招平断裂带金矿勘查模型与成矿预测
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摘要
胶东以约0.3%的国土面积占有中国约25%的黄金储量,是中国最重要的金矿集中区和黄金产区,该区经历了长期的构造—岩浆活动,形成了复杂的构造格架和一系列岩浆岩。近年来,广大地质工作者深入贯彻“理论先导、攻深找盲、瞄准大带、重点突破”的找矿思路,金矿床研究和普查找矿不断取得突破。
招平断裂带是胶东地区最重要的金成矿带之一,前人做了大量研究工作,多侧重于矿床尺度的观测和分析,对整个成矿带进行系统研究和总结,进而构建各类金矿类型及深部矿体勘查模型方面还缺乏系统性。勘查实践证明,找矿的成功率越来越依赖于成矿规律研究和成矿预测的开展,而在信息集成基础上建立勘查模型指导找矿已越来越受到重视。本文运用成矿系统的理论和方法,在充分收集、消化前人研究成果和工作资料的基础上,结合科研项目和本职勘查工作,开展金矿调查研究,系统采集各种岩石和矿石样品,开展大量的测试分析工作,总结成矿地质背景及矿床地质-地球化学-地球物理特征,分析招平带成矿系统各要素,解剖典型金矿床,总结控矿规律,建立勘查模型,开展成矿预测。
论文总结了招平断裂带分段地质特征、构造控矿型式、成矿规律、找矿方向和成矿模式,金矿带产出石英脉型(玲珑式)、蚀变岩型(焦家式)及过渡型(灵山沟式)三种金矿类型,具有构造-蚀变—矿化的水平分带性,自黄铁绢英岩化碎裂岩→黄铁绢英岩化花岗质碎裂岩→花岗质碎裂岩→碎裂状花岗岩,岩石的破碎程度逐渐降低(碎粒岩到碎裂岩),矿化逐渐减弱(浸染状、密集网脉状到稀疏脉状矿化),蚀变分带明显(黄铁绢英岩化、绢英岩化、硅化到钾化带)。断裂带多期叠加成矿作用明显,至少有金成矿期和银多金属成矿期两期成矿作用复合,两期成矿的成矿元素不同,金成矿期划分4个成矿阶段,银多金属成矿期划分3个成矿阶段。根据断裂带微量元素特征,探讨了成矿物质来源,估算了断裂带资源潜力。在多元信息集成的基础上,构建了招平断裂带六类勘查模型:矿床(体)综合预测模型、矿床(体)定位综合预测模型、焦家式金矿地质-地球物理勘查模型、焦家式金矿地质-地球化学勘查模型、玲珑式金矿地质-地球物理勘查模型、深部矿体定位预测模型。开展了成矿预测,圈定成矿预测区11处,经工程验证,取得了较满意的找矿效果。
The Jiaodong peninsula, accounting for 0.3% of China’s land area and hosting 25% of the nation’s gold reserve, is one of the most important gold mine concentrating and gold production area. This area underwent a long tectonic-magmatic evolution, and formed a complex geological structural framework and a series of magmatic rocks. Putting into practice the prospecting idea of“Theory direct, exploring depth and blind, focusing on huge belts, breakthrough in key areas”, gold deposit research and preliminary geological survey and prospecting have made important progress in recent years.
The Zhao-Ping fault zone is the most important gold metallogenic belts in Jiaodong. Lots of research focusing on the deposit-scale observation and analysis were done. While systematic research and summaries of the whole gold belt are weak, and lack of systematic build of deep gold ore body’s exploration models of different gold deposit types. It has been proved by the prospecting practice that the successes of mineral deposit prospecting rely on the prediction based on metallogenic regularity studies. Hence, more importance has been attached on the prediction of exploration model building based on geological information integration. Field observations were done, and collected samples of rocks and ores were tested and analyzed. Directed by the metallogenic theory, and in combination of scientific research projects and exploration work, I collected and analyzed systematically the existing data and research results. Summaries were done to geological settings, mineral deposit geology, and regional geochemical and geophysical characters. Analyses were done to factors of gold metallogenic system of the Zhaoping fault zone. Gold mtallogenic prediction was done according to the established exploration model based on summaries of metallogenic regularities and detailed analyses of typical gold deposits.
This paper summarized the segment geological features of the Zhaoping fault, Ore-Control Structures, metallogenic regularities, gold prospecting area and metallogenic model. There are three types of gold deposits, the quartz vein type (the Linglong type), the structural altered rock type (the Jiaojia type), and the intermediate type (the Lingshangou type), in the Zhaoping fault zone, which show clear lateral structural, alteration and mineralization zones from proximal phyllic alteration bearing pyrite, phyllic alteration, to distal siliconization and potassic feldspar alteration. From proximal to distal, the degree of crushing decrease from crush rocks to fractured rocks, and the mineralization degree decrease from disseminated and dense stockwork to sparse stockwork. There exist at least two events of mineralization in the Zhaoping fault zone, the former gold mineralization and the later silver and base metal mineralization. The gold mineralization event contains four stages, and the silver and base metal mineralization contains three stages. The sources of ore materials were discussed base on the trace elements analysis. The resources potential of the Zhaoping fault belt was estimated. Based on multi-geology information integration, six exploration models were built in the Zhaoping fault zone. They are gold ore deposit (bodies) integrated forecasting model, gold ore deposit (bodies) location prediction integrated model, geological-geophysical exploration model for Jiaojia type gold deposits, geological-geochemical exploration model for Jiaojia type gold deposits, geological-geophysical exploration model for Linglong type gold deposits, geological-geochemical exploration model for Linglong type gold deposits, deep ore bodies location prediction model. Based on these models, gold prediction was made, and 11 prospecting area were delineated. Satisfactory exploration results were achieved by engineering validation according to the prediction.
招平断裂带是胶东地区最重要的金成矿带之一,前人做了大量研究工作,多侧重于矿床尺度的观测和分析,对整个成矿带进行系统研究和总结,进而构建各类金矿类型及深部矿体勘查模型方面还缺乏系统性。勘查实践证明,找矿的成功率越来越依赖于成矿规律研究和成矿预测的开展,而在信息集成基础上建立勘查模型指导找矿已越来越受到重视。本文运用成矿系统的理论和方法,在充分收集、消化前人研究成果和工作资料的基础上,结合科研项目和本职勘查工作,开展金矿调查研究,系统采集各种岩石和矿石样品,开展大量的测试分析工作,总结成矿地质背景及矿床地质-地球化学-地球物理特征,分析招平带成矿系统各要素,解剖典型金矿床,总结控矿规律,建立勘查模型,开展成矿预测。
论文总结了招平断裂带分段地质特征、构造控矿型式、成矿规律、找矿方向和成矿模式,金矿带产出石英脉型(玲珑式)、蚀变岩型(焦家式)及过渡型(灵山沟式)三种金矿类型,具有构造-蚀变—矿化的水平分带性,自黄铁绢英岩化碎裂岩→黄铁绢英岩化花岗质碎裂岩→花岗质碎裂岩→碎裂状花岗岩,岩石的破碎程度逐渐降低(碎粒岩到碎裂岩),矿化逐渐减弱(浸染状、密集网脉状到稀疏脉状矿化),蚀变分带明显(黄铁绢英岩化、绢英岩化、硅化到钾化带)。断裂带多期叠加成矿作用明显,至少有金成矿期和银多金属成矿期两期成矿作用复合,两期成矿的成矿元素不同,金成矿期划分4个成矿阶段,银多金属成矿期划分3个成矿阶段。根据断裂带微量元素特征,探讨了成矿物质来源,估算了断裂带资源潜力。在多元信息集成的基础上,构建了招平断裂带六类勘查模型:矿床(体)综合预测模型、矿床(体)定位综合预测模型、焦家式金矿地质-地球物理勘查模型、焦家式金矿地质-地球化学勘查模型、玲珑式金矿地质-地球物理勘查模型、深部矿体定位预测模型。开展了成矿预测,圈定成矿预测区11处,经工程验证,取得了较满意的找矿效果。
The Jiaodong peninsula, accounting for 0.3% of China’s land area and hosting 25% of the nation’s gold reserve, is one of the most important gold mine concentrating and gold production area. This area underwent a long tectonic-magmatic evolution, and formed a complex geological structural framework and a series of magmatic rocks. Putting into practice the prospecting idea of“Theory direct, exploring depth and blind, focusing on huge belts, breakthrough in key areas”, gold deposit research and preliminary geological survey and prospecting have made important progress in recent years.
