玲珑金矿田黑云母二长岩的发现及其Ar-Ar热年代学意义
|
摘要
胶东玲珑金矿田地表以下2070 m处发现黑云母二长岩,不仅可以探索该区金矿成矿物质的来源,而且对研究矿床成因提供了新的证据。黑云母二长岩在胶东金矿集中区地表及其他钻孔岩芯中尚未见报道,通过显微镜下观察、鉴定,具有典型的二长结构。非金属矿物主要有斜长石、正长石、石英、黑云母和角闪石;含有较多的金属矿物,主要为原生的黄铁矿和磁铁矿等。黑云母的40Ar-39Ar热年代学研究表明,黑云母二长岩的成岩年龄为123.7±1.5 Ma,晚于玲珑花岗岩、滦家河花岗岩和郭家岭花岗岩,与玲珑金矿的形成年龄非常接近。尽管玲珑金矿矿体中的金属矿物并不一定直接来源于黑云母二长岩,但从形成时间分析,二者具有成因联系。黑云母二长岩在侵入过程中可能为金矿的形成提供成矿物质、成矿流体,而且为成矿物质和成矿流体的运移提供能量及驱动力。因而可以推断,黑云母二长岩的侵入与玲珑金矿成矿作用关系密切。
The biotite monzolite that was discovered at 2170 meters below the surface in Linglong Gold Field in Jiaodong is not only used to find out the source of ore-forming material,but also is used to furnish new evidence for study the cause of mineralization of gold deposit. As the new rock types that was discovered in this area,Biotite monzonitichas the typical monzonitic texture under microscope. The non-metallic minerals composed the rock mainly are plagioclase,sodium feldspar,quartz,biotite and hornblende. It contains more metal minerals that mainly are pyrite and magnetitethan the other magmatic rocks in Northwest of Jiaodong. The biotite40Ar-39 Ar thermochronology indicate that the age of the formation of biotite monzonite is 123. 7 ± 1. 5 Ma which was later than the time of formation of Linglong granite,Luanjiahe granite and Guojialing granites,and is very close with the age of the formation of Linglong Gold Deposit. Although it is not sure that the metal minerals in the gold ore bodies in Linglong gold field directly come from biotite monzonite,the result of analysis of the characteristics of their generation time demonstrate that the metal minerals and biotite monzonite form in the same period and come from the same originate. In the process of invasion of the Biotite monzonite magma,it supply ore-forming materials for the formation of gold mine,and provides energy and driving force for ore-forming elements and ore-forming fluid migration. It can be deduced that the gold mineralization is closely related with the intrusion of biotite monzonite
The biotite monzolite that was discovered at 2170 meters below the surface in Linglong Gold Field in Jiaodong is not only used to find out the source of ore-forming material,but also is used to furnish new evidence for study the cause of mineralization of gold deposit. As the new rock types that was discovered in this area,Biotite monzonitichas the typical monzonitic texture under microscope. The non-metallic minerals composed the rock mainly are plagioclase,sodium feldspar,quartz,biotite and hornblende. It contains more metal minerals that mainly are pyrite and magnetitethan the other magmatic rocks in Northwest of Jiaodong. The biotite40Ar-39 Ar thermochronology indicate that the age of the formation of biotite monzonite is 123. 7 ± 1. 5 Ma which was later than the time of formation of Linglong granite,Luanjiahe granite and Guojialing granites,and is very close with the age of the formation of Linglong Gold Deposit. Although it is not sure that the metal minerals in the gold ore bodies in Linglong gold field directly come from biotite monzonite,the result of analysis of the characteristics of their generation time demonstrate that the metal minerals and biotite monzonite form in the same period and come from the same originate. In the process of invasion of the Biotite monzonite magma,it supply ore-forming materials for the formation of gold mine,and provides energy and driving force for ore-forming elements and ore-forming fluid migration. It can be deduced that the gold mineralization is closely related with the intrusion of biotite monzonite
引文
[1]杨立强,邓军,王中亮,等.胶东中生代金成矿系统[J].岩石学报,2014,30(9):2447~2467.YANG Li-qiang,DENG Jun,WANG Zhong-liang,et al.Mesozoic gold metallogenic system of the Jiaodong gold province,eastern China[J].Acta Petrologica Sinica,2014,30(9):2447~2467.
[2]WWANG H N,CHEN J,WANG Y,et al.1989.Geochemical Studies of Au-bearing Formation in Jiaodong Peninsula,Shandong Province[J].Chinese Journal of Geochemistry,8(3):213~227.
[3]Zhai M G,Yang J H,Liu W J.Large clusters of gold deposits and large-scale metallogenesis in the Jiaodong Peninsula,Eastern China[J].Science in China:Series D,2001,44(8):758~768.
[4]Qiu Y M,Groves D I,Mc Naughton N J,et al.Nature,age and tectonic setting of granitoid-hosted orogenic golddeposits of the Jiaodong Peninsula,eastern North China craton,China[J].Mineralium Deposit,2002,37(3/4):283~305.
[5]宋明春,张军进,张丕建,等.胶东三山岛北部海域超大型金矿床的发现及其构造-岩浆背景[J].地质学报,2015,89(2):365~383.SONG Ming-chun,ZHANG Jin-jun,ZHANG Pi-jian,et al.Discovery and tectonic-magmatic background of superlarge gold deposit in offshore of northern Sanshandao Shandong Peninsula,China[J].Acta Geoscientia Sinica,2015,89(2):365~383.
