全部 标题 作者
关键词 摘要

OALib Journal期刊
ISSN: 2333-9721
费用:99美元

查看量下载量

相关文章

更多...
矿床地质  2010 

胶东大庄子构造角砾岩型金矿床地质地球化学特征及其成矿流体来源探讨

Keywords: 地球化学,成矿流体,构造角砾岩,大庄子金矿

Full-Text   Cite this paper   Add to My Lib

Abstract:

大庄子金矿受胶莱盆地边缘发育于荆山群内的顺层状低角度断裂带控制,以大理岩质碎裂岩及角砾岩等张性构造岩胶结物发生矿化为特点。容矿岩石与成矿流体具有强烈的物质交换,矿化与SiO2、Fe2O3、Na2O及As、Cd、Hg、Cu、Pb等元素关系密切。矿石具有富集轻稀土元素、铕正异常的特征,其稀土元素特征和基性脉岩具有一定的相似性,又具有原岩的一些特点,表明容矿岩石受到了深部成矿流体的影响。硫、铅、碳-氧及氢-氧等同位素地球化学及流体包裹体研究显示,成矿物质较复杂,成矿流体来源于地壳深部或上地幔的岩浆热液,在成矿作用中,萃取了部分围岩,并与围岩发生了强烈反应。

References

[1]  Deines P,Stable istope variations in carbonatite,London:Umwin Hyman,1989.
[2]  Frimmel H E,Genesis of the world\'s largest gold deposits,Science,2002(5588).
[3]  郭百创,赵冬冬,平度市大庄子矿区金矿床成因类型探讨,地质与勘探,2002(4).
[4]  Jing L H,Shen Y C,Lin Q Z,Zeng Q D and Zou W L,Extraction and interperation for the northern marigin of the Jiaolai Basin with remote sensing,Geolgy and Prospecting,2001(1).
[5]  Hoefs Jochen,Stable isotope geochemistry,Beilin:Springer-Verlag,1987.
[6]  Koppel V H,Rudolf S,Lead isotope evidence on the detrital origin of Witwatersrand pyrites and its bearing on the provenance of the Witwatersrand gold,Economic Geology,1974(3).
[7]  Li X M,Oxygen,hydrogen,carbon stable isotopic study of Sanshangdao gold deposit,Shandong Province,Cotributions to Geology and Mineral Resources Resesreh,1988(3).
[8]  Lian G J,Study on stable isotope geochemistry and genesis of Dazhuangzi gold deposit,Contributions to Geolgy and Mineral Resources Research,2003(Supp).
[9]  Lian G J,Shi W Q,Mei S N,Liu L,Fluid inclusions in the Dazhuangzi gold deposit in Pingdu County,Shandong,Geolgy and Prospecting,2005(1).
[10]  Liu J M,Ye J,Xu J H,Jiang N and Ying H L,Preliminary discussion on geodynamic background of mesozoic gold metallogeny in eastern northchina:With examples from eastern Shandong Province,Pregress in Geophysics,2001(1).
[11]  Liu Y W,Li H J,Interlayer gliding structure and mineralization of Xilapkou gold field,east Shandong,Gold,2002(10).
[12]  Lu K Z,Dai J S,Formation and evolvement of the Jiaolai basin,Dongying:Uinversity of Petroleum Press,1994.
[13]  Mao J W,H Y,Li Y F,Mantle fluids involved in metallogenesis of Jiaodong(east Shandong) gold district:Evidence of C,O and H Isotopes,Mineral Deposits,2002(2).
[14]  Mao J W,Li H M,Wang Y T,Zhang C Q and Wang R T,The relationship between mantle-derived fluid and gold ore-formation in the eastern Shandong Peninsula:Evidences from D-O-C-S isotopes,Acta Geologica Sinica,2005(6).
[15]  Meier D L,Heinrich C A,Li Z X,Mafic dikes displacing Witwatersrand gold reefs:Evidence against metamorphic-hydrothermal ore formation,Geology,2009(7).
[16]  Minter W E L,Feather C E,Glatthaar C W,Sedimentological and mineralogical aspects of the newly discovered Witwatersrand placer deposit that reflect Proterozic weathering,Welkom gold field,south Africa,Economic Geology,1988(3).
[17]  曲少飞,西涝口金矿区物化探特征及找矿方向,黄金科学技术,2007(6).
[18]  Reimer T O,Alternative model for the derivation of gold in the Witwatersrand Supergroup,Journal of the Geological Society,1984(2).
[19]  Shen Y C,Liu T B,Li H M,Li G M and Liu F T,Geological and geochemical features and genesis of Guocheng gold deposit in Haiyang County,Shandong Province,Geolgy and Prospecting,2001(1).
[20]  Shen Y C,Zhang L C,Liu T B,Zeng Q D and Li G M,Interlayer slid fault and its ore-controlling process,Geolgy and Prospecting,2001(1).
[21]  更多...
[22]  Song Y C,Hu W X,Lian G J,Gao X K,Trace elemental and Pb-S isotopic geochemistry of the Dazhuangzi gold deposit,east Shandong,China,Journalof Nanjing University,2004(6).
[23]  Spangenberg J E,Frimmel H E,Basin-internal derivation of hydrocarbons in the Witwatersrand Basin,south Africa:Evidence from bulk and molecular delta 13C data,Chemical Geology,2001(4).