The Zhao-Ping fault zone is the most important gold metallogenic belts in Jiaodong. Lots of research focusing on the deposit-scale observation and analysis were done. While systematic research and summaries of the whole gold belt are weak, and lack of systematic build of deep gold ore body’s exploration models of different gold deposit types. It has been proved by the prospecting practice that the successes of mineral deposit prospecting rely on the prediction based on metallogenic regularity studies. Hence, more importance has been attached on the prediction of exploration model building based on geological information integration. Field observations were done, and collected samples of rocks and ores were tested and analyzed. Directed by the metallogenic theory, and in combination of scientific research projects and exploration work, I collected and analyzed systematically the existing data and research results. Summaries were done to geological settings, mineral deposit geology, and regional geochemical and geophysical characters. Analyses were done to factors of gold metallogenic system of the Zhaoping fault zone. Gold mtallogenic prediction was done according to the established exploration model based on summaries of metallogenic regularities and detailed analyses of typical gold deposits.
This paper summarized the segment geological features of the Zhaoping fault, Ore-Control Structures, metallogenic regularities, gold prospecting area and metallogenic model. There are three types of gold deposits, the quartz vein type (the Linglong type), the structural altered rock type (the Jiaojia type), and the intermediate type (the Lingshangou type), in the Zhaoping fault zone, which show clear lateral structural, alteration and mineralization zones from proximal phyllic alteration bearing pyrite, phyllic alteration, to distal siliconization and potassic feldspar alteration. From proximal to distal, the degree of crushing decrease from crush rocks to fractured rocks, and the mineralization degree decrease from disseminated and dense stockwork to sparse stockwork. There exist at least two events of mineralization in the Zhaoping fault zone, the former gold mineralization and the later silver and base metal mineralization. The gold mineralization event contains four stages, and the silver and base metal mineralization contains three stages. The sources of ore materials were discussed base on the trace elements analysis. The resources potential of the Zhaoping fault belt was estimated. Based on multi-geology information integration, six exploration models were built in the Zhaoping fault zone. They are gold ore deposit (bodies) integrated forecasting model, gold ore deposit (bodies) location prediction integrated model, geological-geophysical exploration model for Jiaojia type gold deposits, geological-geochemical exploration model for Jiaojia type gold deposits, geological-geophysical exploration model for Linglong type gold deposits, geological-geochemical exploration model for Linglong type gold deposits, deep ore bodies location prediction model. Based on these models, gold prediction was made, and 11 prospecting area were delineated. Satisfactory exploration results were achieved by engineering validation according to the prediction.
引文
[1]曹新志,高秋斌,徐伯骏,等.矿区深部矿体定位预测的有效途径和方法研究-以山东招远界河金矿为例.中国地质大学出版社,2005:2-56
[2]陈光远,邵伟,孙岱生.胶东金矿成因矿物学与找矿.重庆:重庆出版社,1989,1-45
[3]陈国华,刘连登,仲崇学.胶东金矿床的矿石地球化学研究.世界地质,1998,17(2):19-26
[4]陈毓川,李廷栋,彭齐鸣,等.矿产资源与可持续发展.北京:中国科学技术出版社, 1999,1-16
[5]陈毓川,李兆鼐,毋瑞身,等.中国金矿床及其成矿规律.北京:地质出版社, 2001
[6]邓军,高帮飞,王庆飞,等.成矿流体系统的形成与演化.地质科技情报,2005,24(1):50- 55
[7]邓军,杨立强,方云.成矿系统嵌套分形结构和自有序效应.地学前缘,2000,7(1): 133-146
[8]邓军,方云,杨立强,等.剪切蚀变与物质迁移及金的富集.地球科学,2000,25(1): 428-437
[9]邓军,吕古贤,杨立强,等.构造应力场转换与界面成矿.地球学报,1998,19(3):244-250
[10]邓军,孙忠实,王建平,等.动力系统转换与金成矿作用.矿床地质,2001,20(1): 71-77
[11]邓军,王庆飞,杨立强,等.胶东西北部金热液成矿系统内部结构解析.地球科学, 2005,30(1):102-108
[12]邓军,王庆飞,杨立强,等.胶西北金矿集成矿作用发生的地质背景.地学前缘, 2004,11(4):527-533
[13]邓军,徐守礼,方云,等.胶东西北部构造体系及金成矿动力学.北京:地质出版社. 1996
[14]邓军,徐守礼,吕古贤,等.胶东西北部断裂构造与成矿作用研究.现代地质,1996, 10(4):424-432
[15]邓军,杨立强,方云,等.胶东地区壳幔相互作用与金成矿效应.地质科学,2000, 35(1):60-70
[16]邓军,杨立强,葛良胜,等.胶东矿集区形成的构造体制研究进展.自然科学进展, 2006,16(5):513-518
[17]邓军,杨立强,孙忠实,等.构造体制转换与流体多层循环成矿动力学.地球科学, 2000,25(4):397-403
[18]邓军,杨立强,孙忠实,等.矿源系统地质-地球化学例析.现代地质,2000,25(1):165- 172
[19]邓军,杨立强,翟裕生,等.构造-流体-成矿系统及其动力学的理论格架与方法体系.地球科学,2000,25(1):71-78
[20]邓军,杨立强,翟裕生,等.地质体元素组合与矿源系统组成及演化.地球学报, 1999,20(增刊):414-419
[21]邓军,杨立强,翟裕生,等.胶东招掖矿集区巨量金质来源和流体成矿效应.地质科,2001,36(3):257-268
[22]邓军,翟裕生,杨立强,等.论剪切带构造成矿系统,现代地质,1998,12(4):493-500
[23]邓军,翟裕生,杨立强,等.构造演化与成矿系统动力学-以胶东金矿集中区为例.地学前缘,1999,6(2):315-323
[24]邓军,翟裕生,杨立强,等.剪切带构造-流体-成矿系统动力学模拟.地学前缘,1999,6(1),115-129
[25]邓军,房天文,杨立强,等.山东省招远市大尹格庄金矿床多元构造体制叠接与4D矿化网络研究.科研报告,2005
[26]邓军,王庆飞,杨立强,等.胶东西北部金热液成矿系统内部结构解析,地球科学, 2005,30(1):102-108
[27]丁式江,翟裕生,邓军.胶东地区地质体含金性的地质地球化学评价.地质找矿论丛,1997,12(3):1-9
[28]杜杨松,壳幔成矿学初探.矿床地质,1999,18(4):341-346
[29]范永香,胡家杰,卢作祥,等.山东招(远)-平(度)断裂构造南段上庄地区构造控矿规律研究.中国地质大学(武汉),黄金研究所,1991
[30]范永香,阳正熙.成矿规律与成矿预测.徐州:中国矿业大学出版社, 2003
[31]郭光裕.脉状金矿床深部大比例尺统计预测.武汉:中国地质大学出版社, 1989
[32]郭涛.胶西北金矿区域成矿系统及其构造-流体-矿化研究.中国地质大学(北京), 2008年博士学位论文
[33]高帮飞.山东招平金矿带构造-流体耦合成矿动力学.中国地质大学(北京),2008年博士学位论文
[34]高秋斌,范永香,王可勇,等.金矿床深部成矿预测的主要途径.黄金地质,1998,4(2):21-26