[6]孙国胜,刘颖,李绪俊,等.玲珑金矿田不同级别构造控矿特征[J].地质地球化学,2003,31(2):18~24.SUN Guo-sheng,LIU Ying,LI Xu-jun,et al.Studies on different types of fracture structures controlling gold orebodies in Linglong gold orefield[J].Geology-Geochemistry,2003,31(2):18~24.
[7]吕古贤,郭涛,刘杜鹃.玲珑-焦家式金矿构造地质特征及成矿构造物理化学参量因子分析——以阜山金矿区为例[J].地球学报,2002,23(5):409~416.LGu-xian,GUO Tao,LIU Du-juan.Geological and structural characteristics of the Linglong-Jiaojia type gold deposits and factor analysis of their metallogenic tectonic physicochemical parameters—exemplified by the Fushan gold deposit[J].Acta Geoscientia Sinica,2002,23(5):409~416.
[8]杜杜松金,李洪喜,张庆龙,等.山东招远玲珑金矿田控矿构造及其形成机制[J].高校地质学报,2003,9(3):420~426.DU Song-jin,LI Hong-xi,ZHANG Qing-long,et al.Relationship between ore-control fracture and gold doposits in Linglong Goldfield,Zhaoyuan,Shandong[J].Geological Journal of China Universities,2003,9(3):420~426.
[9]张张炳林,杨立强,黄锁英,等.胶东焦家金矿床热液蚀变作用[J].岩石学报,2014,30(9):2533~2545.ZHANG Bing-lin,YANG Li-qiang,HUANG Suo-ying,et al.Hydrothermal alteration in the Jiaojia gold deposit,Jiaodong,China[J].Acta Petrologica Sinica,2014,30(9):2533~2545.
[10]孙国胜,姚凤良,胡瑞忠,等.玲珑金矿田矿体富集规律及其控制因素[J].大地构造与成矿学,2001,25(4):464~470.SUN Guo-sheng,YAO Feng-liang,HU Rui-zhong,et al.Enriched laws and controlling factorsof ore bodies in the Linglong gold deposit[J].Geotectonic et Metallogenia,2001,25(4):464~470.
[11]吕古贤,邓军,郭涛,等.玲珑-焦家式金矿构造变形岩相形迹大比例尺填图与构造成矿研究[J].地球学报,1998,19(2):177~186.LGu-xian,DENG Jun,GUO Tao,et al.Large scale geological mapping of tectono deformation facies features and research of tectonic metallogenesis for the Linglong-Jiaojia type gold deposits[J].Acta Geoscientia Sinica,1998,19(2):177~186.
[12]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[J].中国区域地质,2001,20(3):313~322.LGu-xian,GUO Tao,SHU Bin,et al.Large-scale mapping of tectonic deformation and facies features and their implications for the prediction of hidden deposits:A case study of the Linglong-Jiaojia style gold deposit,Jiaodong[J].Regional Geology of China,2001,20(3):313~322.
[13]吕古贤.构造岩浆活化区金矿矿源岩系的矿化趋势度概念与研究性填图方法—以胶东玲珑-焦家式金矿为例[J].地球学报,2002,23(2):107~114.LGu-xian.The Concept of Mineralization Trending Degree and the Method for the Mapping of Gold Source Rocks in Structure-Magmatic Mobilized Area—Taking the Linglong-Jiaojia Type Gold Deposits as an Example[J].Acta Geoscientia Sinica,2002,23(2):107~114.
[14]卢焕章,Guha J,方根保.山东玲珑金矿的成矿流体特征[J].地球化学,1999,28(5):421~437.LU Huan-zhang,Guha J,FANG Gen-bao.Characteristics of ore-forming fluid in Linglong Gold Mine,Shandong,China[J].Geochimica,1999,28(5):421~437.
[15]卢焕章,袁万春,张国平,等.玲珑-焦家地区主要金矿床稳定同位素及同位素年代学[J].桂林工学院学报,1999,19(1):1~8.LU Huan-zhang,YUAN Wan-chun,ZHANG Guo-ping P,et al.Stable isotopes studies and age dating of gold deposits and Linglong granites in Linglong-Jiaojia area,Shandong,China[J].Journal of Guilin Institute of Technology,1999,19(1):1~8.
[16]范宏瑞,胡芳芳,杨进辉,等.胶东中生代构造体制转折过程中流体演化和金的大规模成矿[J].岩石学报,2005,21(5):1317~1328.FAN Hong-rui,HU Fang-fang,YANG Jin-hui,et al.Fluid evolution and large-scale gold metallogeny during Mesozoic tectonic transition in the eastern Shandong province[J].Acta Petrologica Sinica,2005,21(5):1317~1328.
[17]申玉科,徐增田,左文喆.山东玲珑矿田九曲矿段地质特征及找矿预测[J].黄金地质,2003,9(1):16~19.SHEN Yu-ke,XU Zeng-tian,ZUO Wen-zhe.Geology character and prospecting forecast in Jiuqu section of Linglong gold minefield,Shandong[J].Gold Geology,2003,9(1):16~19.
[18]李德江,宋泉吾,张勇,等.玲珑金矿田175支脉地质综合研究与成矿预测[J].黄金,2003,24(7):15~18.LI De-jiang,SONG Quan-wu,ZHANG Yong,et al.The comprehensive geological study and mineralizing prognosis of175th branch vein of Linglong gold field[J].Gold,2003,24(7):15~18.
