胶东新城金矿床构造—蚀变—矿化网络结构
|
摘要
新城金矿床是胶东焦家金矿田内的超大型焦家式金矿床。论文以详细的矿床地质调查为基础,对该金矿床控矿构造、蚀变分带及矿化网络结构进行了研究。
焦家主断裂及其次级断裂构造是金矿床最重要的控矿因素,直接控制了矿体的形成及分布。由于区域构造应力场的长期演化,这些断裂构造经历了多期次构造活动:成矿前韧性剪切活动、成矿早期压性韧-脆性剪切活动、成矿期压剪性构造活动及张剪性构造活动、成矿后张性构活动五个时期。
围岩蚀变受断裂构造控制,水平方向具明显的分带性,但并非简单的线性分带特征。在焦家断裂带下盘,自主断裂面向外,蚀变岩有一定渐变趋势:断层泥→黄铁绢英岩→绢英岩→绢英岩化花岗岩→硅化-钾化花岗岩→新鲜花岗岩(-630m以上为黑云母花岗岩、-630m以下为花岗闪长岩)。运用质量平衡计算方法对围岩热液蚀变过程中元素质量迁移进行了研究。从新鲜花岗岩到各种蚀变岩过程中:Si、Na、Al元素主要为迁出,Fe元素主要为迁入,Ca、K元素既有迁入也有迁出;微量元素Ba、Pb、Zn、Sr表现活跃,其次为Cu和Rb。其中Ba、Sr多为迁出,Pb、Zn及Cu多为迁入。
新城金矿床黄铁绢英岩型矿化(Ⅰ号矿体)和含金石英脉型矿化(Ⅴ号矿体)是同源成矿溶液在同一构造作用下不同构造(断裂带)部位的产物,是由于控矿构造的部位不同、级序高低、性质差异所造成的:缓倾斜压扭性主控断裂中构造活动强烈,岩石破碎强烈,流体以渗透交代作用为主,发育蚀变岩型矿化;焦家主断裂下盘远离主断裂的次级构造以张扭性为主,成矿流体以充填为主,利于成矿矿物质沉淀而形成硫化物石英脉型矿体。
焦家断裂构造分带与蚀变矿化分带有良好的吻合性和统一性,呈水平分带为主的空间分带性。从主断裂面近旁的挤压片理带至远离断面的节理带,其蚀变岩亦由黄铁绢英岩化带至远离断面的钾化带,矿化类型也出现由破碎蚀变岩型矿化带至石英脉型矿化带变化。
Xincheng gold deposit is one of the largest gold deposits, which is“Jiaojia Type”gold deposit in the Jiaojia gold field of Jiaodong Peninsula. Based on the detailed field geological survey, characteristics of ore-controlling structures, alteration belt as well as the mineralization network were studied in this paper.
The Jiaojia fault and its secondary structures are the most important ore-controlling factors of Xincheng gold deposit, which directly controlled the formation and distribution of the deposit. Owing to long-term evolution of regional tectonic stress field, the Jiaojia main fault and its secondary structures experienced multistage structure-activity: ductile shearing activity before the ore-forming stage, compression-ductile-brittle shearing activity before the ore-forming stage, compression-shearing and stretching-shearing activity of ore-forming stage, stretching activity after ore-forming stage.
Wall rock alteration of Xincheng gold deposit, controlled by fault, has a clear belt, which is not simply linear, however. From the footwall of major fracture planes to the external, altered rocks present a gradual change trend: from fault gouge, through beresitization belt, sericite-quartz alteration belt, granite of sericite-quartz belt and alteration silicified-potassic granitic belt, to fresh granite (biotite granite exists up -630 m while granodiorite exists below -630 m). By the method of mass balance calculation, the migration of the elements in the process of wall rock alteration, which means fresh granite altered to altered rocks, was studied. The result of study shows that the moving out elements are mainly Si, Na and Al, the immigration elements are mainly Fe, and both cases present in elements of Ca and K; trace elements of Ba, Pb, Zn, Sr are active, and secondly are Cu and Rb, of which, Ba and Sr always move out and Pb, Zn and Cu mostly move in.
The beresitization mineralization of Xincheng gold deposit (No.I orebody) and Au-bearing quartz vein-type mineralization are the production of the same ore- forming fluids under the same tectonic activity but different structural site, which were caused by ore-controlling structure of different parts, level of sequence and property. Tectonic activity in the main slightly inclined fault with shear- compressional mechanical property, act intensively with strong fragment of rocks, and the ore-forming fluids characterized with infiltration metasomatism, with altered rock-type mineralization while in the secondary structure with the tenso-shear property which is the footwall of Jiaojia fault, far away from the main fault, the ore-forming fluids characterized with the ore-forming process of filling which was favorable for the precipitation for ore-forming mineral and forming sulfide quartz vein type ore bodies.
The structure belt of Jiaojia faults coincide with the belt of alteration mineralization and the mineralization type presents as domimated horizontal belt. The alterated rocks changed from beresitization belt into potassic belt with compressional schistosity belt near the fault plane to the fissuring belt far from fault plane, and the mineralization types are changed from fractured altered rock type into Au-bearing quartz vein-type mineralization.
焦家主断裂及其次级断裂构造是金矿床最重要的控矿因素,直接控制了矿体的形成及分布。由于区域构造应力场的长期演化,这些断裂构造经历了多期次构造活动:成矿前韧性剪切活动、成矿早期压性韧-脆性剪切活动、成矿期压剪性构造活动及张剪性构造活动、成矿后张性构活动五个时期。
围岩蚀变受断裂构造控制,水平方向具明显的分带性,但并非简单的线性分带特征。在焦家断裂带下盘,自主断裂面向外,蚀变岩有一定渐变趋势:断层泥→黄铁绢英岩→绢英岩→绢英岩化花岗岩→硅化-钾化花岗岩→新鲜花岗岩(-630m以上为黑云母花岗岩、-630m以下为花岗闪长岩)。运用质量平衡计算方法对围岩热液蚀变过程中元素质量迁移进行了研究。从新鲜花岗岩到各种蚀变岩过程中:Si、Na、Al元素主要为迁出,Fe元素主要为迁入,Ca、K元素既有迁入也有迁出;微量元素Ba、Pb、Zn、Sr表现活跃,其次为Cu和Rb。其中Ba、Sr多为迁出,Pb、Zn及Cu多为迁入。
新城金矿床黄铁绢英岩型矿化(Ⅰ号矿体)和含金石英脉型矿化(Ⅴ号矿体)是同源成矿溶液在同一构造作用下不同构造(断裂带)部位的产物,是由于控矿构造的部位不同、级序高低、性质差异所造成的:缓倾斜压扭性主控断裂中构造活动强烈,岩石破碎强烈,流体以渗透交代作用为主,发育蚀变岩型矿化;焦家主断裂下盘远离主断裂的次级构造以张扭性为主,成矿流体以充填为主,利于成矿矿物质沉淀而形成硫化物石英脉型矿体。
焦家断裂构造分带与蚀变矿化分带有良好的吻合性和统一性,呈水平分带为主的空间分带性。从主断裂面近旁的挤压片理带至远离断面的节理带,其蚀变岩亦由黄铁绢英岩化带至远离断面的钾化带,矿化类型也出现由破碎蚀变岩型矿化带至石英脉型矿化带变化。
Xincheng gold deposit is one of the largest gold deposits, which is“Jiaojia Type”gold deposit in the Jiaojia gold field of Jiaodong Peninsula. Based on the detailed field geological survey, characteristics of ore-controlling structures, alteration belt as well as the mineralization network were studied in this paper.