[35]高占林,林尔为.金厂峪金矿有关岩石金丰度的研究.长春地质学院学报, 1987,17 (1):23-32
[36]胡受奚,王鹤年,王德滋,等.中国东部金矿地质学及地球化学.科学出版社,1998
[37]韩润生,陈进,高德荣,等.构造地球化学在隐伏矿定位预测中的应用.地质与勘探, 2003,39(6):25-29
[38]黎彤,倪守斌.地球化学讲义.广州:冶金工业部广东冶金地质勘探公司,1982
[39]李惠,郑涛,汤磊,等.山东招远大尹格庄金矿床隐伏矿定位预测的叠加晕模式.有色金属矿产与勘查,1998,7(3):178-185
[40]李惠,张文华,常凤池,等.大型、特大型金矿盲矿预测的原生叠加晕模型.北京:冶金工业出版社,1998,84-95,114-119
[41]李惠,张文华.胶东大型金矿床的地球化学分带特征.贵金属地质,1999,8(4),217-222
[42]李惠,张文华.胶东大型金矿床的地球化学分带特征.贵金属地质,1999,8(4): 217-222
[43]李四光.地质力学概论.北京:科学出版社,1973
[44]李士先,刘长春,安郁宏,等.胶东金矿地质.北京:地质出版社, 2007
[45]李卫革,李龙义,张瑞忠,等.胶东大尹格庄金矿床地质特征与深部资源前景.地质力学学报,2003,9(3):254-260
[46]李晓英.招远地区金矿找矿若干问题浅析.山东招金集团公司矿山地质论文集,地震出版社,2001,20-31
[47]李俊建,沈保丰.华北地台主要花岗岩-绿岩带含金丰度值的研究.前寒武纪研究进展, 1997, 20(4), 25-33
[48]李兆龙,杨敏之,李治平,等.胶东金矿床地质地球化学.天津:天津科学技术出版社,1993
[49]李金祥.胶东西北部招平断裂带构造特征与成矿.中国地质大学(北京)博士论文,2005
[50]林文蔚,赵一鸣,徐钰.胶东招远-平度断裂活动性质及活动时代.中国区域地质,2000,19(1),43-50
[51]凌洪飞,胡受奚,孙景贵,等.胶东金青顶和大尹格庄金矿床花岗质围岩的蚀变地球化学研究.矿床地质, 2002,21(2):187-199
[52]刘玉强,李洪喜,黄太岭,等.山东省金、铁、煤矿床成矿系列及成矿预测.地质出版社,2004
[53]刘光智.胶东地区岩浆岩与金-多金属矿的关系.黄金,2003,24(11):12-16
[54]卢焕章,Guha J,方根保.山东玲珑金矿的成矿流体特征.地球化学,1999,28(5): 421-437
[55]卢作祥,范永香,刘石年.山东玲珑金矿田断裂构造控矿作用探讨.地球科学-武汉地质学院学报,1983,(3),127-138
[56]吕古贤,林文蔚,罗元华,等.构造物理化学与金成矿预测.北京:地质出版社,1999
[57]吕古贤,杨敏之.胶东玲珑-焦家式金矿地质.北京:科学出版社,1993
[58]吕古贤,韦昌山,郭涛,等.胶东矿集区金矿成矿地质事件研究初探.黄金地质,2004, 10(2):1-6
[59]罗镇宽,苗来成.胶东招莱地区花岗岩和金矿床.北京:冶金工业出版社,2002
[60]罗镇宽,关康,余和勇,等.胶东招莱地区大-超大型金矿床形成的几个关键因素.地质找矿论丛,2003,18(2):95-102
[61]罗镇宽,关康,苗来成.胶东玲珑金矿田煌斑岩脉与成矿关系的讨论.黄金地质, 2001, 7(4):15-20
[62]苗来成,罗镇宽,黄佳展.山东招掖金矿带内花岗岩类侵入体锆石SHRIMP研究及其意义.中国科学,1997,27(3): 207-213
[63]苗来成,朱成伟,翟裕生,等.山东招掖金矿带内花岗岩与金矿化关系探讨,黄金地质,1999,5(4),7-10
[64]山东省地质六队.大尹格庄金矿床勘探地质报告.1993 (内部资料)
[65]山东招金集团公司.招远金矿集中区地质与找矿.北京:地震出版社,2002
[66]申玉科,邓军,徐叶兵.煌斑岩在玲珑金矿田形成过程中的地质意义.地质与勘探,2005,41(3):45-49
[67]沈昆,胡受奚,孙景贵,等.山东招远大尹格庄金矿成矿流体特征.岩石学报, 2000.16(4):542-551
[68]沈远超,曾庆栋,刘铁兵,等.郯庐断裂与金矿成矿.世界地质,2003,22(1):41-44
[69]申萍,沈远超,李光明,等.胶东金牛山金矿区深部地球化学特征及成矿预测.地质与勘探, 2003,39(4):21-26
[70]孙丰月.胶东地区中新生代区域构造演化与成矿.长春地质学院学报,1994(24),378-422
[71]孙殿卿,高庆华.隐伏矿床预测.北京:地质出版社,1987
[72]孙国胜,姚风良,胡瑞忠,等.玲珑金矿田矿体富集规律及其控制因素.大地构造与成矿学,2001, 25(4), 464-470
[73]孙国胜,刘颖,李绪俊,等.玲珑金矿田不同级别构造控矿特征.地质地球化学,2003,31(2):18-24
[74]孙国胜,李绪俊,姚风良,等.玲珑金矿田矿物组合与地球化学分带及矿体定位预测意义.地质与勘探,2002,38(4):28-31
[75]孙林,马学欣.招远地区北西向断裂构造控矿浅析.山东招金集团公司矿山地质论文集,地震出版社,2001,33-37
[76]涂光炽等.中国超大型矿床.北京:科学出版社,2000,1-583
[77]王建平,戚开静,杨立强.中国金矿床发现的启示.地质找矿论丛,2001,16(2): 104-107
[78]王义文,朱奉三,宫润潭.胶东金矿集中区金矿成矿年代学研究.黄金地质,2002,8(4): 48-55
[79]王义文,朱奉三,宫润谭.构造同位素地球化学-胶东金矿集中区硫同位素再研究.黄金,2002(23):1-16
[80]王世称,杨毅恒,严光生,等.大型、超大型金矿床密集区综合信息预测.北京:地质出版社,,2001,21-28
[81]王世称,刘玉强,伊丕厚,等.山东省金矿床及金矿床密集区综合信息成矿预测.北京:地质出版社, 2003
[82]王希今,鲍亚凡,李永胜.玲珑金矿田两种矿化类型元素空间分带性研究.黄金地质,2007(8):20-23
[83]吴淦国.矿田构造与成矿预测.地质力学学报,1998,4(2):1-4
[84]徐兵.中国山东半岛大尹格庄金矿床的地质与地球化学特征.东京大学博士论文,1999,1-139
[85]徐述平,朱洪岭,张华全.胶东大磨曲家金矿控矿断裂及成矿规律.黄金科学技术, 2006,12(2):11-22
[86]徐述平,邓军,高帮飞,等.胶东山后金矿床地质体微量元素特征及找矿意义.地质与勘探,2008 (5): 23-29
[87]徐贵忠,周瑞,王艺芬,等.胶东和鲁西地区中生代成矿作用重大差异性的内在因素.现代地质,2002, 16(1):9-16
[88]徐金方,沈步云,牛良柱,等.胶北地块与金矿有关的花岗岩类的研究.山东地质,1989, 5(2): 1-22
[89]徐刚,郑达兴,温长顺.胶东焦家断裂带与金矿的成生关系.地质力学学报,1998(4):53-58
[90]杨金中,李光明.胶东中生代两期金矿化作用的对比研究及其意义.地质与勘探, 2001,37(1):33-37
[91]杨金中,沈远超,刘铁兵.大型-超大型金矿密集区的形成条件.地质与勘探, 2001,37(1):30-33
[92]杨进辉,朱美妃,刘伟,等.胶东地区郭家岭花岗闪长岩的地球化学特征及成因.岩石学报, 2003,19(4): 692-700
[93]杨锋,刘连登,陈国华.平度1号脉金矿晚期叠加成矿初探.黄金,2001,22(5):1-5
[94]杨立强,邓军,方云,等.构造-流体成矿效应计算模拟.地球学报,1999,20(增刊): 433-437
[95]杨立强,邓军,葛良胜,等.胶东金矿成矿时代和矿床成因研究述评.自然科学进展, 2006,16(7): 797-802
[96]杨立强,邓军,王庆飞,等.深部构造与地质过程控矿研究.矿床地质,2006,25(增刊): 107-110
[97]杨立强,邓军,翟裕生.构造-流体-成矿系统及其动力学.地学前缘,2000,7(1):178
[98]杨立强,邓军,翟裕生,等.胶东夏甸金矿地球化学场结构.现代地质,2001,15(4): 409-413
[99]杨立强,邓军,张中杰,等.构造应力场转换的成矿地球化学响应.大地构造与成矿学,2003,27 (3):243-249
[100]杨立强,张中杰,邓军.深浅构造耦合成矿效应-以胶东招掖金矿带为例.地学前缘, 2004,11(1):56
[101]杨立强,张中杰,王光杰,等.胶东金矿集中区岩石圈结构与深部成矿作用.地球科学,2000, 25(4): 421-427
[102]杨忠芳,徐景奎,赵伦山,等.胶东区域地壳演化与金成矿作用地球化学.北京:地质出版社, 1998
[103]杨敏之,吕古贤.胶东绿岩带型金矿地质地球化学.北京:地质出版社,1996
[104]杨敏之.金矿床围岩蚀变带地球化学-以胶东金矿床为例.北京:地质出版社,1998
[105]杨进辉,周新华,陈立辉.胶东地区破碎带蚀变岩型金矿时代的测定及其地质意义.岩石学报,2000,16(03):454-458
[106]姚凤良,刘连登,孔庆存,等.胶东西北部脉状金矿长春.吉林科学技术出版社,1990
[107].於崇文.成矿动力系统在混沌边缘分形生长—一种新的成矿理论与方法论(上).地学前缘,2001,(06): 28-34
[108]於崇文.成矿作用动力学.北京:地质出版社,1998
[109]於崇文.大型矿床和成矿区(带)在混沌边缘.地学前缘,1999,6(1):85-101
[110]翟裕生,邓军,崔彬,等.成矿系统及综合地质异常.现代地质,1999,13(1):99-104
[111]翟裕生,邓军,李晓波.区域成矿学.北京:地质出版社,1999
[112]翟裕生,邓军,汤中立,等.古陆边缘成矿系统.北京:地质出版社,2002,1-416
[113]翟裕生,邓军,王建平,等.深部找矿研究问题.矿床地质,2004,23(2):143-149
[114]翟裕生,邓军,杨立强,等.山东夏甸金矿及其外围隐伏矿体定位预测.地学前缘, 1999,6(2):230
[115]翟裕生,吕古贤.构造动力体制转换与成矿作用.地球学报,2002,23(2):97-102
[116]翟裕生,张湖,宋鸿林,等.大型构造与超大型矿床.北京:地质出版社,1997
[117]翟裕生. 21世纪矿床学研究展望.中国地质,2000,(3): 14-17
[118]翟裕生.关于构造-流体-成矿作用研究的几个问题.地学前缘,1996,3(3-4): 230-236
[119].翟裕生.古大陆边缘构造演化和成矿系统.北京大学地质系主编,北京大学国际地质科学学术研讨会论文集,地震出版社,1998,769-778
[120]翟裕生.论成矿系统.地学前缘,1999,6(1):13-28
[121]翟裕生.矿田构造学概论.北京:冶金工业出版社,1984
[122]翟裕生,彭润民,邓军,等.成矿系统分析与新类型矿床预测.地学前缘, 2000, 7(1): 123-132
[123]翟裕生.区域构造、地球化学与成矿.地质调查与研究,2003,26(1):1-7
[124]翟裕生,邓军,彭润民.中国区域成矿若干问题探讨.矿床地质,1999(18):323-332
[125]翟国明,杨进辉,刘文军.胶东大型黄金矿集区及大规模成矿作用.中国科学(D辑),2001,31(7):545-552
[126]赵一鸣,吴良士,白鸽,等.中国主要金属矿床成矿规律.北京:地质出版社, 2004
[127]朱有光,蒋敬业.金矿地球化学找矿.武汉:中国地质大学出版社,1993
[128]张本仁.地球化学的基本观念与方法论.地球科学,1992,17(增刊):18-25
[129]张连昌,沈远超,李厚民,等.胶东地区金矿床流体包裹体的He、Ar同位素组成及成矿流体来源示踪.岩石学报,2002(18):559-565
[130]Chang T W, Choo C O. Faulting processes and K-Ar ages of fault gouges in the Yangsan Fault Zone. Journal of Earth Science of Korea, 1998, 20: 25-37