[19]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[J].岩石学报,2000,16(3):454~458.YANG Jin-hui,ZHOU XHin-hua,CHEN Li-hui.Dating of gold mineralization for super-large altered tectonite-type golddepositsin Northwestern Jiaodong Peninsulaanditsimplicationsforgold metallogeny[J].Acta Petrologica Sinica,2000,16(3):454~458.
[20]黄涛,杨立强,刘向东,等.胶北地体地壳演化:玲珑黑云母花岗岩继承锆石U-Pb年龄、微量元素和Hf同位素证据[J].岩石学报,2014,30(9):2574~2594.HUANG Tao,YANG Li-qiang,LIU Xiang-dong,et al.Crustal evolution of the Jiaobeiterrane:Evidence from U-Pb ages,trace element compositions and Hf isotopes of inherited zircons of the Linglong biotitegranite[J].Acta Petrologica Sinica,2014,30(9):2574~2594.
[21]林文蔚,赵一呜,赵国红,等.玲珑花岗质杂岩的时代、空间形态、源岩及其数学模拟[J].岩石矿物杂志,1997,16(2):97~111.LIN Wen-wei,ZHAO Yi-ming,ZHAO Guo-hong,et al.Ages,Spatial Forms,Source Rocks and Mathematical Modeling of Linglong Granitic Complex[J].Acta Petrologica ET Mineralogica,1997,16(2):97~111.
[22]王安平,于洪林,姚杰.山东招远玲珑金矿田黄铜矿特征研究[J].黄金,2002,23(12):10~11.WANG An-ping,YU Hong-lin,YAO Jie.The characteristics of chalcopyrite in Linglong Goldfield,Zhaoyuan,Shandong Province[J].Gold,2002,23(12):10~11.
[23]Yang L Q,Deng J,Richard J G,et al.40Ar/39Ar geochronological constraints on the formation of the Dayingezhuang gold deposit:New implications for timing and duration of hydrothermal activity in the Jiaodong gold province,China[J].Gondwana Research,2014,25:1469~1483.
[24]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[J].黄金地质,2001,7(4):15~21.LUO Zhen-kuan,GUAN Kang,MIAO Lai-cheng.Discussion on relationship between lamprophyre veins and mineralization in the Linglong gold field,eastern Shandong[J].Gold Geology,2001,7(4):15~21.
[25]卫清,范宏瑞,蓝廷广,等.胶东寺庄金矿床成因:流体包裹体与石英溶解度证据[J].岩石学报,2015,31(4):1049~1062.WEI Q,FAN HR,LAN TG,et al.Genesis of Sizhuang gold deposit,Jiaodong Peninsula:Evidences from fluid inclusion and quartz solubility modeling[J].Acta Petrologica Sinica,2015,31(4):1049~1062.
[26]Xue J L,Li S R,Sun W Y,et al.Characteristics of the genetic mineralogy of pyrite and its significance for prospecting in the Denggezhuang gold deposit,Jiaodong Peninsula,China[J].Science in China:Earth Sciences,2014,57(4):644~661.
[27]王安平,姚杰.玲珑金矿金矿物表面电子显微结构的特征[J].黄金,2000,21(2):13~15.WANG An-ping,YAO Jie.The electron microstructural feature of the surface of the gold minerals of Linglong Gold Mine[J].Gold,2000,21(2):13~15.
[28]Li J W,Vasconcelos P M,Zhang J,et al.40Ar/39Ar constraints on a temporal link between gold mineralization,magmatism,and continental margin transtension in the Jiaodong gold province,eastern China[J].Journal of Geology,2003,111(6):741~751.
[29]Yang J H,Zhou X H.Rb-Sr,Sm-Nd and Pb isotope systematics of pyrite:Implications for the age and genesis of lode gold deposits[J].Geology,2001,29(8):711~714.
[30]李厚民,毛景文,沈远超,等.胶西北东季金矿床钾长石和石英的Ar-Ar年龄及其意义[J].矿床地质,2003,22(1):72~77.LI Hou-min,MAO Jing-wen,SHEN Yuan-chao,et al.Ar-Ar ages of K-feldspar and quartz from Dongji Gold Deposit,Northwest Jiaodong,and their significance[J].Mineral deposits,2003,22(1):72~77.
[31]Li Q L,Chen F K,Yang J H.Single grain pyrite Rb-Sr dating of the Linglong gold deposit,eastern China[J].Ore Geology Reviews,2008,34(3):263~270.
[32]Hu F F,Fan H R,Yang J H,et al.Mineralizing age of the Rushan lode gold deposit in the Jiaodong Peninsula:SHRIMP U-Pb dating on hydrothermal zircon[J].Chinese Science Bulletin,2004,49(15):1629~1636.
[33]胡芳芳,范宏瑞,杨进辉,等.胶东乳山金矿蚀变岩中绢云母40Ar/39Ar年龄及其对金成矿事件的制约[J].矿物岩石地球化学通报,2006,25(2):109~114.HU Fang-fang,FAN Hong-rui,YANG Jin-hui,et al.The40Ar/39Ar dating age of sericite from altered rocks in the Rushan lode gold deposit,Jiaodong Peninsula and its constraints on the gold mineralization[J].Bulletin of Mineralogy,Petrology and Geochemistry,2006,25(2):109~114.
[34]Zhang L C,Shen Y C,Liu T B,et al.40Ar/39Ar and Rb-Sr isochron dating of the gold deposits in northern margin of the Jiaolai Basin,Shandong,China[J].Science in China:Series D,2003,46(7):708~718.