The Jiaojia fault and its secondary structures are the most important ore-controlling factors of Xincheng gold deposit, which directly controlled the formation and distribution of the deposit. Owing to long-term evolution of regional tectonic stress field, the Jiaojia main fault and its secondary structures experienced multistage structure-activity: ductile shearing activity before the ore-forming stage, compression-ductile-brittle shearing activity before the ore-forming stage, compression-shearing and stretching-shearing activity of ore-forming stage, stretching activity after ore-forming stage.
Wall rock alteration of Xincheng gold deposit, controlled by fault, has a clear belt, which is not simply linear, however. From the footwall of major fracture planes to the external, altered rocks present a gradual change trend: from fault gouge, through beresitization belt, sericite-quartz alteration belt, granite of sericite-quartz belt and alteration silicified-potassic granitic belt, to fresh granite (biotite granite exists up -630 m while granodiorite exists below -630 m). By the method of mass balance calculation, the migration of the elements in the process of wall rock alteration, which means fresh granite altered to altered rocks, was studied. The result of study shows that the moving out elements are mainly Si, Na and Al, the immigration elements are mainly Fe, and both cases present in elements of Ca and K; trace elements of Ba, Pb, Zn, Sr are active, and secondly are Cu and Rb, of which, Ba and Sr always move out and Pb, Zn and Cu mostly move in.
The beresitization mineralization of Xincheng gold deposit (No.I orebody) and Au-bearing quartz vein-type mineralization are the production of the same ore- forming fluids under the same tectonic activity but different structural site, which were caused by ore-controlling structure of different parts, level of sequence and property. Tectonic activity in the main slightly inclined fault with shear- compressional mechanical property, act intensively with strong fragment of rocks, and the ore-forming fluids characterized with infiltration metasomatism, with altered rock-type mineralization while in the secondary structure with the tenso-shear property which is the footwall of Jiaojia fault, far away from the main fault, the ore-forming fluids characterized with the ore-forming process of filling which was favorable for the precipitation for ore-forming mineral and forming sulfide quartz vein type ore bodies.
The structure belt of Jiaojia faults coincide with the belt of alteration mineralization and the mineralization type presents as domimated horizontal belt. The alterated rocks changed from beresitization belt into potassic belt with compressional schistosity belt near the fault plane to the fissuring belt far from fault plane, and the mineralization types are changed from fractured altered rock type into Au-bearing quartz vein-type mineralization.
引文
Ague J J. Evidence for major mass Transfer and volume strain during regional metamorphism of pelites.Geology.1991, 19:855-858
Ague J J. Mass-transfer during barrovian metamorphism of pelites, south-central Connecticut. 1. Evidence for changes in composition and volume. American Journal of Science.1994, 294.989-1057
Ague J J. Mass-transfer during barrovian metamorphism of pelites, south-central Connecticut. 2. Channelized fluid-flow and the growth of staurolite and kyanite. American Journal of Science.1994, 294.1061-1134
Argue J J, Brimhall G H. Geochemical modelling of steady state fluid flow and chemical reaction during supergene enrichment of porphyry copper deposits. Economic Geology.1989, 84: 506-528
Argue J J, Brimhall G H. Magmatic arc asymmetry and distribution of anomalous plutonic belts in the batholiths of California-effects of assimilation, crustal theickness, and depth of crystallization. Geological Society of America Bulletin.1988.100:912-927
Argue J J, Brimhall G H. Regional variations in bulk chemistry, mineralogy, and the compositions of mafic and accessory minerals in the batholiths of California. Geological Society of America Bulletin.1988.100:891-911
Batchelor R A, Bowden P.Petrogenetic interpretation of granitoid rock series using multicationic parameters.Chemical Geology.1985, 48:43-55
Brimhall G H, Dietrich W F. Constitutive mass balance relations between chemical composition, volume, density, porosity and strain in metasomatic hydrothermal systems: Results on weathering and pedogenesis.Geochimicaet Cosmochimica Acta, 1987, 51:566-587
Condie K C, Sinha A K.Rare earth and other trace element mobility during mylonitization:a comparison ofthe Brevasrd and Hope Valley shear zones in the Appalachian Mountains,USA.J.Metamorphic Geol.1996,14:213-226
Eilu P and Mikucki E J. Alteration and primary geochemical dispersion associated with the Bulletin lode-gold deposit, Wiluna, Western Australia.Journal of Geochemical Exploration. 1998, 63:73-103
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 (Sup): 123-134
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
Grant J A. The isocon diagram-a simple solution to Gresens' equation for metasomatic alteration. Economic Geology.1986, 81:1976-1982
Gresens R L.Composition-volume relation of metasonatism.Chemical Geology.1967, 2:47-55. Groves D I,Condie K C,Goldfarb R J,et al.Secular changes in global tectonic processes and their influence on the temporal distribution of gold-bearing mineral deposits:Economic Geology.2005,100:203-224
Harris N B W, Pearce J A, Tindle A G.Geochemical characteristics of collision-zone magmatism. In: Coward M P and Reis A C (eds), Collision tectonics.Spec.Publ.Geol.Soc.Lond.1986, 19:67-81
Klammer D.Mass change during extreme acide-sulphate hydrothermal alteration of a Tertiary latite, Styria, Kutina J.Ore deposit controls by fracture patterns of the crust and by mantle-rooted structural discontinuities.Earth Science Front.1999, 6(1):29-35
MacLean W H.Mass change calculations in altered rock series.Mineralium Deposita.1990, 25:44-49
MacLean W H, Kranidiotis P.Immobile elements as monitorsof mass transfer in hydroth- ermal alteration: Phelps Dodgemassive sulphide deposit.Matagami, Quebec.Economic Geology. 1987, 82:951-962
Maniar P D,Piccoli P M.Tectonic discriminations of granitoids.Geological Society of America Bulletin.1989,101:635-643
Moustafa E O,巩恩普,孙旭东,等.浙江花岗岩中斜长石钾交代产生的条纹长石.地质与资源. 2003,12(3):129-138
O’Hara K.Fluid flow and volume loss during mylonitization-An origin for phyllonite in an overthrust getting, North Carnolina,U.S.A.Toctonophysics.1988, 156:21-36.