[131]Cheng Qiuming. Multifractal Theory and Geochemical Element Distribution Pattern. Earth Science, 2000, 25(3):311-318
[132]Deng Jun, Fang Yun, Wan Li et al. Fuzzy Comprehensive Appraisal of Concealed Ore Deposits. Journal of China University of Geosciences, 2000, 11(2):134-137
[133]Deng Jun, Fang Yun, Yang Liqiang et al. Numerical modeling of ore-forming dynamics of fractal dispersive fluid systrms. Acta Geologica Sinica. 2001,75(2):220-232
[134]Deng Jun, Huang Dinghua, Wang Qingfei. The Formation Mechanism of the“drag Depressions”and the Irregular Boundaries in Intraplate Deformation. Acta Geologica Sinica, 2004, 78(1): 267-272
[135]Deng Jun, Liu Wei, Sun Zhongshi et al. Evidence of mantle-rooted fluids and multi-level circulation ore-forming dynamics: A case study from the Xiadian gold deposit, Shandong province,China.Science in China(Series D),2003,46(Supp):138-142
[136]Deng Jun, Wang Qingfei, Huang Dinghua et al. Transport network and flow mechanism of shallow ore-bearing magma in Tongling ore cluster area. Science in China (Series D), 2006, 49 (4): 397-407
[137]Deng Jun, Wang Qingfei, Wei Yanguang et al. Metallogenic Effect of Transition of Tectonic Dynamic System, Journal of China University of Geosciences, 2004, 15(1): 23-28
[138]Deng Jun, Yang Liqiang, Chen Xueming et al. Fluid system and ore-forming dynamics of Yuebei basin, China. In:Mao J W and Bierlein F P, Editors. Mineral Deposit Research: Meeting the Global Challenge, Vol. 1. Berlin: Springer, 2005, 107-110
[139]Deng Jun, Yang Liqiang, Ge Liangsheng et al. Research Advances in the Mesozoic Tectonic Regimes during the Formation of Jiaodong Ore Cluster Area. Progress in Nature Sciences, 2006, 16(8): 777-784
[140].Deng Jun,Yang Liqiang,Sun Zhongshi et al. A metallogenic model of gold deposits of the Jiaodong granite-greenstone belt. Acta Geologica Sinica.2003,77(4):537-546
[141]Deng Jun,Yang Liqiang,Zhai Yusheng et al.Crust-mantle interaction and dynamics of metallogenic system of Jiaodong gold ore concentrating area, China. Journal of Geosciences of China, 1999, 1(1): 39-46
[142]Deng Jun, Zhai Yusheng, Wang Jingping et al. Shear Alteration, Mass Transfer and Gold Mineralization: An Example from Jiaodong Ore Deposit Concertrating Area, Shangdong, China. Journal of China University of Geosciences, 2000, 11(3):281-287
[143]Deng Jun, Fang Yun, Wan Li, et al. Fuzzy Comprehensive Appraisal of Concealed Ore Deposits. Journal of China University of Geosciences, 2000, 11(2),134-137
[144]D Thomas and P Ortoleva.Differentiated structures arising from mechano-chemical feedback in stressed rocks.Earth Science Reviews,1990,V.29,283-298
[145]Drummond B J,Goleby B R,Owen A J, et al. 2000.Seismic reflection imaging of mineral systems: Three case histories. Geophysics,65: 1852-1861
[146]Dirks P H,Wilson C J.Structural controls on the distribution of gold-bearing quartz vein in the Arltunga gold field,Northern Territory,Australia.Economic Geology,1991,86: 249-269
[147]Eion M. Cameron Derivation of gold by oxidative metamorphism of a deep ductile shear zones (part 2): evidence from the Bamble Belt, South Norway. Journal of Geochemical Exploration,1989,31:149-169
[148]Elder D,Cashman S M.Tectonic control and fluid evolution in the Quartz Hill, California,Lode Gold Deposits . Econology Geology , 1992 , 87 : 1795-1813
[149]Fan H R, Zhai M G, Xie Y H, et al. Ore-forming fluids associated with granite-hosted gold mineralization at the Sanshandao deposit, Jiaodong gold province, China. Miner. Dep, 2003, 38:739-750
[150]Fan Q C,Hooper P R. The Cenozoic basaltic rocks of Eastern China: petrology and chemical composition. Jouranl of Petrology,1991,32: 765-810
[151]Feng R,and Kerrich R.Archean geodynamics and the Abitibi—Pontiac collision: implications for advection of fluids at transpressive collisonal boundaries and the origin of giant vein systems.Earth—Science Reviews,1992,32:33-60
[152]Feng R and Kerrich R. Geochemical evolution of granitoids from the Archean Abitibi southern volcanic zone and the Pontiac subprovince,Superior province,Canada: Implication for tectonic history and source regions.Chemical Geology, 1992,98:23-70
[153]Goulty N.Controlled-source tomography formining and engineer ing application. In: Iyer H M and Hirahara K, eds. Seismic to mography: Theory and practice. London: Chapmanand Hall. 1993,797-813
[154]Gebre-Mariam M, Hagemann S G, Groves D I. A classification scheme for epigenetic Archaean lode-gold deposits. Miner. Deposita, 1995, 30:408-410
[155]Goldfarb G J, Groves D I, Gardoll S. Orogenic gold and geologic time: A global synthesis. Ore Geology Reviews, 2001, 18: 12-75
[156]Groves D I. The crustal continuum model for late-Archaean lode gold deposits of the Yilgarn Block, Western Australia . Mineralium Deposit, 1993, 28: 366-374
[157]Haynes D W, Cross K C, Bills R T, et al. Olympic Damore genesis: a fluid-mixing model. Economic Geology, 1995, 90: 281-307
[158]Hedenquist J W, Lowenstern J B. The role of magmas in the formation of hydrothermal ore deposits. Nature, 1994, 370: 519-527
[159]Kerrich R, Cassidy K F. Temporal relationships of lode-gold mineralization to accretion, magmatism, metamorphism and deformation, Archean to present: a review. Ore Geol. Rev., 1994, 9: 263-310