[35]Wang L G,Qiu Y M,Mc Naughton N J,et al.Constraints on crustal evolution and gold metallogeny in the northwestern Jiaodong Peninsula,China,from SHRIMP U-Pb zircon studies of granitoids[J].Ore Geology Reviews,1998,13(1):275~291.
[36]张田,张岳桥,胶东半岛中生代侵入岩浆活动序列及其构造制约[J].高校地质学报,2007,13(2):323~336.ZHANG Tian,ZHANG Yue-qiao.Geochronological sequence of mesozoic Intrusive magmatism in Jiaodong peninsula and Its tectonic constraints[J].Geological Journal of China Universities,2007,13(2):323~336.
[37]陆丽娜,范宏瑞,胡芳芳,等.胶西北郭家岭花岗闪长岩侵位深度:来自角闪石温压计和流体包裹体的证据[J].岩石学报,2011,27(5):1521~1532.LU Li-na,FAN Hong-rui,HU Fang-fang,et al.Emplacement depth of the Guojialing granodiorites from the northwestern Jiaodong Peninsula,eastern China:Evidences from hornblende thermobarometry and fluid inclusions[J].Acta Petrologica Sinica,2011,27(5):1521~1532.
[38]梁亚运,刘学飞,李龚健,等.胶东地区脉岩成因与金成矿关系的研究:年代学及Sr-Nd-Pb同位素的约束[J].地质科技情报,2014,33(3):10~24.LIANG Ya-yun,LIU Xue-fei,LI Gong-jian,et al.Petrogenesis and Connection with Gold Deposits of Dikes in Jiaodong Peninsula,Eastern of North China Craton:Constraint on Geochronology and Sr-Nd-Pb Isotope[J].Geological Science and Technology Information,2014,33(3):10~24.
[39]陈文,万渝生,李华芹,等.同位素地质年龄测定技术及应用[J].地质学报,2011,85(11):1917~1947.CHEN Wen,WAN Yu-sheng,LI Hua-qin,et al.Isotope Geochronology:Technique and Application[J].Acta Geologica Sinica,2011,85(11):1917~1947.
[40]张连昌,沈远超,曾庆栋,等.山东中生代胶莱盆地北缘金矿床硫铅同位素地球化学[J].矿物岩石地球化学通报,2001,20(4):380~384.ZHANG Lian-chang,SHEN Yuan-chao,ZENG Qing-dong,et al.Sulfur and lead isotopic geochemistry of gold deposits at the Northern margin of Jiaolai Basin,East Shandong[J].Bulletin of Mineralogy,Petrology and Geochemistry,2001,20(4):380~384.
[41]Zhang X O,Cawood P A,Wilde S A,et al.Geology and timing of mineralization at the Cangshang gold deposit,northwestern Jiaodong Peninsula,China[J].Mineralium Deposita,2003,38:141~153.
[42]Qian J P,Chen H Y,Meng Y.Geological characteristics of the Sizhuang gold deposit in the region of Jiaodong,Shandong Province:A study on tectono-geochemical ore prospecting of ore deposits[J].Chinese Journal of Geochemistry,2011,30:539~553.
[43]吕古贤.胶东玲珑-焦家式金矿床矿源岩系(序)列研究[J].地质地球化学,2001,29(3):140~143.LGu-xian.Research on ore source series of the Linglong-Jiaojia-type gold deposits[J].Geology-Geochemistry,2001,29(3):140~143.
[44]刘辅臣,卢作祥,范永香,等.玲珑金矿中基性岩脉与矿化的关系探讨[J].地球科学:武汉地质学院学报,1984,27(4):37~46.LIU Fu-chen,LU Zuo-xiang,FAN Yong-xiang,et al.On the relation between inter mediate basic dykes and mineralization in Lingling Gold orefeild[J].Earth Science:Journal of Wuhan College of Geology,1984,27(4):37~46.
[45]刘连登,姚凤良,孔庆存,等.岩脉在热液矿床成因研究中的意义——以胶东西北部金矿床为例[J].长春地质学院学报,1984,(4):13~28.LIU Lian-deng,YAO Feng-liang,KONG Qing-cun,et al.The significance about the vain in studying the genesis of hydrothermal ore deposits[J].Journal of Changchun University of Earth Science,1984,(4):13~28.
[46]毛景文,赫英,丁悌平.胶东金矿形成期间地幔流体参与成矿过程的碳氧氢同位素证据[J].矿床地质,2002,21(2):121~128.MAO Jing-wen,HE Ying,DING Ti-ping.Mantle fluids Involved in metallogenesis of Jiaodong(East Shandong)Gold District:Evidence of C,O and H isotopes[J].Mineral Deposits,2002,21(2):121~128.
[47]Deng J,Liu W,Sun Z S,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[J].Science in China:Series D,2003,46(Supp.):123~134.
[48]张群喜,王生龙.山东谢家沟金矿脉岩特征及其与金矿成矿关系[J].安徽地质,2007,17(1):24~27,36.ZHANG Qun-xi,WANG Sheng-long.Characteristics of vein rocksand their relationship with gold metallogenism in the Xiejiagou gold mine,Shandong province[J].Geology of Anhui,2007,17(1):24~27,36.
[49]邓军,吕古贤,杨立强,等.构造应力场转换与界面成矿[J].地球学报,1998,19(3):244~250.DENG Jun,LGu-xian,YANG Li-qiang,et al.The transformation of tectonic stress field and i Interfacial metallogensis[J].Acta Geoscientia Sinica,1998,19(3):244~250.