O’Hara K D.Fluid-rock interaction in crustal shear zones: a directed percolation approach. Geology.1994, 22:843-846
O’Hara K and Blavkburn W H.Volume-loss model for trace element enrichments in mylonite. Geology.1989, 17:524-527
Pearce J A,Harris N W,Tindle A G.Trace element discrimination diagrams for the tectonic interpretation of granitic rocks.Journal of Petrology,1984,25:956-983
Yang LQ,Deng J,Wang QF,et al.Coupling effects on gold mineralization of deep and shallow structures in the Northwestern Jiaodong Peninsula,Eastern China.Acta Geologica Sinica. 2006,80(3):400-411
Yang L Q,Deng J,Wang J G,et al.Control of deep tectonics on the superlarge deposits in China.Acta Geologica Sinica,2004,78(2):358-367
Yang L Q,Deng J,Zhang J,et al. Preliminarystudies of Fluid Inclusions in Damoqujia Gold Deposit along Zhaoping Fault Zone,Shandong province,China.Acta Petrologica Sinica,2006, 23(1):1-10
Yigit O and Hofstra A H. Lithogeochemistry of Carlin-type gold mineralization in the Gold Bar district, Battle Mountain-Eureka trend, Nevada.Ore Geology Reviews.2003, 22:201-224
边秋娟,张汉凯.乌拉山金矿钾长石的标型性及其与金矿化关系.黄金地质,1997,3(3):8-15
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.北京:中国地质大学出版社,2004
陈光远,鲁安怀.矿物成分标型继承性与金矿矿质来源.地学前缘,1994,1(3-4):204-210
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
陈光远,孙岱生,周珣若,等.胶东郭家岭花岗闪长岩成因矿物学与金矿化.武汉:中国地质大学出版社.1993
陈小龙.胶东新城金矿控矿构造解析及分形动力学研究:[硕士学位论文] .西安:长安大学,2010
陈衍景,Pirajno F,赖勇,等.胶东矿集区大规模成矿时间和构造环境.岩石学报,2004,20(4):907-922
陈衍景,郭光军,李欣.华北克拉通花岗绿岩地体中中生代金矿床的成矿地球动力学背景.中国科学(D辑),1998,28(1):35-40
陈玉民,邓军,杨立强等.《山东三山岛-仓上金矿带控矿规律研究及深部外围成矿预测》科研报告,2008
邓海琳,涂光炽,李朝阳,等.地球化学开放系统的质量平衡:1.理论.矿物学报,1999,19(2):121-131
邓军,王庆飞,杨立强,等.胶西北金矿集区成矿作用发生的地质背景.地学前缘,2004,11(4):527-533
邓军,方云,杨立强,等.剪切蚀变与物质迁移及金的富集——以胶东矿集区为例.地球科学,2000a,25(4):428-432
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
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,2005a,24(1):49-54
邓军,孙忠实,杨立强,等.成矿流体运动系统与金质来源和富集机制讨论.地质科技情报,2000b,19(1):41-45
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,2005b,30(1):102-108.
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,1996a.61-74
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,1996b,4:502-511
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
邓军,杨立强,刘伟,等.胶东招掖矿集区巨量金质来源和流体成矿效应.地质科学,2001,3:257-268
邓军,杨立强,孙忠实,等.剪切带构造成矿动力机制与模式.现代地质,1999a,13(2):125-129
邓军,杨立强,翟裕生,等.构造-流体-成矿系统及其动力学理论格架与方法体系.地球科学,2000c,25(1):71-78
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,1999b,6(2) :315-323
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
邓军.胶东西北部构造体系及其对金矿分布的控制作用:[博士学位论文].北京:中国地质科学院,1992
邓军.山东招掖金矿带断裂构造分带与蚀变矿化分带关系研究.矿床地质,1994,13(增刊):17-19
董敏.新城金矿构造控矿及矿体三维定位预测:[硕士学位论文] .西安:长安大学,2010 范永香,高秋斌,等.山东招远-掖县金矿带构造控矿规律研究.北京:中国地质大学出版社,1993
范永香,卢作祥,孙庆存,等.山东玲珑金矿田西山金矿床断裂构造控矿规律研究.黄金,1984,4.18-24
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,2003:108-136
高帮飞.山东招平金矿带构造-流体耦合成矿动力学[博士学位论文].北京:中国地质大学(北京),2008
高斌,马东升,刘连文.围岩蚀变过程中地球化学组分质量迁移计算——以湖南沃溪金锑钨矿床为例.地质学报,1999,73(3):272-277
郭春影.胶东三山岛-仓上金矿带构造-岩浆-流体金成矿系统:[博士学位论文].北京:中国地质大学(北京),2009
郭涛,吕古贤.胶东西北部金成矿带控矿构造系统分析.地质力学学报,2007,13(2):119-130
郭涛.胶西北金矿区域成矿系统及其构造-流体-矿化研究:[博士学位论文].北京:中国地质大学(北京),2005
胡受奚,王鹤年,王德滋,等.中国东部金矿地质及地球化学.北京:科学出版社.1998
胡受奚,叶瑛,赵懿英,等.华北地台中生代热液成矿的构造环境.高校地质学报,1995,1(1):58-66
胡受奚,赵懿英,徐金方,等.华北地台金矿地质.北京:科学出版社,1997
江少卿.招平断裂带金矿床构造-流体演化——磁组构与流体包裹体面约束:[硕士学位论文].北京:中国地质大学(北京),2007
李宏骥.胶北地区内生金矿成矿规律.山东地质,2002,18(3-4):72-77
李厚民,沈远超,毛景文,等.焦家式金矿构造-流体成矿作用特征—以胶西北金城金矿床为例.大地构造与成矿学,2002b,26(4):396-402
李厚民.山东莱州金城金矿床构造-流体成矿特征:[博士学位论文] .北京:中国科学院地质与地球物理研究所,2002a
李惠,张国义,禹斌.构造叠加晕模型及找矿效果.北京:地质出版社,2006
李惠,张文华,刘宝林.山东新城金矿床的叠加晕模式.地质找矿论丛,1998,13(1):1-12
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(04):217-223
李金祥,郭涛,吕古贤.试论胶东西北部金矿化类型及其与构造关系.贵金属地质,1999,8(2):87-91
李金祥.胶东西北部招平断裂带构造特征与成矿:[博士学位论文].北京:中国地质大学(北京),2005
李俊英.焦家构造带控矿作用探讨—以莱州新城金矿床为例.山东地质,2001,17(2):36-43
李士先,刘连生.山东胶西北S型构造及其对金矿的控制作用.地质力学文集,1981,5:38-57
李士先,王建收.胶东“玲珑-焦家式”金矿资源潜力与找矿.山东国土资源,2006.22(12):36-41
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
林景仟,谭东娟,迟效国,等.胶辽半岛中生代花岗岩.北京:科学出版社,1992
林伟,Michel Faure,王清晨.胶东半岛中生代构造演化的几何学和运动学.地质科学,2003,38(4):495-505
林文蔚,赵一鸣,徐珏.胶东招远-平度断裂活动性质及活动时代.中国区域地质,2002,19(2):43-50
林文蔚,赵一鸣,赵国红,等.胶东西北部金矿的控制因素.矿床地质,1997,16(2):107-117
凌其聪,刘丛强.层控夕卡岩型矿床成矿系统的元素活动性及质量迁移——以铜陵冬瓜山铜矿床为例.矿物学报,2003,23(1):37-44
刘春华,孙景贵,郑常青.胶东文登岩体——二长花岗质岩石地球化学特征及成因探讨.吉林地质,1995,14(4):51-58
刘德良,杨晓勇,杨海涛,等.郯庐断裂带南段桴槎山韧性剪切带糜棱岩的变形条件和组分迁移系.岩石学报,1996,12(4):573-588
刘建明,叶杰,徐九华,等.初论华北东部中生代金成矿的地球动力学背景—以胶东金矿为例.地球物理学进展,2001,16(1):39-46
刘景波,游振东.秦岭中条带状混合岩质量等比线分析.岩石学报,1997,13(3):427-438
刘俊.胶东西北部金矿床成岩成矿深度及变化保存研究:[硕士学位论文].北京:中国地质大学(北京),2009
刘日富.胶东西北地区金矿床控矿构造特征及金矿床类型.黄金,1997,18((7):13-15
刘忠明.剪切带流体与蚀变和金矿成矿作用.地学前缘,2001,8(4):271-274
卢作祥,范永香,刘石年,等.山东玲珑金矿田断裂构造控矿作用探讨.地球科学,1983,3:127-138
卢作祥,范永香,孙丰月.山东招掖金矿带的构造-岩浆控制.地球科学,1987b,12(6):589-597
卢作祥,范永香.山东招掖金矿带的构造一岩浆控制.地球科学,1987a,12(6):589-597
卢作祥,章增凤,张亚雄.山东招掖金矿带控矿断裂断面迁移规律及其意义地球科学.1988,13(2):121-128
鲁安怀,陈光远.铬铝云母成因矿物学——兼论焦家式金矿床成因与找矿.北京:地质出版社,1995.