[160]Kerrich R, Wyman D. Geodynamic setting of mesothermal gold deposits: an association with accretionary tectonic regimes. Geology, 1990, 18: 882-885
[161]Landefeld L A.The geology of the Mother Lode-gold belt, Sierra Nevada Foot hills metamorphic belt, California. In: Bicentennial Gold 88, Extended Abstracts. Orl Programme. Geol. Soc. Aust. Abstr., 1988, 22: 167-172
[162]Loucks R R, and Mavrogenes J A. Gold solubility in supercritical hydrothermal brines measured in synthetic fluid inclusions. Science, 1999, 284: 2159-2163
[163]Sun X.X. and Deng J. Preliminary discussion on the grey characters of concealed form type of deposits and its grey forecasting and decision making. Japan Society of Geoinformatics(29th IGC Special Issue), 1993,V.4, No.3
[164]Wallace R E,Morris H T. Characteristic of fault and shear zone in deep mines.Pure Appl.Geophys, 1986,14(1/2)
[165]Wan T F. Zhu H. Proterozoic-Triassic in South China. J SE Asian Earth Sciences, 1991,6(2):147-157
[166]Wang Qingfei, Deng Jun, Yang Liqiang et al. Tectonic Constraints on the Transformation of Paleozoic Framework of Uplift and Depression in the Ordos Area. Acta Geologica Sinica, 2006, 80(6): 945-954
[167]Wang X H, Wen Z X, Huang Z.A. A Capital Asset Pricing Model under Stable Paretian Distributionin a Pure Exchang Economy. Acta Mathematiae Applicatae Sinica,English Series, 2004, 20(4):675-684
[168]Wang Z H, Lu H F. Ductile deformation and 40Ar/39Ar dating of the Changle- Nanaoductile shear zone, southeastern China. Journal of Structural. Geology, 2000, 22, 561-570
[169]White N C, Hedenquist J W. Epithermal gold deposits: styles, characteristics and exploration. Soc. Econ. Geol. Newslett, 1995, 23(1): 9-13
[170]Wyman D, Kerrich R. Alkaline magmatism, majors tructures, and gold deposits: implications for greenstone belt gold metallogeny. Econ. Geol., 1988, 83: 451-458
[171]Wan T. F. et al.,Formation and evolution of the Tancheng-Lujiang fault zone,China university of Geosciences press,1996
[172]Wan Tianfeng. Evolution of Tan cheng-Lujiang Wrench fault zone and paleostress fields. In:. Wan Tianfeng, Zhu Hong, Zhao Lei et al.(eds.). Formation and Evolution of Tan cheng-Lujiang Wrench Fault Zone. Wuhan: China University of Geosciences Press, 1996. 43-56
[173]Wedepohl, K.H.The composition of the continental crust. Geochemica et Cosmochimica Acta,1995,59:1217-1232
[174]X Xie,X Wang,L Xu, et al..Orientation study of strategic deep penetration geochemical methods in the central Kyzylkumdesert terrain,Uzbekistan. J. Geochem. Explor. 1999,66: 135-144
[175]Xu Jiawei. The Tancheng-Lujiang Wrench Fault System. New York: John Wiley&Sons Ltd,1993.300
[176]Xu J W, Zhu G, Tong W X, et al. Formation and evolution of the Tancheng-Lujiang wrench fault system: a major shear system to the northwest of the Pacific Ocean. Tectonophysics, 1987, 134:273-310
[177]Yang J H, Wu F Y, Wilde S A. A review of the geodynamic setting of large-scale Late Mesozoic gold mineralization in the North China Craton: an association with lithospheric thinning. Ore Geol. Rev., 2003, 23:123-152
[178]Yang Jinhui, Zhou Xinhua, Chen Lihui. Dating of gold mineralization for super-large altered tectonite-type gold deposits in Northwestern Jiaodong Peninsula and its implications for gold metallogeny. Acta Petrologica Sinica, 2000, 16(3):454-458
[179]Yang K H. Magmatic fluid and mineralization. Earth Science Frontiers, 1998, 5(3):7-36
[180]Yang Liqiang, Deng Jun, Wang Jianguo et al. Control of deep tectonics on the superlarge deposits in China. Acta Geologica Sinica, 2004,78(2):358-367
[181]Yang Liqiang, Deng Jun, Zhang Zhongjie, et al. Crust-mantle structure and coupling effects on mineralization: an example from Jiaodong Gold Ore Deposits Concentrating Area. China. Journal of China University of Geosciences, 2003, 14(1):42-51
[182]Yingqing Chen, Pengda Zhao, Jianguo Chen, et al. Application of The Geo-anomaly Unit Conceptin Quantitative Delineation and Assessment of Gold Ore Targets In Western Shandong Uplift Terrain, Eastern China. Natural Resources Research, 2001, 10 (1): 35-49
[183]Zhai Y,Deng J.Outline of the mineral resources of China and their tectonic setting. Australia Journal of Earth Sciences,1996,43(6): 673-685
[2]陈光远,邵伟,孙岱生.胶东金矿成因矿物学与找矿.重庆:重庆出版社,1989,1-45
[3]陈国华,刘连登,仲崇学.胶东金矿床的矿石地球化学研究.世界地质,1998,17(2):19-26
[4]陈毓川,李廷栋,彭齐鸣,等.矿产资源与可持续发展.北京:中国科学技术出版社, 1999,1-16
[5]陈毓川,李兆鼐,毋瑞身,等.中国金矿床及其成矿规律.北京:地质出版社, 2001
[6]邓军,高帮飞,王庆飞,等.成矿流体系统的形成与演化.地质科技情报,2005,24(1):50- 55
[7]邓军,杨立强,方云.成矿系统嵌套分形结构和自有序效应.地学前缘,2000,7(1): 133-146
[8]邓军,方云,杨立强,等.剪切蚀变与物质迁移及金的富集.地球科学,2000,25(1): 428-437
[9]邓军,吕古贤,杨立强,等.构造应力场转换与界面成矿.地球学报,1998,19(3):244-250
[10]邓军,孙忠实,王建平,等.动力系统转换与金成矿作用.矿床地质,2001,20(1): 71-77
[11]邓军,王庆飞,杨立强,等.胶东西北部金热液成矿系统内部结构解析.地球科学, 2005,30(1):102-108
[12]邓军,王庆飞,杨立强,等.胶西北金矿集成矿作用发生的地质背景.地学前缘, 2004,11(4):527-533
[13]邓军,徐守礼,方云,等.胶东西北部构造体系及金成矿动力学.北京:地质出版社. 1996
[14]邓军,徐守礼,吕古贤,等.胶东西北部断裂构造与成矿作用研究.现代地质,1996, 10(4):424-432
[15]邓军,杨立强,方云,等.胶东地区壳幔相互作用与金成矿效应.地质科学,2000, 35(1):60-70
[16]邓军,杨立强,葛良胜,等.胶东矿集区形成的构造体制研究进展.自然科学进展, 2006,16(5):513-518
[17]邓军,杨立强,孙忠实,等.构造体制转换与流体多层循环成矿动力学.地球科学, 2000,25(4):397-403
[18]邓军,杨立强,孙忠实,等.矿源系统地质-地球化学例析.现代地质,2000,25(1):165- 172