[50]陆丽娜,范宏瑞,胡芳芳,等.胶西北新城金矿成矿流体与矿床成因[J].矿床地质,2011,30(3):522~532.LU Li-na,Fan Hong-rui,HU Fang-fang,et al.Ore-forming fluids and genesis of Xincheng altered rock gold deposit innorthwestern Jiaodong Peninsula[J].Mineral Deposits,2011,30(3):522~532.
[51]姜晓辉,范宏瑞,胡芳芳,等.胶东三山岛金矿中深部成矿流体对比及矿床成因[J].岩石学报,2011,27(5):1327~1340.JIANG Xiao-hui,FAN Hong-rui,HU Fang-fang,et al.Comparative studies on fluid inclusion indifferent depths and ore genesis of the Sanshandao gold deposit,Jiaodong Peninsula[J].Acta Petrologica Sinica,2011,27(5):1327~1340.
[52]胡芳芳,范宏瑞,沈昆,等.胶东乳山脉状金矿床成矿流体性质与演化[J].岩石学报,2005,21(5):1329~1338.HU Fang-fang,FAN Hong-rui,SHEN Kun,et al.Nature and evolution of oreforming fluids in the Rushanlode gold deposit,Jiaodong Peninsula of eastern China[J].Aeta Petrologica Sinica,2005,21(5):1329~1338.
[53]徐九华,谢玉玲,申世亮.小秦岭与胶东金矿床的成矿流体特征对比[J].矿床地质,1997,16(2):151~162.XU Jiu-hua,XIE Yu-ling,SHEN Shi-liang.A comparison of ore-forming fluids between gold deposits in Xiaoqinling Mountains and those in Jiaodong Peninsula[J].Mineral deposits,1997,16(2):151~162.
[54]林文蔚,殷秀兰.胶东金矿成矿流体同位素的地质特征[J].岩石矿物学杂志,1998,17(3):249~259.LIN Wen-wei,YIN Xiu-lan.Isotope geological characteristics of mineralizing fluids of gold deposits in Jiaodong area and a discussion on the application conditions of H.P.Taylor’s Equation[J].Acta Petrologica Et Mineralogica,1998,17(3):249~259.
[2]WWANG H N,CHEN J,WANG Y,et al.1989.Geochemical Studies of Au-bearing Formation in Jiaodong Peninsula,Shandong Province[J].Chinese Journal of Geochemistry,8(3):213~227.
[3]Zhai M G,Yang J H,Liu W J.Large clusters of gold deposits and large-scale metallogenesis in the Jiaodong Peninsula,Eastern China[J].Science in China:Series D,2001,44(8):758~768.
[4]Qiu Y M,Groves D I,Mc Naughton N J,et al.Nature,age and tectonic setting of granitoid-hosted orogenic golddeposits of the Jiaodong Peninsula,eastern North China craton,China[J].Mineralium Deposit,2002,37(3/4):283~305.
[5]宋明春,张军进,张丕建,等.胶东三山岛北部海域超大型金矿床的发现及其构造-岩浆背景[J].地质学报,2015,89(2):365~383.SONG Ming-chun,ZHANG Jin-jun,ZHANG Pi-jian,et al.Discovery and tectonic-magmatic background of superlarge gold deposit in offshore of northern Sanshandao Shandong Peninsula,China[J].Acta Geoscientia Sinica,2015,89(2):365~383.
[6]孙国胜,刘颖,李绪俊,等.玲珑金矿田不同级别构造控矿特征[J].地质地球化学,2003,31(2):18~24.SUN Guo-sheng,LIU Ying,LI Xu-jun,et al.Studies on different types of fracture structures controlling gold orebodies in Linglong gold orefield[J].Geology-Geochemistry,2003,31(2):18~24.
[7]吕古贤,郭涛,刘杜鹃.玲珑-焦家式金矿构造地质特征及成矿构造物理化学参量因子分析——以阜山金矿区为例[J].地球学报,2002,23(5):409~416.LGu-xian,GUO Tao,LIU Du-juan.Geological and structural characteristics of the Linglong-Jiaojia type gold deposits and factor analysis of their metallogenic tectonic physicochemical parameters—exemplified by the Fushan gold deposit[J].Acta Geoscientia Sinica,2002,23(5):409~416.
[8]杜杜松金,李洪喜,张庆龙,等.山东招远玲珑金矿田控矿构造及其形成机制[J].高校地质学报,2003,9(3):420~426.DU Song-jin,LI Hong-xi,ZHANG Qing-long,et al.Relationship between ore-control fracture and gold doposits in Linglong Goldfield,Zhaoyuan,Shandong[J].Geological Journal of China Universities,2003,9(3):420~426.
[9]张张炳林,杨立强,黄锁英,等.胶东焦家金矿床热液蚀变作用[J].岩石学报,2014,30(9):2533~2545.ZHANG Bing-lin,YANG Li-qiang,HUANG Suo-ying,et al.Hydrothermal alteration in the Jiaojia gold deposit,Jiaodong,China[J].Acta Petrologica Sinica,2014,30(9):2533~2545.
[10]孙国胜,姚凤良,胡瑞忠,等.玲珑金矿田矿体富集规律及其控制因素[J].大地构造与成矿学,2001,25(4):464~470.SUN Guo-sheng,YAO Feng-liang,HU Rui-zhong,et al.Enriched laws and controlling factorsof ore bodies in the Linglong gold deposit[J].Geotectonic et Metallogenia,2001,25(4):464~470.