吕古贤,郭涛,舒斌,等.构造变形岩相形迹的大比例尺填图及其对隐伏矿床地质预测——以胶东玲珑-焦家式金矿为例.中国区域地质,2001b,20(3) .313-321
吕古贤,郭涛,舒斌,等.胶东金矿集中区构造控岩控矿地质特征研究.地球学报,2006,21(5):471-478
吕古贤,郭涛,舒斌,等.胶东金矿集中区构造体系多层次控矿规律研究.大地构造与成矿学,2007,31(2):193-203
吕古贤,孔庆存.胶东玲珑-焦家式金矿地质.北京:科学出版社,1993
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,2004,17(2):1-6
吕古贤.胶东玲珑-焦家式金矿床矿源岩系(序)列研究.地质地球化学,2001a,29(3):140-143
吕古贤.山东玲珑金矿田和焦家金矿田成矿深度的研究与测算.中国科学D辑,1997,27(4):337-342
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
马丽芳(主编).中国地质图集.北京:地质出版社,2002
马胜利,马瑾.岩石的流变性质与断层模型.地球物理学进展,1995,10(3):21-42
毛景文,赫英,丁梯平.胶东金矿形成期间地慢流体参与成矿过程的碳氧氢同位素证据.矿床地质,2002,2:121-128
苗来成,罗镇宽,关康,等.胶东招掖金矿带控矿断裂演化规律.地质找矿论丛,1997,12(1):26-34
潘玉成.胶东金矿中浸染状钾长石的发现及其意义.黄金地质,1995,1(3):76-80
邱家骧.岩浆岩岩石学.北京:地质出版社,1985
裘有守,王孔海,杨广华,等.山东招远-掖县地区金矿区域成矿条件.沈阳:辽宁科学技术出版社,1988
任英忱,王铁军,王存昌.山东招远-掖县地区金矿床的矿物分带.地质找矿论丛,1988,3(4):42-52
任云生,蔺刚,彭晓蕾.郯庐断裂构造系统对胶东西部地区金矿的控制作用.黄金1997,18(2):3-7
山东六队.山东招(远)掖(县)地区金矿床控矿地质条件与矿床地质特征的研究报告.1983
山东省地质矿产局.山东省区域地质志.北京:地质出版社.1991
申玉科,吕古贤,李颖,等.构造-流体-蚀变矿化网络模式浅析.矿物学报,2009:244-247
申玉科.胶西北金矿集中区构造-蚀变网络研究:[博士学位论文].北京:中国地质大学(北京),2006
石玉臣,刘长春,杨承海,等.胶东地区蚀变岩型与石英脉型金矿的空间分布关系及形成机制.山东国土资源,2005,21(8):19-21
舒斌.胶东西北部典型金矿构造一岩相形迹与构造物理化学特征:[博士学位论文] .北京:中国地质大学(北京),1997
孙丰月,石准立,冯本智.胶东金矿地质及幔源C-H-O流体分异成岩成矿.长春:吉林人民出版社,1995
孙景贵,胡受奚,凌洪飞,等.胶西北两类金矿田的高钾-钾质脉岩元素地球化学与成岩作用研究.地球化学,2000b,29(2):143-152
孙景贵,胡受奚,凌洪飞.胶东金矿区高钾-钾质脉岩地球化学与俯冲-壳幔作用研究.岩石学报,2000a,16(3):401-412
孙莉.胶东谢家沟金矿床流体包裹体研究:[硕士学位论文].北京:中国地质大学(北京),2006
孙涛,关会明,陈华珍.浅议焦家金矿田构造控矿规律及进一步找矿方向.黄金,2007,28(2):7-11
唐红峰,刘丛强,谢国刚.区域变质作用中岩石的质量迁移和元素活动-以庐山双桥山群变泥质岩系为例.地质论评,2000,46(3):245-254
王海芹,霍光辉.胶东地区与金矿成矿有关的花岗岩体中的流体包裹体研究.地质力学学报,2008,14(3):263-273
王鹤年,徐克勤,陈延安,等.胶东中元古代玲珑花岗岩及其后期叠加改造作用的地质地球化学证据.南京大学学报-地球科学版,1988,1:105-118
王华东,张建国,宗绪臻.新城金矿床围岩蚀变与金矿化的关系.黄金学报,1999,1(4):249-252
王吉珺.玲珑花岗岩成因探讨.地质找矿论丛,2000,15(4):289-298
王来军,王秀娟.河西金矿构造控矿规律及预测研究.黄金,2003,2(24) :18-23
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
王铁军,阎方.胶东地区岩浆热液型金矿成矿流体演化与成矿预测.地质找矿论丛,2002,3:169-174
王燕,卢作祥.山东招掖金矿带焦家式金矿的矿床分带.地球科学.1988,13(2):137-146
魏俊浩,刘丛强,丁振举.热液型金矿床围岩蚀变过程中元素迁移规律——以张家口地区东
坪、后沟、水晶屯金矿为例.矿物学报,2000,20(2):200-206
吴海庆,叶官威,龙世祥,等.新城矿区资源储量年度报告.山东黄金矿业股份有限公司新城金矿,2007
肖庆辉,邓晋福,马大铨,等.花岗岩研究思维与方法.北京:地质出版社,2002,1-588
谢荣举,彭省临.岩石钾质变化及钾交代与成矿关系.大地构造与成矿学,1998,22(3):274-279
徐刚,郑达兴.胶东焦家断裂带韧性变形特征.地质力学学报,2003,9(1):70-76
徐刚.焦家断裂带特征及其与焦家金矿的成生关系:[博士学位论文] .北京:中国地质大学(北京),1996
徐贵忠,周瑞等.论胶东地区中生代岩石圈减薄的证据及其动力学机制.大地构造与成矿学,2001,4:368-380
徐红,徐光平.胶东煌斑岩的地球化学特征及成因探讨.岩石矿物学杂志,2000,19(1):36-44
徐洪林,张德全,孙桂英.胶东昆嵛山花岗岩的特征、成因及其与金矿的关系.岩石矿物学杂志,1997,16(2):131-143
阎凤增,邓军,张文钊,等.《山东大磨曲家金矿成矿动力学及找矿预测》科研报告,2006
杨承海,石玉臣,刘长春等.山东省焦家金成矿带大比例尺成矿预测中地质模型的研究与应用.山东国土资源地质力学学报,2006,22(5):34-37
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
杨进辉.胶东地区金矿床成矿时代及其成矿地球动力学背景-兼论壳幔相互作用与成岩成矿:[博士学位论文] .北京:中国科学院,2000
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
杨立强,邓军,翟裕生,王建平.胶东夏甸金矿地球化学场结构.现代地质,200l,15(4):409-413
杨立强,王光杰,张中杰,邓军,赵爱华,王建平.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
杨敏之,吕古贤.胶东绿岩带金矿地质地球化学.北京:地质出版社,1996
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
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
应汉龙.胶东邓格庄和金青顶金矿区煌斑岩特征及其与金成矿关系.岩石矿物学杂志,1996,15(3):221-227
於崇文,骆庭川,鲍征宇,等.南岭地区区域地球化学.北京:地质出版社,1987
翟明国,范宏瑞,杨进辉,等.非造山带型金矿—胶东型金矿的陆内成矿作用.地学前缘,2004,11(1):85-98
翟明国,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
翟明国,朱日祥,刘建明,等.华北东部中生代构造体制转折的关键时限.中国科学D辑,2003,33(10):913-920
翟裕生,邓军,李晓波.区域成矿学.北京:地质出版社,1999
翟裕生,邓军,彭润民.矿床变化与保存的研究内容和研究方法.地球科学-中国地质大学学报,2000,25(4):340-345
翟裕生,彭润民,王建平,邓军.成矿系列的结构模型研究.高校地质学报,2003,9(4):510-518
翟裕生,王建平,邓军,彭润民.成矿系统与矿化网络研究.矿床地质,2002,21(2):106-110
翟裕生.成矿系统研究与找矿.地质调查与研究,2003,26(2):65-71
张存勇,熊正莲,尹剑飞等.新城金矿床控矿因素及深部成矿预测.黄金,2002,23(11):6-9
张可清,杨勇.蚀变岩质量平衡计算方法介绍.地质科技情报,2002,21(3):104-107
张瑞忠.胶东大尹格庄金矿床构造控矿规律与矿体定位预测:[硕士学位论文].北京:中国地质大学(北京),2008
张施晨.新城金矿金工艺矿物学研究报告.沈阳矿冶研究所.1986
赵冬冬,黄吉友,金刚.胶东半岛金矿床控矿构造特点浅析.地质找矿论丛,2008,23(2):125-128
赵海,赵可广,马耀丽,修春华.胶东新城金矿地质构造特征及深部找矿方向.地质力学学报,2004,10(2):129-131
赵鹏沄,顾雪祥,邓小华.山东焦家金矿矿床成因及成矿模式.地质与勘探,2007,43(4):29-35
赵振华,涂光炽.中国超大型矿床(II).北京:科学出版社,2003