[24]  Stanko M,Genesis of the Witwatersrand gold-uranium deposits,Economic Geology,1954(5).
[25]  Sun F Y,Shi Z L,Feng B Z,Gold ore geology lithogenesis and metallogenesis related to the differentiation of mantle-derived C-H-O fluids in Jiaodong peninsula eastern China,Chang Chun:People Publishing House of Jili,1995.
[26]  Xu S P,Wen Z T,Mineralization and ore Prospecting of gold deposit in Laiyang and Zangjiazhuang Basin of Jiaodong,Gold Geolgy,2003(1).
[27]  Yang M Z,L(U) G X,Geology and geochemistry of gold deposits in Jiaodong greestone belt,China,北京:地质出版社,1996.
[28]  Yang Z F,Xu J K,Zhao L S,The evolution of regional crust and the geochemistry on gold mineralization in Jiaodong,北京:地质出版社,1998.
[29]  Zhai M G,Zhu R X,Liu J M,Meng Q R Hou Q L Hu S B Li Z Zhang H F and Liu W,Key time limit of Mesozic tectonic regime transition in eastern North China Block,Science in China(Series D),2003(10).
[30]  Zhang Z R,Cheng S Z,Superlarge gold deposit exploration perspective in Jiaolai Basin of Jiaodong gold metallogenetic domain,Geochimica,1999(3).
[31]  Zhu D G,Lu G X,Deng J,Lu A Hand Zhang Z J,Tectonic lithofacies features of gold deposit of metamorphic rock type in eastern Shandong and its ore controlling,Journal of Geomechancs,1998(2).
[32]  Zhu D G,Zhang Z J,The geological characteristics of gold deposits in Dazhuangzi area,eastern Shandong Province,Bulletin of Mineralogy Petrology and Geochemistry,1998(1).
[33]  Zhu D G,Lu G X,Deng J,Lu A H,Discussion on the geology and genesis of Dazhuangzi gold deposit in eastern Shandong Province,Journal of Precious Metallic Geology,1999(2).
[34]  Zhu H L,Zhang H Q,Analysis on West Tangezhuang area gold mineralization Prospect in Jiaolai Basin,Gold Science and Technology,2006(2).
[35]  Zou W L,Geological -geochemical characteristics and the genesis of the Dazhuangzi gold deposit in Pingdu city,Shandong Provice:Descussing on the mineralization model of the interstratified glide breccia type gold deposit,Beijing:Institute of Geology and Geophysics,Chinese Academy of Sciences,2001.
[36]  郭百创,赵冬冬,平度市大庄子矿区金矿床成因类型探讨,地质与勘探,2002(4).
[37]  荆林海,沈远超,蔺启忠,曾庆栋,邹为雷,胶莱盆地北缘遥感信息提取及解译分析,地质与勘探,2001(1).
[38]  李晓明,山东三山岛金矿床氧、氢碳稳定同位素的研究及其应用,地质找矿论丛,1988(3).
[39]  连国建,大庄子金矿床稳定同位素地球化学研究,地质找矿论丛,2003(增刊).
[40]  连国建,史维全,门树宁,刘莉,山东省平度市大庄子金矿流体包裹体研究,地质与勘探,2005(1).
[41]  刘建明,叶杰,徐九华,姜能,应汉龙,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(1).
[42]  刘于旺,李洪杰,胶东西涝口金矿区层间滑动构造与成矿,黄金,2002(10).
[43]  陆克政,戴俊生,胶莱盆地的形成和演化,东营:中国石油大学出版社,1994.
[44]  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,矿床地质,2002(2).
[45]  毛景文,李厚民,王义天,张长青,王瑞廷,地幔流体参与胶东金矿成矿作用的氢氧碳硫同位素证据,地质学报,2005(6).
[46]  曲少飞,西涝口金矿区物化探特征及找矿方向,黄金科学技术,2007(6).
[47]  沈远超,刘铁兵,李厚民,李光明,刘福涛,山东海阳郭城金矿床地质地球化学特征及成因,地质与勘探,2001(1).
[48]  沈远超,张连昌,刘铁兵,曾庆栋,李光明,论层间滑动断层及其控矿作用——以山东胶莱盆地北缘金成矿带为例,地质与勘探,2001(1).
[49]  宋玉财,胡文瑄,连国建,高小康,胶东大庄子金矿微量元素及Pb-S同位素地球化学研究,南京大学学报(自然科学版),2004(6).
[50]  孙丰月,石准立,冯本智,胶东金矿地质及地幔C-H-O流体分异成岩成矿,长春:吉林人民出版社,1995.
[51]  徐述平,文中田,胶东莱阳和臧家庄盆地金矿成矿及找矿预测,黄金地质,2003(1).
[52]  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.
[53]  杨忠芳,徐景奎,赵伦山,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.
[54]  翟明国,朱日祥,刘建明,孟庆任,侯泉林,胡圣标,李忠,张宏福,刘伟,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(10).
[55]  张竹如,陈世桢,胶东金成矿域胶莱盆地中超大型金矿床找矿远景,地球化学,1999(3).
[56]  朱大岗,吕古贤,邓军,鲁安怀,张振江,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(2).
[57]  朱大岗,张振江,胶东大庄子金矿地质特征,矿物岩石地球化学通报,1998(1).
[58]  朱大岗,吕古贤,邓军,鲁安怀,胶东大庄子金矿地质特征和成因探讨,贵金属地质,1999(2).
[59]  朱洪岭,张华全,胶莱盆地西谭格庄地区金成矿前景分析,黄金科学技术,2006(2).
[60]  邹为雷,山东平度大庄子金矿床地质地球化学特征及成因--兼论层间滑动角砾岩型金矿成矿模式,北京:中国科学院地质与地球物理研究所,2001.

Full-Text

Contact Us

service@oalib.com

QQ:3279437679

WhatsApp +8615387084133