[11]吕古贤,邓军,郭涛,等.玲珑-焦家式金矿构造变形岩相形迹大比例尺填图与构造成矿研究[J].地球学报,1998,19(2):177~186.LGu-xian,DENG Jun,GUO Tao,et al.Large scale geological mapping of tectono deformation facies features and research of tectonic metallogenesis for the Linglong-Jiaojia type gold deposits[J].Acta Geoscientia Sinica,1998,19(2):177~186.
[12]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[J].中国区域地质,2001,20(3):313~322.LGu-xian,GUO Tao,SHU Bin,et al.Large-scale mapping of tectonic deformation and facies features and their implications for the prediction of hidden deposits:A case study of the Linglong-Jiaojia style gold deposit,Jiaodong[J].Regional Geology of China,2001,20(3):313~322.
[13]吕古贤.构造岩浆活化区金矿矿源岩系的矿化趋势度概念与研究性填图方法—以胶东玲珑-焦家式金矿为例[J].地球学报,2002,23(2):107~114.LGu-xian.The Concept of Mineralization Trending Degree and the Method for the Mapping of Gold Source Rocks in Structure-Magmatic Mobilized Area—Taking the Linglong-Jiaojia Type Gold Deposits as an Example[J].Acta Geoscientia Sinica,2002,23(2):107~114.
[14]卢焕章,Guha J,方根保.山东玲珑金矿的成矿流体特征[J].地球化学,1999,28(5):421~437.LU Huan-zhang,Guha J,FANG Gen-bao.Characteristics of ore-forming fluid in Linglong Gold Mine,Shandong,China[J].Geochimica,1999,28(5):421~437.
[15]卢焕章,袁万春,张国平,等.玲珑-焦家地区主要金矿床稳定同位素及同位素年代学[J].桂林工学院学报,1999,19(1):1~8.LU Huan-zhang,YUAN Wan-chun,ZHANG Guo-ping P,et al.Stable isotopes studies and age dating of gold deposits and Linglong granites in Linglong-Jiaojia area,Shandong,China[J].Journal of Guilin Institute of Technology,1999,19(1):1~8.
[16]范宏瑞,胡芳芳,杨进辉,等.胶东中生代构造体制转折过程中流体演化和金的大规模成矿[J].岩石学报,2005,21(5):1317~1328.FAN Hong-rui,HU Fang-fang,YANG Jin-hui,et al.Fluid evolution and large-scale gold metallogeny during Mesozoic tectonic transition in the eastern Shandong province[J].Acta Petrologica Sinica,2005,21(5):1317~1328.
[17]申玉科,徐增田,左文喆.山东玲珑矿田九曲矿段地质特征及找矿预测[J].黄金地质,2003,9(1):16~19.SHEN Yu-ke,XU Zeng-tian,ZUO Wen-zhe.Geology character and prospecting forecast in Jiuqu section of Linglong gold minefield,Shandong[J].Gold Geology,2003,9(1):16~19.
[18]李德江,宋泉吾,张勇,等.玲珑金矿田175支脉地质综合研究与成矿预测[J].黄金,2003,24(7):15~18.LI De-jiang,SONG Quan-wu,ZHANG Yong,et al.The comprehensive geological study and mineralizing prognosis of175th branch vein of Linglong gold field[J].Gold,2003,24(7):15~18.
[19]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[J].岩石学报,2000,16(3):454~458.YANG Jin-hui,ZHOU XHin-hua,CHEN Li-hui.Dating of gold mineralization for super-large altered tectonite-type golddepositsin Northwestern Jiaodong Peninsulaanditsimplicationsforgold metallogeny[J].Acta Petrologica Sinica,2000,16(3):454~458.
[20]黄涛,杨立强,刘向东,等.胶北地体地壳演化:玲珑黑云母花岗岩继承锆石U-Pb年龄、微量元素和Hf同位素证据[J].岩石学报,2014,30(9):2574~2594.HUANG Tao,YANG Li-qiang,LIU Xiang-dong,et al.Crustal evolution of the Jiaobeiterrane:Evidence from U-Pb ages,trace element compositions and Hf isotopes of inherited zircons of the Linglong biotitegranite[J].Acta Petrologica Sinica,2014,30(9):2574~2594.
[21]林文蔚,赵一呜,赵国红,等.玲珑花岗质杂岩的时代、空间形态、源岩及其数学模拟[J].岩石矿物杂志,1997,16(2):97~111.LIN Wen-wei,ZHAO Yi-ming,ZHAO Guo-hong,et al.Ages,Spatial Forms,Source Rocks and Mathematical Modeling of Linglong Granitic Complex[J].Acta Petrologica ET Mineralogica,1997,16(2):97~111.
[22]王安平,于洪林,姚杰.山东招远玲珑金矿田黄铜矿特征研究[J].黄金,2002,23(12):10~11.WANG An-ping,YU Hong-lin,YAO Jie.The characteristics of chalcopyrite in Linglong Goldfield,Zhaoyuan,Shandong Province[J].Gold,2002,23(12):10~11.
[23]Yang L Q,Deng J,Richard J G,et al.40Ar/39Ar geochronological constraints on the formation of the Dayingezhuang gold deposit:New implications for timing and duration of hydrothermal activity in the Jiaodong gold province,China[J].Gondwana Research,2014,25:1469~1483.
[24]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[J].黄金地质,2001,7(4):15~21.LUO Zhen-kuan,GUAN Kang,MIAO Lai-cheng.Discussion on relationship between lamprophyre veins and mineralization in the Linglong gold field,eastern Shandong[J].Gold Geology,2001,7(4):15~21.