钟增球,郭宝罗.构造岩与显微构造.武汉:中国地质大学出版社,1991
钟增球,游振东.剪切带的成分变异及体积亏损——以河台剪切带为例.科学通报,1995,40(10):913-916
周雷.胶西北上庄金矿床控矿构造与元素地球化学特征:[硕士学位论文].北京:中国地质大学(北京),2009
周伟新,万天丰.玲珑花岗岩体的变形磁组构特征及其与金矿的关系.地质科学,2000,35 (4):385-395
周永胜,何昌荣.地壳岩石变形行为的转变及其温压条件.地震地质,2000,22(2):167-178
朱大岗,吕古贤,郭初笋.胶东变质岩型金矿构造-岩相特征及其控矿作用.地质力学学报,1998,4(2):67-73
朱奉三.混合岩化热液型金矿床成矿作用初步研究——以招掖地区的金矿为例.地质与勘探,1980,7:1-9
朱作山,任英忱.应用数理统计方法研究玲珑、焦家两种类型金矿床的成因.地质找矿论丛,1988,3(3):72-78
Ague J J. Mass-transfer during barrovian metamorphism of pelites, south-central Connecticut. 1. Evidence for changes in composition and volume. American Journal of Science.1994, 294.989-1057
Ague J J. Mass-transfer during barrovian metamorphism of pelites, south-central Connecticut. 2. Channelized fluid-flow and the growth of staurolite and kyanite. American Journal of Science.1994, 294.1061-1134
Argue J J, Brimhall G H. Geochemical modelling of steady state fluid flow and chemical reaction during supergene enrichment of porphyry copper deposits. Economic Geology.1989, 84: 506-528
Argue J J, Brimhall G H. Magmatic arc asymmetry and distribution of anomalous plutonic belts in the batholiths of California-effects of assimilation, crustal theickness, and depth of crystallization. Geological Society of America Bulletin.1988.100:912-927
Argue J J, Brimhall G H. Regional variations in bulk chemistry, mineralogy, and the compositions of mafic and accessory minerals in the batholiths of California. Geological Society of America Bulletin.1988.100:891-911
Batchelor R A, Bowden P.Petrogenetic interpretation of granitoid rock series using multicationic parameters.Chemical Geology.1985, 48:43-55
Brimhall G H, Dietrich W F. Constitutive mass balance relations between chemical composition, volume, density, porosity and strain in metasomatic hydrothermal systems: Results on weathering and pedogenesis.Geochimicaet Cosmochimica Acta, 1987, 51:566-587
Condie K C, Sinha A K.Rare earth and other trace element mobility during mylonitization:a comparison ofthe Brevasrd and Hope Valley shear zones in the Appalachian Mountains,USA.J.Metamorphic Geol.1996,14:213-226
Eilu P and Mikucki E J. Alteration and primary geochemical dispersion associated with the Bulletin lode-gold deposit, Wiluna, Western Australia.Journal of Geochemical Exploration. 1998, 63:73-103
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 (Sup): 123-134
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
Grant J A. The isocon diagram-a simple solution to Gresens' equation for metasomatic alteration. Economic Geology.1986, 81:1976-1982
Gresens R L.Composition-volume relation of metasonatism.Chemical Geology.1967, 2:47-55. Groves D I,Condie K C,Goldfarb R J,et al.Secular changes in global tectonic processes and their influence on the temporal distribution of gold-bearing mineral deposits:Economic Geology.2005,100:203-224
Harris N B W, Pearce J A, Tindle A G.Geochemical characteristics of collision-zone magmatism. In: Coward M P and Reis A C (eds), Collision tectonics.Spec.Publ.Geol.Soc.Lond.1986, 19:67-81
Klammer D.Mass change during extreme acide-sulphate hydrothermal alteration of a Tertiary latite, Styria, Kutina J.Ore deposit controls by fracture patterns of the crust and by mantle-rooted structural discontinuities.Earth Science Front.1999, 6(1):29-35
MacLean W H.Mass change calculations in altered rock series.Mineralium Deposita.1990, 25:44-49
MacLean W H, Kranidiotis P.Immobile elements as monitorsof mass transfer in hydroth- ermal alteration: Phelps Dodgemassive sulphide deposit.Matagami, Quebec.Economic Geology. 1987, 82:951-962
Maniar P D,Piccoli P M.Tectonic discriminations of granitoids.Geological Society of America Bulletin.1989,101:635-643
Moustafa E O,巩恩普,孙旭东,等.浙江花岗岩中斜长石钾交代产生的条纹长石.地质与资源. 2003,12(3):129-138
O’Hara K.Fluid flow and volume loss during mylonitization-An origin for phyllonite in an overthrust getting, North Carnolina,U.S.A.Toctonophysics.1988, 156:21-36.
