科学版).1993,15(4):6-10.
[33]张文佑.断块构造导论[M].石油工业出版社.1984:296-318.
[34]李锡荣,伦志强等.内蒙古自治区区域地质志[M].北京:地质出版社.1991:.
[35]余靖安等.内蒙古自治区赤峰市南部金矿第二轮成矿远景区划报告[R].内蒙古自治区第三地质矿产勘查开发院.1993.
[36]谷峰.内蒙古镶黄旗-赤峰地区二叠纪地层的新认识[C].中国北方板块构造文集.1983.
[37]李宏臣.华北地台北缘金矿类型及成矿区带[J].地质找矿论丛.2001,16(3):167-172.
[38]朴寿成,李绪俊,师磊等.赤峰-朝阳金矿化集中区元素分带特征及其应用[J].地质与勘探.2006,42(1):17-20.
[39]肖荣阁,彭润民,王美娟等.华北地台北缘西段主要成矿系统分析[J].地球科学—中国地质大学学报.2000,25(4):362-368.
[40]谢学锦,邵跃,王学求.矿产勘查地球化学[M].北京:地质出版社.1999:61-195.
[41]王继伦,李善芳,齐文秀等.中国金矿物探、化探方法技术的研究与应用[M].地质出版社.1997,123-200.
[42]雷万杉,张振庭,刘亚剑等.吉林江源县小石人金矿综合勘查方法研究[J].世界地质.2009.28(1):45-52.
[43]李月柱,于文卿.金矿床上元素的地球化学组合[J].国外铀金地质.1996,V13(4):313-319.
[44]张义,李公时.化探异常多元素组合模式识别[J].甘肃地质学报.1997,6(增):62-66.
[45]李惠,张文华,刘宝林等.中国主要类型金矿床的原生晕轴向分带序列研究及其应用准则[J].地质与勘探.1999,35(1):32-35.
[46]杨万志,姜云辉,周军等.新疆区域地球化学参数特征及其研究意义[J].新疆地质.2008,26(3):236-239.
[47]黄太岭.胶莱盆地地球化学参数特征及赋金层位[J].物探与化探.2000,24(5):363-372.
[48]石玉臣.山东省焦家成矿带深部金成成矿预测研究及其应用[D].长春:吉林大学,2005:74-78.
[49]纪宏金.地球化学数据的统计分析[M].长春地质学院.1993:195-294.
[50]郭万超,陈学华.峪耳崖金矿床元素地球化学地质统计分析[J].地质找矿论从,2002,17(1):63-72.
[51] Williams T M,Gunn A G.Application of enzyme leach soil analysis for epithermal gold exploration in the Andes of Ecuador[J].Apllied Geochemistry,2002(17):367-385.
[52]方继萱.试论地球化学场的研究方法[J].西北地质.1999,32(1):28-34.
[53]何厚强.论区域地球化学场的结构性及其在异常评价中的意义[J].岩土工程界.1997,6(增):48-51.
[54]黄薰德,吴郁彦等.地球化学找矿[M].北京:地质出版社.1989:130-136.
[55]成都地质学院物探系.金属矿地球物理勘探[M].北京:地质出版社.1978:383-392.
[56]孟令顺,高锐等.亚东-格尔木岩石圈地学断面综合研究-青藏高原重力测量与岩石圈构造[M].北京:地质出版社.1992:44-83.
[57]娄德波.东天山铜镍矿产资源潜力评价方法研究[D].北京:中国地质科学院.2007:72-79.
[58]刘亚剑.山东省龙口南部地区金矿综合信息成矿预测[D].长春:吉林大学.2007:40.
[59]曹广利.内蒙红花沟金矿蚀变岩型金矿体控构造分析[J].世界地质.2001,20(4):353-355.
[60]内蒙古第三地质大队.内蒙古自治区赤峰市南部地区原生金矿资源总量预测报告[R].1988.
[61]内蒙古第三地质大队.红花沟金矿田大比例尺总量预测[R].1991.
[62]王建平,刘永山,董法先.内蒙古金厂沟梁金矿构造控矿分析[M].北京:地质出版社.1992:8-19.
[63]褚金锁.金厂沟梁矿床地质特征及成因[J].矿产与地质.2000,14(3):155-157.