[19]邓军,杨立强,翟裕生,等.构造-流体-成矿系统及其动力学的理论格架与方法体系.地球科学,2000,25(1):71-78
[20]邓军,杨立强,翟裕生,等.地质体元素组合与矿源系统组成及演化.地球学报, 1999,20(增刊):414-419
[21]邓军,杨立强,翟裕生,等.胶东招掖矿集区巨量金质来源和流体成矿效应.地质科,2001,36(3):257-268
[22]邓军,翟裕生,杨立强,等.论剪切带构造成矿系统,现代地质,1998,12(4):493-500
[23]邓军,翟裕生,杨立强,等.构造演化与成矿系统动力学-以胶东金矿集中区为例.地学前缘,1999,6(2):315-323
[24]邓军,翟裕生,杨立强,等.剪切带构造-流体-成矿系统动力学模拟.地学前缘,1999,6(1),115-129
[25]邓军,房天文,杨立强,等.山东省招远市大尹格庄金矿床多元构造体制叠接与4D矿化网络研究.科研报告,2005
[26]邓军,王庆飞,杨立强,等.胶东西北部金热液成矿系统内部结构解析,地球科学, 2005,30(1):102-108
[27]丁式江,翟裕生,邓军.胶东地区地质体含金性的地质地球化学评价.地质找矿论丛,1997,12(3):1-9
[28]杜杨松,壳幔成矿学初探.矿床地质,1999,18(4):341-346
[29]范永香,胡家杰,卢作祥,等.山东招(远)-平(度)断裂构造南段上庄地区构造控矿规律研究.中国地质大学(武汉),黄金研究所,1991
[30]范永香,阳正熙.成矿规律与成矿预测.徐州:中国矿业大学出版社, 2003
[31]郭光裕.脉状金矿床深部大比例尺统计预测.武汉:中国地质大学出版社, 1989
[32]郭涛.胶西北金矿区域成矿系统及其构造-流体-矿化研究.中国地质大学(北京), 2008年博士学位论文
[33]高帮飞.山东招平金矿带构造-流体耦合成矿动力学.中国地质大学(北京),2008年博士学位论文
[34]高秋斌,范永香,王可勇,等.金矿床深部成矿预测的主要途径.黄金地质,1998,4(2):21-26
[35]高占林,林尔为.金厂峪金矿有关岩石金丰度的研究.长春地质学院学报, 1987,17 (1):23-32
[36]胡受奚,王鹤年,王德滋,等.中国东部金矿地质学及地球化学.科学出版社,1998
[37]韩润生,陈进,高德荣,等.构造地球化学在隐伏矿定位预测中的应用.地质与勘探, 2003,39(6):25-29
[38]黎彤,倪守斌.地球化学讲义.广州:冶金工业部广东冶金地质勘探公司,1982
[39]李惠,郑涛,汤磊,等.山东招远大尹格庄金矿床隐伏矿定位预测的叠加晕模式.有色金属矿产与勘查,1998,7(3):178-185
[40]李惠,张文华,常凤池,等.大型、特大型金矿盲矿预测的原生叠加晕模型.北京:冶金工业出版社,1998,84-95,114-119
[41]李惠,张文华.胶东大型金矿床的地球化学分带特征.贵金属地质,1999,8(4),217-222
[42]李惠,张文华.胶东大型金矿床的地球化学分带特征.贵金属地质,1999,8(4): 217-222
[43]李四光.地质力学概论.北京:科学出版社,1973
[44]李士先,刘长春,安郁宏,等.胶东金矿地质.北京:地质出版社, 2007
[45]李卫革,李龙义,张瑞忠,等.胶东大尹格庄金矿床地质特征与深部资源前景.地质力学学报,2003,9(3):254-260
[46]李晓英.招远地区金矿找矿若干问题浅析.山东招金集团公司矿山地质论文集,地震出版社,2001,20-31
[47]李俊建,沈保丰.华北地台主要花岗岩-绿岩带含金丰度值的研究.前寒武纪研究进展, 1997, 20(4), 25-33
[48]李兆龙,杨敏之,李治平,等.胶东金矿床地质地球化学.天津:天津科学技术出版社,1993
[49]李金祥.胶东西北部招平断裂带构造特征与成矿.中国地质大学(北京)博士论文,2005
[50]林文蔚,赵一鸣,徐钰.胶东招远-平度断裂活动性质及活动时代.中国区域地质,2000,19(1),43-50
[51]凌洪飞,胡受奚,孙景贵,等.胶东金青顶和大尹格庄金矿床花岗质围岩的蚀变地球化学研究.矿床地质, 2002,21(2):187-199
[52]刘玉强,李洪喜,黄太岭,等.山东省金、铁、煤矿床成矿系列及成矿预测.地质出版社,2004
[53]刘光智.胶东地区岩浆岩与金-多金属矿的关系.黄金,2003,24(11):12-16
[54]卢焕章,Guha J,方根保.山东玲珑金矿的成矿流体特征.地球化学,1999,28(5): 421-437
[55]卢作祥,范永香,刘石年.山东玲珑金矿田断裂构造控矿作用探讨.地球科学-武汉地质学院学报,1983,(3),127-138
[56]吕古贤,林文蔚,罗元华,等.构造物理化学与金成矿预测.北京:地质出版社,1999
[57]吕古贤,杨敏之.胶东玲珑-焦家式金矿地质.北京:科学出版社,1993
[58]吕古贤,韦昌山,郭涛,等.胶东矿集区金矿成矿地质事件研究初探.黄金地质,2004, 10(2):1-6
[59]罗镇宽,苗来成.胶东招莱地区花岗岩和金矿床.北京:冶金工业出版社,2002
[60]罗镇宽,关康,余和勇,等.胶东招莱地区大-超大型金矿床形成的几个关键因素.地质找矿论丛,2003,18(2):95-102
[61]罗镇宽,关康,苗来成.胶东玲珑金矿田煌斑岩脉与成矿关系的讨论.黄金地质, 2001, 7(4):15-20
[62]苗来成,罗镇宽,黄佳展.山东招掖金矿带内花岗岩类侵入体锆石SHRIMP研究及其意义.中国科学,1997,27(3): 207-213
[63]苗来成,朱成伟,翟裕生,等.山东招掖金矿带内花岗岩与金矿化关系探讨,黄金地质,1999,5(4),7-10
[64]山东省地质六队.大尹格庄金矿床勘探地质报告.1993 (内部资料)
[65]山东招金集团公司.招远金矿集中区地质与找矿.北京:地震出版社,2002
[66]申玉科,邓军,徐叶兵.煌斑岩在玲珑金矿田形成过程中的地质意义.地质与勘探,2005,41(3):45-49
[67]沈昆,胡受奚,孙景贵,等.山东招远大尹格庄金矿成矿流体特征.岩石学报, 2000.16(4):542-551
[68]沈远超,曾庆栋,刘铁兵,等.郯庐断裂与金矿成矿.世界地质,2003,22(1):41-44
[69]申萍,沈远超,李光明,等.胶东金牛山金矿区深部地球化学特征及成矿预测.地质与勘探, 2003,39(4):21-26
[70]孙丰月.胶东地区中新生代区域构造演化与成矿.长春地质学院学报,1994(24),378-422
[71]孙殿卿,高庆华.隐伏矿床预测.北京:地质出版社,1987
[72]孙国胜,姚风良,胡瑞忠,等.玲珑金矿田矿体富集规律及其控制因素.大地构造与成矿学,2001, 25(4), 464-470
[73]孙国胜,刘颖,李绪俊,等.玲珑金矿田不同级别构造控矿特征.地质地球化学,2003,31(2):18-24
[74]孙国胜,李绪俊,姚风良,等.玲珑金矿田矿物组合与地球化学分带及矿体定位预测意义.地质与勘探,2002,38(4):28-31
[75]孙林,马学欣.招远地区北西向断裂构造控矿浅析.山东招金集团公司矿山地质论文集,地震出版社,2001,33-37
[76]涂光炽等.中国超大型矿床.北京:科学出版社,2000,1-583
[77]王建平,戚开静,杨立强.中国金矿床发现的启示.地质找矿论丛,2001,16(2): 104-107
[78]王义文,朱奉三,宫润潭.胶东金矿集中区金矿成矿年代学研究.黄金地质,2002,8(4): 48-55
[79]王义文,朱奉三,宫润谭.构造同位素地球化学-胶东金矿集中区硫同位素再研究.黄金,2002(23):1-16
[80]王世称,杨毅恒,严光生,等.大型、超大型金矿床密集区综合信息预测.北京:地质出版社,,2001,21-28
[81]王世称,刘玉强,伊丕厚,等.山东省金矿床及金矿床密集区综合信息成矿预测.北京:地质出版社, 2003
[82]王希今,鲍亚凡,李永胜.玲珑金矿田两种矿化类型元素空间分带性研究.黄金地质,2007(8):20-23
[83]吴淦国.矿田构造与成矿预测.地质力学学报,1998,4(2):1-4
[84]徐兵.中国山东半岛大尹格庄金矿床的地质与地球化学特征.东京大学博士论文,1999,1-139
[85]徐述平,朱洪岭,张华全.胶东大磨曲家金矿控矿断裂及成矿规律.黄金科学技术, 2006,12(2):11-22
[86]徐述平,邓军,高帮飞,等.胶东山后金矿床地质体微量元素特征及找矿意义.地质与勘探,2008 (5): 23-29
[87]徐贵忠,周瑞,王艺芬,等.胶东和鲁西地区中生代成矿作用重大差异性的内在因素.现代地质,2002, 16(1):9-16
[88]徐金方,沈步云,牛良柱,等.胶北地块与金矿有关的花岗岩类的研究.山东地质,1989, 5(2): 1-22
[89]徐刚,郑达兴,温长顺.胶东焦家断裂带与金矿的成生关系.地质力学学报,1998(4):53-58
[90]杨金中,李光明.胶东中生代两期金矿化作用的对比研究及其意义.地质与勘探, 2001,37(1):33-37
[91]杨金中,沈远超,刘铁兵.大型-超大型金矿密集区的形成条件.地质与勘探, 2001,37(1):30-33
[92]杨进辉,朱美妃,刘伟,等.胶东地区郭家岭花岗闪长岩的地球化学特征及成因.岩石学报, 2003,19(4): 692-700
[93]杨锋,刘连登,陈国华.平度1号脉金矿晚期叠加成矿初探.黄金,2001,22(5):1-5
[94]杨立强,邓军,方云,等.构造-流体成矿效应计算模拟.地球学报,1999,20(增刊): 433-437
[95]杨立强,邓军,葛良胜,等.胶东金矿成矿时代和矿床成因研究述评.自然科学进展, 2006,16(7): 797-802
[96]杨立强,邓军,王庆飞,等.深部构造与地质过程控矿研究.矿床地质,2006,25(增刊): 107-110
[97]杨立强,邓军,翟裕生.构造-流体-成矿系统及其动力学.地学前缘,2000,7(1):178
[98]杨立强,邓军,翟裕生,等.胶东夏甸金矿地球化学场结构.现代地质,2001,15(4): 409-413
[99]杨立强,邓军,张中杰,等.构造应力场转换的成矿地球化学响应.大地构造与成矿学,2003,27 (3):243-249
[100]杨立强,张中杰,邓军.深浅构造耦合成矿效应-以胶东招掖金矿带为例.地学前缘, 2004,11(1):56
[101]杨立强,张中杰,王光杰,等.胶东金矿集中区岩石圈结构与深部成矿作用.地球科学,2000, 25(4): 421-427
[102]杨忠芳,徐景奎,赵伦山,等.胶东区域地壳演化与金成矿作用地球化学.北京:地质出版社, 1998
[103]杨敏之,吕古贤.胶东绿岩带型金矿地质地球化学.北京:地质出版社,1996
[104]杨敏之.金矿床围岩蚀变带地球化学-以胶东金矿床为例.北京:地质出版社,1998
[105]杨进辉,周新华,陈立辉.胶东地区破碎带蚀变岩型金矿时代的测定及其地质意义.岩石学报,2000,16(03):454-458
[106]姚凤良,刘连登,孔庆存,等.胶东西北部脉状金矿长春.吉林科学技术出版社,1990
[107].於崇文.成矿动力系统在混沌边缘分形生长—一种新的成矿理论与方法论(上).地学前缘,2001,(06): 28-34
[108]於崇文.成矿作用动力学.北京:地质出版社,1998
[109]於崇文.大型矿床和成矿区(带)在混沌边缘.地学前缘,1999,6(1):85-101
[110]翟裕生,邓军,崔彬,等.成矿系统及综合地质异常.现代地质,1999,13(1):99-104
[111]翟裕生,邓军,李晓波.区域成矿学.北京:地质出版社,1999
[112]翟裕生,邓军,汤中立,等.古陆边缘成矿系统.北京:地质出版社,2002,1-416
[113]翟裕生,邓军,王建平,等.深部找矿研究问题.矿床地质,2004,23(2):143-149
[114]翟裕生,邓军,杨立强,等.山东夏甸金矿及其外围隐伏矿体定位预测.地学前缘, 1999,6(2):230