O’Hara K D.Fluid-rock interaction in crustal shear zones: a directed percolation approach. Geology.1994, 22:843-846
O’Hara K and Blavkburn W H.Volume-loss model for trace element enrichments in mylonite. Geology.1989, 17:524-527
Pearce J A,Harris N W,Tindle A G.Trace element discrimination diagrams for the tectonic interpretation of granitic rocks.Journal of Petrology,1984,25:956-983
Yang LQ,Deng J,Wang QF,et al.Coupling effects on gold mineralization of deep and shallow structures in the Northwestern Jiaodong Peninsula,Eastern China.Acta Geologica Sinica. 2006,80(3):400-411
Yang L Q,Deng J,Wang J G,et al.Control of deep tectonics on the superlarge deposits in China.Acta Geologica Sinica,2004,78(2):358-367
Yang L Q,Deng J,Zhang J,et al. Preliminarystudies of Fluid Inclusions in Damoqujia Gold Deposit along Zhaoping Fault Zone,Shandong province,China.Acta Petrologica Sinica,2006, 23(1):1-10
Yigit O and Hofstra A H. Lithogeochemistry of Carlin-type gold mineralization in the Gold Bar district, Battle Mountain-Eureka trend, Nevada.Ore Geology Reviews.2003, 22:201-224
边秋娟,张汉凯.乌拉山金矿钾长石的标型性及其与金矿化关系.黄金地质,1997,3(3):8-15
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.北京:中国地质大学出版社,2004
陈光远,鲁安怀.矿物成分标型继承性与金矿矿质来源.地学前缘,1994,1(3-4):204-210
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
陈光远,孙岱生,周珣若,等.胶东郭家岭花岗闪长岩成因矿物学与金矿化.武汉:中国地质大学出版社.1993
陈小龙.胶东新城金矿控矿构造解析及分形动力学研究:[硕士学位论文] .西安:长安大学,2010
陈衍景,Pirajno F,赖勇,等.胶东矿集区大规模成矿时间和构造环境.岩石学报,2004,20(4):907-922
陈衍景,郭光军,李欣.华北克拉通花岗绿岩地体中中生代金矿床的成矿地球动力学背景.中国科学(D辑),1998,28(1):35-40
陈玉民,邓军,杨立强等.《山东三山岛-仓上金矿带控矿规律研究及深部外围成矿预测》科研报告,2008
邓海琳,涂光炽,李朝阳,等.地球化学开放系统的质量平衡:1.理论.矿物学报,1999,19(2):121-131
邓军,王庆飞,杨立强,等.胶西北金矿集区成矿作用发生的地质背景.地学前缘,2004,11(4):527-533
邓军,方云,杨立强,等.剪切蚀变与物质迁移及金的富集——以胶东矿集区为例.地球科学,2000a,25(4):428-432
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
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,2005a,24(1):49-54
邓军,孙忠实,杨立强,等.成矿流体运动系统与金质来源和富集机制讨论.地质科技情报,2000b,19(1):41-45
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,2005b,30(1):102-108.
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,1996a.61-74
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,1996b,4:502-511
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
邓军,杨立强,刘伟,等.胶东招掖矿集区巨量金质来源和流体成矿效应.地质科学,2001,3:257-268
邓军,杨立强,孙忠实,等.剪切带构造成矿动力机制与模式.现代地质,1999a,13(2):125-129
邓军,杨立强,翟裕生,等.构造-流体-成矿系统及其动力学理论格架与方法体系.地球科学,2000c,25(1):71-78
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,1999b,6(2) :315-323
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
邓军.胶东西北部构造体系及其对金矿分布的控制作用:[博士学位论文].北京:中国地质科学院,1992
邓军.山东招掖金矿带断裂构造分带与蚀变矿化分带关系研究.矿床地质,1994,13(增刊):17-19
董敏.新城金矿构造控矿及矿体三维定位预测:[硕士学位论文] .西安:长安大学,2010 范永香,高秋斌,等.山东招远-掖县金矿带构造控矿规律研究.北京:中国地质大学出版社,1993
范永香,卢作祥,孙庆存,等.山东玲珑金矿田西山金矿床断裂构造控矿规律研究.黄金,1984,4.18-24
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,2003:108-136
高帮飞.山东招平金矿带构造-流体耦合成矿动力学[博士学位论文].北京:中国地质大学(北京),2008
高斌,马东升,刘连文.围岩蚀变过程中地球化学组分质量迁移计算——以湖南沃溪金锑钨矿床为例.地质学报,1999,73(3):272-277
郭春影.胶东三山岛-仓上金矿带构造-岩浆-流体金成矿系统:[博士学位论文].北京:中国地质大学(北京),2009
郭涛,吕古贤.胶东西北部金成矿带控矿构造系统分析.地质力学学报,2007,13(2):119-130
郭涛.胶西北金矿区域成矿系统及其构造-流体-矿化研究:[博士学位论文].北京:中国地质大学(北京),2005