[64]陈军强.内蒙赤峰金厂沟梁金矿床地质、地球化学特征及成因研究[D].长春:吉林大学.2006:14-32.
[65]内蒙古第三地质大队.金厂沟梁金矿田及其外围大比例尺综合信息金矿预测[R].1990.
[66]王有爵.辽西火山岩型金矿地质特征及成因讨论[J].辽宁地质.1990,12(4):289-303.
[67]沙德铭,董连慧,毋瑞身.西天山地区浅成低温热液型金矿地质特征及成矿模式[J].西北地质.2003,36(2):50-57.
[68]王忠.内蒙古陈家杖子隐爆角砾岩型金矿床地质特征及找矿方向[J].中国地质.2004, 31(2):206-212.
[69]王喜宽,王宝林,廖蕾等.陈家杖子金矿地球化学特征及其指示意义[J].2005. 29(4):308-314.
[70]王存贤,杨文华,黄占起.内蒙古陈家杖子金矿地质特征及资源潜力探讨[J].地质与资源.2003, 12(1):25-31.
[71]杨文华.内蒙古陈家杖子隐爆角砾岩筒及金矿床地质特征[J].内蒙古地质.2001,(2):7-12.
[72]佘宏全,张桂兰,张德全.赤峰陈家杖子隐爆角砾岩型金矿床地质地球化学特征与成因[J].矿床地质.2005, 24(4):373-386.
[73]王长秋,崔文元.辽西-赤峰一带太古代变质杂岩中石榴石的研究[J].岩石矿物学杂志.1992,(2):157-165.
[74]崔文元,王长秋,张承志.辽西-赤峰一带太古代变质岩中锆石U-Pb年龄[J].北京大学学报(自然科学版).1991,(2):229-236.
[75]张忠生,周乃武,王建国等.赤峰红花沟金矿田成矿规律与成矿预测[M].沈阳:东北大学出版社.1993:171-204.
[76]岳永君,何国琦.内蒙古林西县二八地一带的二叠统双峰式火山岩组合[C].北京:中国地质科学院地质研究所文集(26),1994.
[77]甘盛飞,钱祥磷.内蒙乌拉山群岩石的稀土地球化学特征及其所反映的成岩环境[J].北京大学学报(自然科学版).1991,(2):210-217.
[78]翟裕生.论成矿系统[J].地学前缘.1999,6(1):13-27.
[79]朱裕生.论矿床成矿模式[J].地质评论.1993,(3):216-222.
[80]李林华,任振湖.内蒙古红花沟金矿成矿地球化学模式[J].地质与勘探.1993(5):45-49.
[81]雷万杉,王淼,刘亚剑等.赤峰南部金地球化学块体评价[J].吉林大学学报(地球科学版).2009(3):255-261.
[82]曾建国,刘国春,刘永利等.内蒙古赤峰红花沟金矿田矿床成因[J].地质地球化学.2002,13(3):18.
[83]李石磊,王文华,刘国春等.内蒙古红花沟金矿控矿断裂构造[J].世界地质.2002, 21(2):126-129.
[84]鲍明学,冯波,赵洁心.内蒙古赤峰红花沟金矿田构造体系分析[J].黄金.2006, 27(6):14-17.
[85]李秀琴,杨吉.内蒙撰山子金矿赋存规律及成矿预测[J].长春科技大学学报.2000,30(1):32-35.
[86]张林,吴琼,杨春雷.内蒙撰山子金矿构造控矿规律与成矿预测[J].地质与勘探.1998,34(2):9-12.
[87]娄德波,肖克炎,孙艳等.区域矿产评价模型-以赤峰红花沟金矿为例[J].吉林大学学报(地球科学版).2008,38(4):559-565.
[88]李石磊,王文华,刘国春等.内蒙古红花沟金矿控矿断裂构造[J].世界地质.2002,21(2):126-129.
[89]程玉明,金昌珍,宋群等.华北地台北缘花岗岩绿岩型金矿田及盲矿体的成矿模型[J].吉林大学学报(地球科学版).1993,23(3):292-298.
[90]王诗元.吉南-石人镇-花山地区1:5万金矿资源预测[D].长春:吉林大学.2008,51-55.