[115]翟裕生,吕古贤.构造动力体制转换与成矿作用.地球学报,2002,23(2):97-102
[116]翟裕生,张湖,宋鸿林,等.大型构造与超大型矿床.北京:地质出版社,1997
[117]翟裕生. 21世纪矿床学研究展望.中国地质,2000,(3): 14-17
[118]翟裕生.关于构造-流体-成矿作用研究的几个问题.地学前缘,1996,3(3-4): 230-236
[119].翟裕生.古大陆边缘构造演化和成矿系统.北京大学地质系主编,北京大学国际地质科学学术研讨会论文集,地震出版社,1998,769-778
[120]翟裕生.论成矿系统.地学前缘,1999,6(1):13-28
[121]翟裕生.矿田构造学概论.北京:冶金工业出版社,1984
[122]翟裕生,彭润民,邓军,等.成矿系统分析与新类型矿床预测.地学前缘, 2000, 7(1): 123-132
[123]翟裕生.区域构造、地球化学与成矿.地质调查与研究,2003,26(1):1-7
[124]翟裕生,邓军,彭润民.中国区域成矿若干问题探讨.矿床地质,1999(18):323-332
[125]翟国明,杨进辉,刘文军.胶东大型黄金矿集区及大规模成矿作用.中国科学(D辑),2001,31(7):545-552
[126]赵一鸣,吴良士,白鸽,等.中国主要金属矿床成矿规律.北京:地质出版社, 2004
[127]朱有光,蒋敬业.金矿地球化学找矿.武汉:中国地质大学出版社,1993
[128]张本仁.地球化学的基本观念与方法论.地球科学,1992,17(增刊):18-25
[129]张连昌,沈远超,李厚民,等.胶东地区金矿床流体包裹体的He、Ar同位素组成及成矿流体来源示踪.岩石学报,2002(18):559-565
[130]Chang T W, Choo C O. Faulting processes and K-Ar ages of fault gouges in the Yangsan Fault Zone. Journal of Earth Science of Korea, 1998, 20: 25-37
[131]Cheng Qiuming. Multifractal Theory and Geochemical Element Distribution Pattern. Earth Science, 2000, 25(3):311-318
[132]Deng Jun, Fang Yun, Wan Li et al. Fuzzy Comprehensive Appraisal of Concealed Ore Deposits. Journal of China University of Geosciences, 2000, 11(2):134-137
[133]Deng Jun, Fang Yun, Yang Liqiang et al. Numerical modeling of ore-forming dynamics of fractal dispersive fluid systrms. Acta Geologica Sinica. 2001,75(2):220-232
[134]Deng Jun, Huang Dinghua, Wang Qingfei. The Formation Mechanism of the“drag Depressions”and the Irregular Boundaries in Intraplate Deformation. Acta Geologica Sinica, 2004, 78(1): 267-272
[135]Deng Jun, Liu Wei, Sun Zhongshi et al. Evidence of mantle-rooted fluids and multi-level circulation ore-forming dynamics: A case study from the Xiadian gold deposit, Shandong province,China.Science in China(Series D),2003,46(Supp):138-142
[136]Deng Jun, Wang Qingfei, Huang Dinghua et al. Transport network and flow mechanism of shallow ore-bearing magma in Tongling ore cluster area. Science in China (Series D), 2006, 49 (4): 397-407
[137]Deng Jun, Wang Qingfei, Wei Yanguang et al. Metallogenic Effect of Transition of Tectonic Dynamic System, Journal of China University of Geosciences, 2004, 15(1): 23-28
[138]Deng Jun, Yang Liqiang, Chen Xueming et al. Fluid system and ore-forming dynamics of Yuebei basin, China. In:Mao J W and Bierlein F P, Editors. Mineral Deposit Research: Meeting the Global Challenge, Vol. 1. Berlin: Springer, 2005, 107-110
[139]Deng Jun, Yang Liqiang, Ge Liangsheng et al. Research Advances in the Mesozoic Tectonic Regimes during the Formation of Jiaodong Ore Cluster Area. Progress in Nature Sciences, 2006, 16(8): 777-784
[140].Deng Jun,Yang Liqiang,Sun Zhongshi et al. A metallogenic model of gold deposits of the Jiaodong granite-greenstone belt. Acta Geologica Sinica.2003,77(4):537-546
[141]Deng Jun,Yang Liqiang,Zhai Yusheng et al.Crust-mantle interaction and dynamics of metallogenic system of Jiaodong gold ore concentrating area, China. Journal of Geosciences of China, 1999, 1(1): 39-46
[142]Deng Jun, Zhai Yusheng, Wang Jingping et al. Shear Alteration, Mass Transfer and Gold Mineralization: An Example from Jiaodong Ore Deposit Concertrating Area, Shangdong, China. Journal of China University of Geosciences, 2000, 11(3):281-287
[143]Deng Jun, Fang Yun, Wan Li, et al. Fuzzy Comprehensive Appraisal of Concealed Ore Deposits. Journal of China University of Geosciences, 2000, 11(2),134-137
[144]D Thomas and P Ortoleva.Differentiated structures arising from mechano-chemical feedback in stressed rocks.Earth Science Reviews,1990,V.29,283-298
[145]Drummond B J,Goleby B R,Owen A J, et al. 2000.Seismic reflection imaging of mineral systems: Three case histories. Geophysics,65: 1852-1861
[146]Dirks P H,Wilson C J.Structural controls on the distribution of gold-bearing quartz vein in the Arltunga gold field,Northern Territory,Australia.Economic Geology,1991,86: 249-269
[147]Eion M. Cameron Derivation of gold by oxidative metamorphism of a deep ductile shear zones (part 2): evidence from the Bamble Belt, South Norway. Journal of Geochemical Exploration,1989,31:149-169
[148]Elder D,Cashman S M.Tectonic control and fluid evolution in the Quartz Hill, California,Lode Gold Deposits . Econology Geology , 1992 , 87 : 1795-1813
[149]Fan H R, Zhai M G, Xie Y H, et al. Ore-forming fluids associated with granite-hosted gold mineralization at the Sanshandao deposit, Jiaodong gold province, China. Miner. Dep, 2003, 38:739-750
[150]Fan Q C,Hooper P R. The Cenozoic basaltic rocks of Eastern China: petrology and chemical composition. Jouranl of Petrology,1991,32: 765-810
[151]Feng R,and Kerrich R.Archean geodynamics and the Abitibi—Pontiac collision: implications for advection of fluids at transpressive collisonal boundaries and the origin of giant vein systems.Earth—Science Reviews,1992,32:33-60
[152]Feng R and Kerrich R. Geochemical evolution of granitoids from the Archean Abitibi southern volcanic zone and the Pontiac subprovince,Superior province,Canada: Implication for tectonic history and source regions.Chemical Geology, 1992,98:23-70
[153]Goulty N.Controlled-source tomography formining and engineer ing application. In: Iyer H M and Hirahara K, eds. Seismic to mography: Theory and practice. London: Chapmanand Hall. 1993,797-813