胡受奚,王鹤年,王德滋,等.中国东部金矿地质及地球化学.北京:科学出版社.1998
胡受奚,叶瑛,赵懿英,等.华北地台中生代热液成矿的构造环境.高校地质学报,1995,1(1):58-66
胡受奚,赵懿英,徐金方,等.华北地台金矿地质.北京:科学出版社,1997
江少卿.招平断裂带金矿床构造-流体演化——磁组构与流体包裹体面约束:[硕士学位论文].北京:中国地质大学(北京),2007
李宏骥.胶北地区内生金矿成矿规律.山东地质,2002,18(3-4):72-77
李厚民,沈远超,毛景文,等.焦家式金矿构造-流体成矿作用特征—以胶西北金城金矿床为例.大地构造与成矿学,2002b,26(4):396-402
李厚民.山东莱州金城金矿床构造-流体成矿特征:[博士学位论文] .北京:中国科学院地质与地球物理研究所,2002a
李惠,张国义,禹斌.构造叠加晕模型及找矿效果.北京:地质出版社,2006
李惠,张文华,刘宝林.山东新城金矿床的叠加晕模式.地质找矿论丛,1998,13(1):1-12
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(04):217-223
李金祥,郭涛,吕古贤.试论胶东西北部金矿化类型及其与构造关系.贵金属地质,1999,8(2):87-91
李金祥.胶东西北部招平断裂带构造特征与成矿:[博士学位论文].北京:中国地质大学(北京),2005
李俊英.焦家构造带控矿作用探讨—以莱州新城金矿床为例.山东地质,2001,17(2):36-43
李士先,刘连生.山东胶西北S型构造及其对金矿的控制作用.地质力学文集,1981,5:38-57
李士先,王建收.胶东“玲珑-焦家式”金矿资源潜力与找矿.山东国土资源,2006.22(12):36-41
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
林景仟,谭东娟,迟效国,等.胶辽半岛中生代花岗岩.北京:科学出版社,1992
林伟,Michel Faure,王清晨.胶东半岛中生代构造演化的几何学和运动学.地质科学,2003,38(4):495-505
林文蔚,赵一鸣,徐珏.胶东招远-平度断裂活动性质及活动时代.中国区域地质,2002,19(2):43-50
林文蔚,赵一鸣,赵国红,等.胶东西北部金矿的控制因素.矿床地质,1997,16(2):107-117
凌其聪,刘丛强.层控夕卡岩型矿床成矿系统的元素活动性及质量迁移——以铜陵冬瓜山铜矿床为例.矿物学报,2003,23(1):37-44
刘春华,孙景贵,郑常青.胶东文登岩体——二长花岗质岩石地球化学特征及成因探讨.吉林地质,1995,14(4):51-58
刘德良,杨晓勇,杨海涛,等.郯庐断裂带南段桴槎山韧性剪切带糜棱岩的变形条件和组分迁移系.岩石学报,1996,12(4):573-588
刘建明,叶杰,徐九华,等.初论华北东部中生代金成矿的地球动力学背景—以胶东金矿为例.地球物理学进展,2001,16(1):39-46
刘景波,游振东.秦岭中条带状混合岩质量等比线分析.岩石学报,1997,13(3):427-438
刘俊.胶东西北部金矿床成岩成矿深度及变化保存研究:[硕士学位论文].北京:中国地质大学(北京),2009
刘日富.胶东西北地区金矿床控矿构造特征及金矿床类型.黄金,1997,18((7):13-15
刘忠明.剪切带流体与蚀变和金矿成矿作用.地学前缘,2001,8(4):271-274
卢作祥,范永香,刘石年,等.山东玲珑金矿田断裂构造控矿作用探讨.地球科学,1983,3:127-138
卢作祥,范永香,孙丰月.山东招掖金矿带的构造-岩浆控制.地球科学,1987b,12(6):589-597
卢作祥,范永香.山东招掖金矿带的构造一岩浆控制.地球科学,1987a,12(6):589-597
卢作祥,章增凤,张亚雄.山东招掖金矿带控矿断裂断面迁移规律及其意义地球科学.1988,13(2):121-128
鲁安怀,陈光远.铬铝云母成因矿物学——兼论焦家式金矿床成因与找矿.北京:地质出版社,1995.
吕古贤,郭涛,舒斌,等.构造变形岩相形迹的大比例尺填图及其对隐伏矿床地质预测——以胶东玲珑-焦家式金矿为例.中国区域地质,2001b,20(3) .313-321
吕古贤,郭涛,舒斌,等.胶东金矿集中区构造控岩控矿地质特征研究.地球学报,2006,21(5):471-478
吕古贤,郭涛,舒斌,等.胶东金矿集中区构造体系多层次控矿规律研究.大地构造与成矿学,2007,31(2):193-203
吕古贤,孔庆存.胶东玲珑-焦家式金矿地质.北京:科学出版社,1993
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,2004,17(2):1-6
吕古贤.胶东玲珑-焦家式金矿床矿源岩系(序)列研究.地质地球化学,2001a,29(3):140-143
吕古贤.山东玲珑金矿田和焦家金矿田成矿深度的研究与测算.中国科学D辑,1997,27(4):337-342
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
马丽芳(主编).中国地质图集.北京:地质出版社,2002
马胜利,马瑾.岩石的流变性质与断层模型.地球物理学进展,1995,10(3):21-42
毛景文,赫英,丁梯平.胶东金矿形成期间地慢流体参与成矿过程的碳氧氢同位素证据.矿床地质,2002,2:121-128
苗来成,罗镇宽,关康,等.胶东招掖金矿带控矿断裂演化规律.地质找矿论丛,1997,12(1):26-34
潘玉成.胶东金矿中浸染状钾长石的发现及其意义.黄金地质,1995,1(3):76-80
邱家骧.岩浆岩岩石学.北京:地质出版社,1985
裘有守,王孔海,杨广华,等.山东招远-掖县地区金矿区域成矿条件.沈阳:辽宁科学技术出版社,1988
任英忱,王铁军,王存昌.山东招远-掖县地区金矿床的矿物分带.地质找矿论丛,1988,3(4):42-52
任云生,蔺刚,彭晓蕾.郯庐断裂构造系统对胶东西部地区金矿的控制作用.黄金1997,18(2):3-7
山东六队.山东招(远)掖(县)地区金矿床控矿地质条件与矿床地质特征的研究报告.1983
山东省地质矿产局.山东省区域地质志.北京:地质出版社.1991
申玉科,吕古贤,李颖,等.构造-流体-蚀变矿化网络模式浅析.矿物学报,2009:244-247
申玉科.胶西北金矿集中区构造-蚀变网络研究:[博士学位论文].北京:中国地质大学(北京),2006
石玉臣,刘长春,杨承海,等.胶东地区蚀变岩型与石英脉型金矿的空间分布关系及形成机制.山东国土资源,2005,21(8):19-21
舒斌.胶东西北部典型金矿构造一岩相形迹与构造物理化学特征:[博士学位论文] .北京:中国地质大学(北京),1997
孙丰月,石准立,冯本智.胶东金矿地质及幔源C-H-O流体分异成岩成矿.长春:吉林人民出版社,1995
孙景贵,胡受奚,凌洪飞,等.胶西北两类金矿田的高钾-钾质脉岩元素地球化学与成岩作用研究.地球化学,2000b,29(2):143-152
孙景贵,胡受奚,凌洪飞.胶东金矿区高钾-钾质脉岩地球化学与俯冲-壳幔作用研究.岩石学报,2000a,16(3):401-412