[91]曹瑜,胡光道,杨志峰.GIS环境下地质变量自动提取与地质异常的圈定[J].计算机工程与应用.2003,14:81-85.
[92]杨毅恒,韩燕,徐兵等.多维地学数据处理技术与方法[M].北京:科学出版社.2002:12-37.
[93]丁建华.新疆东天山铜、镍、金矿资源潜力评价[D].北京:中国地质科学院.2007:87-89.
[94] Li Peilan,Yu Xingzhen. Locating mechanism study of several types of gold deposits[J]. Journal of Central South University of Technology. 1996, 3(1):54-57
[95] R. P. Shaw, R. D. Morton, J. Gray and H. R. Krouse.Origins of metamorphic lode gold deposits: Implications of stable isotope data from the central Rocky Mountains, Canada[J]. Mineralogy and Petrology, 1991,43(3):193-209.
[96] Raimundo NetunoVillas and Marcio Santos. Gold deposits of the Carajás mineral province: deposit types and metallogenesis[J]. 2001,36(3-4): 300-331.
[97] Hong Rui Fan, Ming Guo Zhai, Yi Han Xie and Jin Hui Yang. Ore-forming fluids associated with granite-hosted gold mineralization at the Sanshandao deposit, Jiaodong gold province, China[J]. Mineralium Deposita. 2003,38(6): 739-750.
[98] E.Gonzalez-Clavijo,M.A.Diez-Balda and F.Alvarez. Structural study of a semiductile strike-slip system in the Central Iberian Zone (Variscan Fold Belt, Spain): structural controls on gold deposits[J]. International Journal of Earth Sciences.1993,82.3:448-460.
[99] Sebastien Strebelle. Conditional Simulation of Complex Geological Structures Using Multiple-Point Statistics[J]. Mathematical Geology. 2002,34(1) :1-21.
[100] Gui-Hua Lin, Huifu Xu and Masao Fukushima. Monte Carlo and quasi-Monte Carlo sampling methods for a class of stochastic mathematical programs with equilibrium constraints[J]. Mathematical Methods of Operations Research.2008,67(3):423-441.
[2]王世称,范继璋,杨永华.矿产资源评价[M].长春:吉林科学技术出版社,1990:21-28.
[3]王世称,成秋明,范继璋.金矿资源综合信息评价方法[M].长春:吉林科学技术出版社,1990:1-21.
[4]王世称,王於天.综合信息解译原理与矿产预测图编制方法[M].长春:吉林大学出版社,1989:3-18.
[5] De Verle Harris著,文世澂译.矿产资源评价—过去、现在的看法和对未来趋势的展望[C].矿产资源评价和矿业经济分析方法与实践.1997:9-19.
[6] Lesley Wyborn,etc.Using GIS for mineral potential evaluation in areas with few known mineral occurrences[J]. Second National forum on GIS in the Geosciences.1995:29-31.
[7]胡惠民等.大比例尺成矿预测方法[M].北京:地质出版社.1995:4-7.
[8] Agterberg F.P.Combining indicator patterns in weights of evidence for resource evaluation[J].Nonrenewable Resources.1992:1.
[9] Agterberg F.P,Bonham Carter G.F.Statistical pattern integration for mineral exploration,in G.Gaal and D.F.Merriam(eds.)-Computer Applications for Mineral Exploration in Resource Exploration[M].Oxford :Pergamon Press.1990
[10] Brinck,J.W.Critical parameters for the production,depletion and substitution of mineral resources-a horizon beyond the limits to growth.Ceol.en Mijnb.1976, V55(3–4):185-194.
[11] Donald A Singer著,张莓译,未发现矿产资源三阶段定量评价的基本原理[C].矿产资源评价与矿业经济分析方法与实践.1997:12-22.
[12]程裕淇,陈毓川等.再论矿床的成矿系列问题-兼论中生代某些矿床的成矿系列[J].地质论评.1983,V29(2):127-141.
[13]陈毓川,裴荣富,宋天锐.中国矿床成矿系列初论[M].北京:地质出版社.1998.
[14]孙启祯.论边缘成矿-关于金属矿床的时空分布及其成因联系[J].地质与勘探.1986(1):7-14.