[25]卫清,范宏瑞,蓝廷广,等.胶东寺庄金矿床成因:流体包裹体与石英溶解度证据[J].岩石学报,2015,31(4):1049~1062.WEI Q,FAN HR,LAN TG,et al.Genesis of Sizhuang gold deposit,Jiaodong Peninsula:Evidences from fluid inclusion and quartz solubility modeling[J].Acta Petrologica Sinica,2015,31(4):1049~1062.
[26]Xue J L,Li S R,Sun W Y,et al.Characteristics of the genetic mineralogy of pyrite and its significance for prospecting in the Denggezhuang gold deposit,Jiaodong Peninsula,China[J].Science in China:Earth Sciences,2014,57(4):644~661.
[27]王安平,姚杰.玲珑金矿金矿物表面电子显微结构的特征[J].黄金,2000,21(2):13~15.WANG An-ping,YAO Jie.The electron microstructural feature of the surface of the gold minerals of Linglong Gold Mine[J].Gold,2000,21(2):13~15.
[28]Li J W,Vasconcelos P M,Zhang J,et al.40Ar/39Ar constraints on a temporal link between gold mineralization,magmatism,and continental margin transtension in the Jiaodong gold province,eastern China[J].Journal of Geology,2003,111(6):741~751.
[29]Yang J H,Zhou X H.Rb-Sr,Sm-Nd and Pb isotope systematics of pyrite:Implications for the age and genesis of lode gold deposits[J].Geology,2001,29(8):711~714.
[30]李厚民,毛景文,沈远超,等.胶西北东季金矿床钾长石和石英的Ar-Ar年龄及其意义[J].矿床地质,2003,22(1):72~77.LI Hou-min,MAO Jing-wen,SHEN Yuan-chao,et al.Ar-Ar ages of K-feldspar and quartz from Dongji Gold Deposit,Northwest Jiaodong,and their significance[J].Mineral deposits,2003,22(1):72~77.
[31]Li Q L,Chen F K,Yang J H.Single grain pyrite Rb-Sr dating of the Linglong gold deposit,eastern China[J].Ore Geology Reviews,2008,34(3):263~270.
[32]Hu F F,Fan H R,Yang J H,et al.Mineralizing age of the Rushan lode gold deposit in the Jiaodong Peninsula:SHRIMP U-Pb dating on hydrothermal zircon[J].Chinese Science Bulletin,2004,49(15):1629~1636.
[33]胡芳芳,范宏瑞,杨进辉,等.胶东乳山金矿蚀变岩中绢云母40Ar/39Ar年龄及其对金成矿事件的制约[J].矿物岩石地球化学通报,2006,25(2):109~114.HU Fang-fang,FAN Hong-rui,YANG Jin-hui,et al.The40Ar/39Ar dating age of sericite from altered rocks in the Rushan lode gold deposit,Jiaodong Peninsula and its constraints on the gold mineralization[J].Bulletin of Mineralogy,Petrology and Geochemistry,2006,25(2):109~114.
[34]Zhang L C,Shen Y C,Liu T B,et al.40Ar/39Ar and Rb-Sr isochron dating of the gold deposits in northern margin of the Jiaolai Basin,Shandong,China[J].Science in China:Series D,2003,46(7):708~718.
[35]Wang L G,Qiu Y M,Mc Naughton N J,et al.Constraints on crustal evolution and gold metallogeny in the northwestern Jiaodong Peninsula,China,from SHRIMP U-Pb zircon studies of granitoids[J].Ore Geology Reviews,1998,13(1):275~291.
[36]张田,张岳桥,胶东半岛中生代侵入岩浆活动序列及其构造制约[J].高校地质学报,2007,13(2):323~336.ZHANG Tian,ZHANG Yue-qiao.Geochronological sequence of mesozoic Intrusive magmatism in Jiaodong peninsula and Its tectonic constraints[J].Geological Journal of China Universities,2007,13(2):323~336.
[37]陆丽娜,范宏瑞,胡芳芳,等.胶西北郭家岭花岗闪长岩侵位深度:来自角闪石温压计和流体包裹体的证据[J].岩石学报,2011,27(5):1521~1532.LU Li-na,FAN Hong-rui,HU Fang-fang,et al.Emplacement depth of the Guojialing granodiorites from the northwestern Jiaodong Peninsula,eastern China:Evidences from hornblende thermobarometry and fluid inclusions[J].Acta Petrologica Sinica,2011,27(5):1521~1532.
[38]梁亚运,刘学飞,李龚健,等.胶东地区脉岩成因与金成矿关系的研究:年代学及Sr-Nd-Pb同位素的约束[J].地质科技情报,2014,33(3):10~24.LIANG Ya-yun,LIU Xue-fei,LI Gong-jian,et al.Petrogenesis and Connection with Gold Deposits of Dikes in Jiaodong Peninsula,Eastern of North China Craton:Constraint on Geochronology and Sr-Nd-Pb Isotope[J].Geological Science and Technology Information,2014,33(3):10~24.
[39]陈文,万渝生,李华芹,等.同位素地质年龄测定技术及应用[J].地质学报,2011,85(11):1917~1947.CHEN Wen,WAN Yu-sheng,LI Hua-qin,et al.Isotope Geochronology:Technique and Application[J].Acta Geologica Sinica,2011,85(11):1917~1947.