[154]Gebre-Mariam M, Hagemann S G, Groves D I. A classification scheme for epigenetic Archaean lode-gold deposits. Miner. Deposita, 1995, 30:408-410
[155]Goldfarb G J, Groves D I, Gardoll S. Orogenic gold and geologic time: A global synthesis. Ore Geology Reviews, 2001, 18: 12-75
[156]Groves D I. The crustal continuum model for late-Archaean lode gold deposits of the Yilgarn Block, Western Australia . Mineralium Deposit, 1993, 28: 366-374
[157]Haynes D W, Cross K C, Bills R T, et al. Olympic Damore genesis: a fluid-mixing model. Economic Geology, 1995, 90: 281-307
[158]Hedenquist J W, Lowenstern J B. The role of magmas in the formation of hydrothermal ore deposits. Nature, 1994, 370: 519-527
[159]Kerrich R, Cassidy K F. Temporal relationships of lode-gold mineralization to accretion, magmatism, metamorphism and deformation, Archean to present: a review. Ore Geol. Rev., 1994, 9: 263-310
[160]Kerrich R, Wyman D. Geodynamic setting of mesothermal gold deposits: an association with accretionary tectonic regimes. Geology, 1990, 18: 882-885
[161]Landefeld L A.The geology of the Mother Lode-gold belt, Sierra Nevada Foot hills metamorphic belt, California. In: Bicentennial Gold 88, Extended Abstracts. Orl Programme. Geol. Soc. Aust. Abstr., 1988, 22: 167-172
[162]Loucks R R, and Mavrogenes J A. Gold solubility in supercritical hydrothermal brines measured in synthetic fluid inclusions. Science, 1999, 284: 2159-2163
[163]Sun X.X. and Deng J. Preliminary discussion on the grey characters of concealed form type of deposits and its grey forecasting and decision making. Japan Society of Geoinformatics(29th IGC Special Issue), 1993,V.4, No.3
[164]Wallace R E,Morris H T. Characteristic of fault and shear zone in deep mines.Pure Appl.Geophys, 1986,14(1/2)
[165]Wan T F. Zhu H. Proterozoic-Triassic in South China. J SE Asian Earth Sciences, 1991,6(2):147-157
[166]Wang Qingfei, Deng Jun, Yang Liqiang et al. Tectonic Constraints on the Transformation of Paleozoic Framework of Uplift and Depression in the Ordos Area. Acta Geologica Sinica, 2006, 80(6): 945-954
[167]Wang X H, Wen Z X, Huang Z.A. A Capital Asset Pricing Model under Stable Paretian Distributionin a Pure Exchang Economy. Acta Mathematiae Applicatae Sinica,English Series, 2004, 20(4):675-684
[168]Wang Z H, Lu H F. Ductile deformation and 40Ar/39Ar dating of the Changle- Nanaoductile shear zone, southeastern China. Journal of Structural. Geology, 2000, 22, 561-570
[169]White N C, Hedenquist J W. Epithermal gold deposits: styles, characteristics and exploration. Soc. Econ. Geol. Newslett, 1995, 23(1): 9-13
[170]Wyman D, Kerrich R. Alkaline magmatism, majors tructures, and gold deposits: implications for greenstone belt gold metallogeny. Econ. Geol., 1988, 83: 451-458
[171]Wan T. F. et al.,Formation and evolution of the Tancheng-Lujiang fault zone,China university of Geosciences press,1996
[172]Wan Tianfeng. Evolution of Tan cheng-Lujiang Wrench fault zone and paleostress fields. In:. Wan Tianfeng, Zhu Hong, Zhao Lei et al.(eds.). Formation and Evolution of Tan cheng-Lujiang Wrench Fault Zone. Wuhan: China University of Geosciences Press, 1996. 43-56
[173]Wedepohl, K.H.The composition of the continental crust. Geochemica et Cosmochimica Acta,1995,59:1217-1232
[174]X Xie,X Wang,L Xu, et al..Orientation study of strategic deep penetration geochemical methods in the central Kyzylkumdesert terrain,Uzbekistan. J. Geochem. Explor. 1999,66: 135-144
[175]Xu Jiawei. The Tancheng-Lujiang Wrench Fault System. New York: John Wiley&Sons Ltd,1993.300
[176]Xu J W, Zhu G, Tong W X, et al. Formation and evolution of the Tancheng-Lujiang wrench fault system: a major shear system to the northwest of the Pacific Ocean. Tectonophysics, 1987, 134:273-310
[177]Yang J H, Wu F Y, Wilde S A. A review of the geodynamic setting of large-scale Late Mesozoic gold mineralization in the North China Craton: an association with lithospheric thinning. Ore Geol. Rev., 2003, 23:123-152
[178]Yang Jinhui, Zhou Xinhua, Chen Lihui. Dating of gold mineralization for super-large altered tectonite-type gold deposits in Northwestern Jiaodong Peninsula and its implications for gold metallogeny. Acta Petrologica Sinica, 2000, 16(3):454-458
[179]Yang K H. Magmatic fluid and mineralization. Earth Science Frontiers, 1998, 5(3):7-36
[180]Yang Liqiang, Deng Jun, Wang Jianguo et al. Control of deep tectonics on the superlarge deposits in China. Acta Geologica Sinica, 2004,78(2):358-367
[181]Yang Liqiang, Deng Jun, Zhang Zhongjie, et al. Crust-mantle structure and coupling effects on mineralization: an example from Jiaodong Gold Ore Deposits Concentrating Area. China. Journal of China University of Geosciences, 2003, 14(1):42-51
[182]Yingqing Chen, Pengda Zhao, Jianguo Chen, et al. Application of The Geo-anomaly Unit Conceptin Quantitative Delineation and Assessment of Gold Ore Targets In Western Shandong Uplift Terrain, Eastern China. Natural Resources Research, 2001, 10 (1): 35-49
[183]Zhai Y,Deng J.Outline of the mineral resources of China and their tectonic setting. Australia Journal of Earth Sciences,1996,43(6): 673-685