[15]孙启祯.边缘成矿与成矿边缘效应[J].地学前缘.1994,V1(3-4):176-183.
[16]翟裕生,彭润民,邓军,王建平,区域成矿学与找矿新思路[J],现代地质,2001(2):151-156.
[17]涂光炽.超大型矿床的找矿和理论研究[J].矿产与地质.1989(1):1-3.
[18]曾庆丰.我国矿田构造(内生金属矿床)研究现状与展望[J],地质与勘探,1979,4:48-55.
[19]季克俭,王立本.热源研究的重要进展和"三源"交代热液成矿学说[J].地学前缘.1994,1(3-4):126-132.
[20]裴荣富.金属成矿省等级体制成矿[J].矿床地质.2004,5(28):131-141.
[21]裴荣富,梅燕雄.矿产勘查的双控论与合理域模型[J].矿床地质.2001,20(4):307-312.
[22]谢学锦,刘大文.地球化学块体-概念与方法学的发展[J].中国地质.2002,29(3):225-233.
[23]赵鹏大,胡旺亮.地质异常理论与矿产预测[J].新疆地质.1992,10(2):93-100.
[24]赵鹏大,池顺都.初论地质异常[J].地球科学.1991,16(3):241-248.
[25]赵鹏大,孟宪国.地质异常与矿产预测[J].地球科学.1993,18(1):39-47.
[26]王世称,陈永良,夏立显.综合信息矿产预测理论与方法[M].北京:科学出版社.2000:183-203
[27]王世称,杨毅恒,李景朝.综合信息矿产资源预测中的定性数据分析方法[M].长春:吉林大学出版社.
[28]肖克炎.应用综合信息法研究成矿规律及成矿预测的新进展[J].地球科学进展.1994,9(2):18-23.
[29]叶天竺.固体矿产预测评价方法技术[M].北京:中国大地出版社.2004:128-163.
[30]黄汲清.中国大地构造及其演化[M].科学出版社.1980:33-35,40-46.
[31]全国重要矿产成矿地质背景研究子项目组.全国大地构造分区划分方案[C].北京,2006.
[32]张伯声,王战.地壳波浪状镶嵌构造学说摘要[J].长安大学学报(地球科学版).1993,15(4):6-10.
[33]张文佑.断块构造导论[M].石油工业出版社.1984:296-318.
[34]李锡荣,伦志强等.内蒙古自治区区域地质志[M].北京:地质出版社.1991:.
[35]余靖安等.内蒙古自治区赤峰市南部金矿第二轮成矿远景区划报告[R].内蒙古自治区第三地质矿产勘查开发院.1993.
[36]谷峰.内蒙古镶黄旗-赤峰地区二叠纪地层的新认识[C].中国北方板块构造文集.1983.
[37]李宏臣.华北地台北缘金矿类型及成矿区带[J].地质找矿论丛.2001,16(3):167-172.
[38]朴寿成,李绪俊,师磊等.赤峰-朝阳金矿化集中区元素分带特征及其应用[J].地质与勘探.2006,42(1):17-20.
[39]肖荣阁,彭润民,王美娟等.华北地台北缘西段主要成矿系统分析[J].地球科学—中国地质大学学报.2000,25(4):362-368.
[40]谢学锦,邵跃,王学求.矿产勘查地球化学[M].北京:地质出版社.1999:61-195.
[41]王继伦,李善芳,齐文秀等.中国金矿物探、化探方法技术的研究与应用[M].地质出版社.1997,123-200.
[42]雷万杉,张振庭,刘亚剑等.吉林江源县小石人金矿综合勘查方法研究[J].世界地质.2009.28(1):45-52.
[43]李月柱,于文卿.金矿床上元素的地球化学组合[J].国外铀金地质.1996,V13(4):313-319.
[44]张义,李公时.化探异常多元素组合模式识别[J].甘肃地质学报.1997,6(增):62-66.
[45]李惠,张文华,刘宝林等.中国主要类型金矿床的原生晕轴向分带序列研究及其应用准则[J].地质与勘探.1999,35(1):32-35.
[46]杨万志,姜云辉,周军等.新疆区域地球化学参数特征及其研究意义[J].新疆地质.2008,26(3):236-239.
[47]黄太岭.胶莱盆地地球化学参数特征及赋金层位[J].物探与化探.2000,24(5):363-372.