[40]张连昌,沈远超,曾庆栋,等.山东中生代胶莱盆地北缘金矿床硫铅同位素地球化学[J].矿物岩石地球化学通报,2001,20(4):380~384.ZHANG Lian-chang,SHEN Yuan-chao,ZENG Qing-dong,et al.Sulfur and lead isotopic geochemistry of gold deposits at the Northern margin of Jiaolai Basin,East Shandong[J].Bulletin of Mineralogy,Petrology and Geochemistry,2001,20(4):380~384.
[41]Zhang X O,Cawood P A,Wilde S A,et al.Geology and timing of mineralization at the Cangshang gold deposit,northwestern Jiaodong Peninsula,China[J].Mineralium Deposita,2003,38:141~153.
[42]Qian J P,Chen H Y,Meng Y.Geological characteristics of the Sizhuang gold deposit in the region of Jiaodong,Shandong Province:A study on tectono-geochemical ore prospecting of ore deposits[J].Chinese Journal of Geochemistry,2011,30:539~553.
[43]吕古贤.胶东玲珑-焦家式金矿床矿源岩系(序)列研究[J].地质地球化学,2001,29(3):140~143.LGu-xian.Research on ore source series of the Linglong-Jiaojia-type gold deposits[J].Geology-Geochemistry,2001,29(3):140~143.
[44]刘辅臣,卢作祥,范永香,等.玲珑金矿中基性岩脉与矿化的关系探讨[J].地球科学:武汉地质学院学报,1984,27(4):37~46.LIU Fu-chen,LU Zuo-xiang,FAN Yong-xiang,et al.On the relation between inter mediate basic dykes and mineralization in Lingling Gold orefeild[J].Earth Science:Journal of Wuhan College of Geology,1984,27(4):37~46.
[45]刘连登,姚凤良,孔庆存,等.岩脉在热液矿床成因研究中的意义——以胶东西北部金矿床为例[J].长春地质学院学报,1984,(4):13~28.LIU Lian-deng,YAO Feng-liang,KONG Qing-cun,et al.The significance about the vain in studying the genesis of hydrothermal ore deposits[J].Journal of Changchun University of Earth Science,1984,(4):13~28.
[46]毛景文,赫英,丁悌平.胶东金矿形成期间地幔流体参与成矿过程的碳氧氢同位素证据[J].矿床地质,2002,21(2):121~128.MAO Jing-wen,HE Ying,DING Ti-ping.Mantle fluids Involved in metallogenesis of Jiaodong(East Shandong)Gold District:Evidence of C,O and H isotopes[J].Mineral Deposits,2002,21(2):121~128.
[47]Deng J,Liu W,Sun Z S,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[J].Science in China:Series D,2003,46(Supp.):123~134.
[48]张群喜,王生龙.山东谢家沟金矿脉岩特征及其与金矿成矿关系[J].安徽地质,2007,17(1):24~27,36.ZHANG Qun-xi,WANG Sheng-long.Characteristics of vein rocksand their relationship with gold metallogenism in the Xiejiagou gold mine,Shandong province[J].Geology of Anhui,2007,17(1):24~27,36.
[49]邓军,吕古贤,杨立强,等.构造应力场转换与界面成矿[J].地球学报,1998,19(3):244~250.DENG Jun,LGu-xian,YANG Li-qiang,et al.The transformation of tectonic stress field and i Interfacial metallogensis[J].Acta Geoscientia Sinica,1998,19(3):244~250.
[50]陆丽娜,范宏瑞,胡芳芳,等.胶西北新城金矿成矿流体与矿床成因[J].矿床地质,2011,30(3):522~532.LU Li-na,Fan Hong-rui,HU Fang-fang,et al.Ore-forming fluids and genesis of Xincheng altered rock gold deposit innorthwestern Jiaodong Peninsula[J].Mineral Deposits,2011,30(3):522~532.
[51]姜晓辉,范宏瑞,胡芳芳,等.胶东三山岛金矿中深部成矿流体对比及矿床成因[J].岩石学报,2011,27(5):1327~1340.JIANG Xiao-hui,FAN Hong-rui,HU Fang-fang,et al.Comparative studies on fluid inclusion indifferent depths and ore genesis of the Sanshandao gold deposit,Jiaodong Peninsula[J].Acta Petrologica Sinica,2011,27(5):1327~1340.
[52]胡芳芳,范宏瑞,沈昆,等.胶东乳山脉状金矿床成矿流体性质与演化[J].岩石学报,2005,21(5):1329~1338.HU Fang-fang,FAN Hong-rui,SHEN Kun,et al.Nature and evolution of oreforming fluids in the Rushanlode gold deposit,Jiaodong Peninsula of eastern China[J].Aeta Petrologica Sinica,2005,21(5):1329~1338.
[53]徐九华,谢玉玲,申世亮.小秦岭与胶东金矿床的成矿流体特征对比[J].矿床地质,1997,16(2):151~162.XU Jiu-hua,XIE Yu-ling,SHEN Shi-liang.A comparison of ore-forming fluids between gold deposits in Xiaoqinling Mountains and those in Jiaodong Peninsula[J].Mineral deposits,1997,16(2):151~162.
[54]林文蔚,殷秀兰.胶东金矿成矿流体同位素的地质特征[J].岩石矿物学杂志,1998,17(3):249~259.LIN Wen-wei,YIN Xiu-lan.Isotope geological characteristics of mineralizing fluids of gold deposits in Jiaodong area and a discussion on the application conditions of H.P.Taylor’s Equation[J].Acta Petrologica Et Mineralogica,1998,17(3):249~259.