孙莉.胶东谢家沟金矿床流体包裹体研究:[硕士学位论文].北京:中国地质大学(北京),2006
孙涛,关会明,陈华珍.浅议焦家金矿田构造控矿规律及进一步找矿方向.黄金,2007,28(2):7-11
唐红峰,刘丛强,谢国刚.区域变质作用中岩石的质量迁移和元素活动-以庐山双桥山群变泥质岩系为例.地质论评,2000,46(3):245-254
王海芹,霍光辉.胶东地区与金矿成矿有关的花岗岩体中的流体包裹体研究.地质力学学报,2008,14(3):263-273
王鹤年,徐克勤,陈延安,等.胶东中元古代玲珑花岗岩及其后期叠加改造作用的地质地球化学证据.南京大学学报-地球科学版,1988,1:105-118
王华东,张建国,宗绪臻.新城金矿床围岩蚀变与金矿化的关系.黄金学报,1999,1(4):249-252
王吉珺.玲珑花岗岩成因探讨.地质找矿论丛,2000,15(4):289-298
王来军,王秀娟.河西金矿构造控矿规律及预测研究.黄金,2003,2(24) :18-23
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
王铁军,阎方.胶东地区岩浆热液型金矿成矿流体演化与成矿预测.地质找矿论丛,2002,3:169-174
王燕,卢作祥.山东招掖金矿带焦家式金矿的矿床分带.地球科学.1988,13(2):137-146
魏俊浩,刘丛强,丁振举.热液型金矿床围岩蚀变过程中元素迁移规律——以张家口地区东
坪、后沟、水晶屯金矿为例.矿物学报,2000,20(2):200-206
吴海庆,叶官威,龙世祥,等.新城矿区资源储量年度报告.山东黄金矿业股份有限公司新城金矿,2007
肖庆辉,邓晋福,马大铨,等.花岗岩研究思维与方法.北京:地质出版社,2002,1-588
谢荣举,彭省临.岩石钾质变化及钾交代与成矿关系.大地构造与成矿学,1998,22(3):274-279
徐刚,郑达兴.胶东焦家断裂带韧性变形特征.地质力学学报,2003,9(1):70-76
徐刚.焦家断裂带特征及其与焦家金矿的成生关系:[博士学位论文] .北京:中国地质大学(北京),1996
徐贵忠,周瑞等.论胶东地区中生代岩石圈减薄的证据及其动力学机制.大地构造与成矿学,2001,4:368-380
徐红,徐光平.胶东煌斑岩的地球化学特征及成因探讨.岩石矿物学杂志,2000,19(1):36-44
徐洪林,张德全,孙桂英.胶东昆嵛山花岗岩的特征、成因及其与金矿的关系.岩石矿物学杂志,1997,16(2):131-143
阎凤增,邓军,张文钊,等.《山东大磨曲家金矿成矿动力学及找矿预测》科研报告,2006
杨承海,石玉臣,刘长春等.山东省焦家金成矿带大比例尺成矿预测中地质模型的研究与应用.山东国土资源地质力学学报,2006,22(5):34-37
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
杨进辉.胶东地区金矿床成矿时代及其成矿地球动力学背景-兼论壳幔相互作用与成岩成矿:[博士学位论文] .北京:中国科学院,2000
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
杨立强,邓军,翟裕生,王建平.胶东夏甸金矿地球化学场结构.现代地质,200l,15(4):409-413
杨立强,王光杰,张中杰,邓军,赵爱华,王建平.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
杨敏之,吕古贤.胶东绿岩带金矿地质地球化学.北京:地质出版社,1996
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
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
应汉龙.胶东邓格庄和金青顶金矿区煌斑岩特征及其与金成矿关系.岩石矿物学杂志,1996,15(3):221-227
於崇文,骆庭川,鲍征宇,等.南岭地区区域地球化学.北京:地质出版社,1987
翟明国,范宏瑞,杨进辉,等.非造山带型金矿—胶东型金矿的陆内成矿作用.地学前缘,2004,11(1):85-98
翟明国,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
翟明国,朱日祥,刘建明,等.华北东部中生代构造体制转折的关键时限.中国科学D辑,2003,33(10):913-920
翟裕生,邓军,李晓波.区域成矿学.北京:地质出版社,1999
翟裕生,邓军,彭润民.矿床变化与保存的研究内容和研究方法.地球科学-中国地质大学学报,2000,25(4):340-345
翟裕生,彭润民,王建平,邓军.成矿系列的结构模型研究.高校地质学报,2003,9(4):510-518
翟裕生,王建平,邓军,彭润民.成矿系统与矿化网络研究.矿床地质,2002,21(2):106-110
翟裕生.成矿系统研究与找矿.地质调查与研究,2003,26(2):65-71
张存勇,熊正莲,尹剑飞等.新城金矿床控矿因素及深部成矿预测.黄金,2002,23(11):6-9
张可清,杨勇.蚀变岩质量平衡计算方法介绍.地质科技情报,2002,21(3):104-107
张瑞忠.胶东大尹格庄金矿床构造控矿规律与矿体定位预测:[硕士学位论文].北京:中国地质大学(北京),2008
张施晨.新城金矿金工艺矿物学研究报告.沈阳矿冶研究所.1986
赵冬冬,黄吉友,金刚.胶东半岛金矿床控矿构造特点浅析.地质找矿论丛,2008,23(2):125-128
赵海,赵可广,马耀丽,修春华.胶东新城金矿地质构造特征及深部找矿方向.地质力学学报,2004,10(2):129-131
赵鹏沄,顾雪祥,邓小华.山东焦家金矿矿床成因及成矿模式.地质与勘探,2007,43(4):29-35
赵振华,涂光炽.中国超大型矿床(II).北京:科学出版社,2003
钟增球,郭宝罗.构造岩与显微构造.武汉:中国地质大学出版社,1991
钟增球,游振东.剪切带的成分变异及体积亏损——以河台剪切带为例.科学通报,1995,40(10):913-916
周雷.胶西北上庄金矿床控矿构造与元素地球化学特征:[硕士学位论文].北京:中国地质大学(北京),2009
周伟新,万天丰.玲珑花岗岩体的变形磁组构特征及其与金矿的关系.地质科学,2000,35 (4):385-395
周永胜,何昌荣.地壳岩石变形行为的转变及其温压条件.地震地质,2000,22(2):167-178
朱大岗,吕古贤,郭初笋.胶东变质岩型金矿构造-岩相特征及其控矿作用.地质力学学报,1998,4(2):67-73
朱奉三.混合岩化热液型金矿床成矿作用初步研究——以招掖地区的金矿为例.地质与勘探,1980,7:1-9
朱作山,任英忱.应用数理统计方法研究玲珑、焦家两种类型金矿床的成因.地质找矿论丛,1988,3(3):72-78
© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号 地址：北京市海淀区学院路29号 邮编：100083 电话：办公室：(+86 10)66554848；文献借阅、咨询服务、科技查新：66554700 |