[48]石玉臣.山东省焦家成矿带深部金成成矿预测研究及其应用[D].长春:吉林大学,2005:74-78.
[49]纪宏金.地球化学数据的统计分析[M].长春地质学院.1993:195-294.
[50]郭万超,陈学华.峪耳崖金矿床元素地球化学地质统计分析[J].地质找矿论从,2002,17(1):63-72.
[51] Williams T M,Gunn A G.Application of enzyme leach soil analysis for epithermal gold exploration in the Andes of Ecuador[J].Apllied Geochemistry,2002(17):367-385.
[52]方继萱.试论地球化学场的研究方法[J].西北地质.1999,32(1):28-34.
[53]何厚强.论区域地球化学场的结构性及其在异常评价中的意义[J].岩土工程界.1997,6(增):48-51.
[54]黄薰德,吴郁彦等.地球化学找矿[M].北京:地质出版社.1989:130-136.
[55]成都地质学院物探系.金属矿地球物理勘探[M].北京:地质出版社.1978:383-392.
[56]孟令顺,高锐等.亚东-格尔木岩石圈地学断面综合研究-青藏高原重力测量与岩石圈构造[M].北京:地质出版社.1992:44-83.
[57]娄德波.东天山铜镍矿产资源潜力评价方法研究[D].北京:中国地质科学院.2007:72-79.
[58]刘亚剑.山东省龙口南部地区金矿综合信息成矿预测[D].长春:吉林大学.2007:40.
[59]曹广利.内蒙红花沟金矿蚀变岩型金矿体控构造分析[J].世界地质.2001,20(4):353-355.
[60]内蒙古第三地质大队.内蒙古自治区赤峰市南部地区原生金矿资源总量预测报告[R].1988.
[61]内蒙古第三地质大队.红花沟金矿田大比例尺总量预测[R].1991.
[62]王建平,刘永山,董法先.内蒙古金厂沟梁金矿构造控矿分析[M].北京:地质出版社.1992:8-19.
[63]褚金锁.金厂沟梁矿床地质特征及成因[J].矿产与地质.2000,14(3):155-157.
[64]陈军强.内蒙赤峰金厂沟梁金矿床地质、地球化学特征及成因研究[D].长春:吉林大学.2006:14-32.
[65]内蒙古第三地质大队.金厂沟梁金矿田及其外围大比例尺综合信息金矿预测[R].1990.
[66]王有爵.辽西火山岩型金矿地质特征及成因讨论[J].辽宁地质.1990,12(4):289-303.
[67]沙德铭,董连慧,毋瑞身.西天山地区浅成低温热液型金矿地质特征及成矿模式[J].西北地质.2003,36(2):50-57.
[68]王忠.内蒙古陈家杖子隐爆角砾岩型金矿床地质特征及找矿方向[J].中国地质.2004, 31(2):206-212.
[69]王喜宽,王宝林,廖蕾等.陈家杖子金矿地球化学特征及其指示意义[J].2005. 29(4):308-314.
[70]王存贤,杨文华,黄占起.内蒙古陈家杖子金矿地质特征及资源潜力探讨[J].地质与资源.2003, 12(1):25-31.
[71]杨文华.内蒙古陈家杖子隐爆角砾岩筒及金矿床地质特征[J].内蒙古地质.2001,(2):7-12.
[72]佘宏全,张桂兰,张德全.赤峰陈家杖子隐爆角砾岩型金矿床地质地球化学特征与成因[J].矿床地质.2005, 24(4):373-386.
[73]王长秋,崔文元.辽西-赤峰一带太古代变质杂岩中石榴石的研究[J].岩石矿物学杂志.1992,(2):157-165.
[74]崔文元,王长秋,张承志.辽西-赤峰一带太古代变质岩中锆石U-Pb年龄[J].北京大学学报(自然科学版).1991,(2):229-236.
[75]张忠生,周乃武,王建国等.赤峰红花沟金矿田成矿规律与成矿预测[M].沈阳:东北大学出版社.1993:171-204.
[76]岳永君,何国琦.内蒙古林西县二八地一带的二叠统双峰式火山岩组合[C].北京:中国地质科学院地质研究所文集(26),1994.
[77]甘盛飞,钱祥磷.内蒙乌拉山群岩石的稀土地球化学特征及其所反映的成岩环境[J].北京大学学报(自然科学版).1991,(2):210-217.
[78]翟裕生.论成矿系统[J].地学前缘.1999,6(1):13-27.
[79]朱裕生.论矿床成矿模式[J].地质评论.1993,(3):216-222.
[80]李林华,任振湖.内蒙古红花沟金矿成矿地球化学模式[J].地质与勘探.1993(5):45-49.
[81]雷万杉,王淼,刘亚剑等.赤峰南部金地球化学块体评价[J].吉林大学学报(地球科学版).2009(3):255-261.
[82]曾建国,刘国春,刘永利等.内蒙古赤峰红花沟金矿田矿床成因[J].地质地球化学.2002,13(3):18.
[83]李石磊,王文华,刘国春等.内蒙古红花沟金矿控矿断裂构造[J].世界地质.2002, 21(2):126-129.
[84]鲍明学,冯波,赵洁心.内蒙古赤峰红花沟金矿田构造体系分析[J].黄金.2006, 27(6):14-17.
[85]李秀琴,杨吉.内蒙撰山子金矿赋存规律及成矿预测[J].长春科技大学学报.2000,30(1):32-35.
[86]张林,吴琼,杨春雷.内蒙撰山子金矿构造控矿规律与成矿预测[J].地质与勘探.1998,34(2):9-12.
[87]娄德波,肖克炎,孙艳等.区域矿产评价模型-以赤峰红花沟金矿为例[J].吉林大学学报(地球科学版).2008,38(4):559-565.
[88]李石磊,王文华,刘国春等.内蒙古红花沟金矿控矿断裂构造[J].世界地质.2002,21(2):126-129.
[89]程玉明,金昌珍,宋群等.华北地台北缘花岗岩绿岩型金矿田及盲矿体的成矿模型[J].吉林大学学报(地球科学版).1993,23(3):292-298.
[90]王诗元.吉南-石人镇-花山地区1:5万金矿资源预测[D].长春:吉林大学.2008,51-55.
[91]曹瑜,胡光道,杨志峰.GIS环境下地质变量自动提取与地质异常的圈定[J].计算机工程与应用.2003,14:81-85.
[92]杨毅恒,韩燕,徐兵等.多维地学数据处理技术与方法[M].北京:科学出版社.2002:12-37.
[93]丁建华.新疆东天山铜、镍、金矿资源潜力评价[D].北京:中国地质科学院.2007:87-89.
[94] Li Peilan,Yu Xingzhen. Locating mechanism study of several types of gold deposits[J]. Journal of Central South University of Technology. 1996, 3(1):54-57
[95] R. P. Shaw, R. D. Morton, J. Gray and H. R. Krouse.Origins of metamorphic lode gold deposits: Implications of stable isotope data from the central Rocky Mountains, Canada[J]. Mineralogy and Petrology, 1991,43(3):193-209.
[96] Raimundo NetunoVillas and Marcio Santos. Gold deposits of the Carajás mineral province: deposit types and metallogenesis[J]. 2001,36(3-4): 300-331.
[97] Hong Rui Fan, Ming Guo Zhai, Yi Han Xie and Jin Hui Yang. Ore-forming fluids associated with granite-hosted gold mineralization at the Sanshandao deposit, Jiaodong gold province, China[J]. Mineralium Deposita. 2003,38(6): 739-750.
[98] E.Gonzalez-Clavijo,M.A.Diez-Balda and F.Alvarez. Structural study of a semiductile strike-slip system in the Central Iberian Zone (Variscan Fold Belt, Spain): structural controls on gold deposits[J]. International Journal of Earth Sciences.1993,82.3:448-460.
[99] Sebastien Strebelle. Conditional Simulation of Complex Geological Structures Using Multiple-Point Statistics[J]. Mathematical Geology. 2002,34(1) :1-21.
[100] Gui-Hua Lin, Huifu Xu and Masao Fukushima. Monte Carlo and quasi-Monte Carlo sampling methods for a class of stochastic mathematical programs with equilibrium constraints[J]. Mathematical Methods of Operations Research.2008,67(3):423-441.