山东胶东金矿成矿理论体系
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摘要
在对胶东地区成矿地质背景、各种致矿地质-构造事件在时间和空间上的耦合、金矿床点时空结构、内在成生联系及时空配置关系研究的基础上,厘定了胶东金矿的概念、特征及主要表现形式,并对其进行了阐述,系统地提出了胶东地区金矿成矿的理论体系,即独具特色的四位一体构造叠置成矿背景、挤压-伸展手风琴式构造-岩浆-成矿作用方式和壳-幔流体多种来源的成矿物质,概括起来就是地质条件、定位方式和物质来源的有机耦合共同构成了胶东地区金矿成矿理论体系,这一理论解释了为何在该区形成巨量金矿的原因,是对胶东地区金矿理论研究的创新性成果。
On the basis of studying geological background of ore-forming,coupling of various tectonic events in time and space,time and space structures of gold deposit,internal relations and spatio-temporal relationship in Jiaodong area,the concept,characteristics and main forms of gold deposits in Jiaodong area have been introduced. The theoretical system of gold mineralization in Jiaodong area has been put forward,they are " four in one" tectonic superimposed metallogenic background,stretch-extrusion accordion style tectonic-magmatic-mineralization,and shell mantle fluid from many sources of ore-forming materials. The organic coupling of geological conditions,locations and material sources constitutes the system of metallogenic theory of gold deposits in Jiaodong area. This theory explains the formation of massive gold deposit in Jiaodong area. It is innovative achievement in the theoretical research of regional gold deposits.
On the basis of studying geological background of ore-forming,coupling of various tectonic events in time and space,time and space structures of gold deposit,internal relations and spatio-temporal relationship in Jiaodong area,the concept,characteristics and main forms of gold deposits in Jiaodong area have been introduced. The theoretical system of gold mineralization in Jiaodong area has been put forward,they are " four in one" tectonic superimposed metallogenic background,stretch-extrusion accordion style tectonic-magmatic-mineralization,and shell mantle fluid from many sources of ore-forming materials. The organic coupling of geological conditions,locations and material sources constitutes the system of metallogenic theory of gold deposits in Jiaodong area. This theory explains the formation of massive gold deposit in Jiaodong area. It is innovative achievement in the theoretical research of regional gold deposits.
引文
[1]李洪奎,李逸凡,耿科,等.山东鲁东碰撞造山型金矿成矿作用探讨[J].大地构造与成矿学,2011,35(4):533-542.
[2]李洪奎,时文革,李逸凡,等.山东胶东地区金矿成矿时代研究[J].黄金科学技术,2013,21(3):1-9.
[3]李洪奎,禚传源,耿科.胶东地区构造热事件对金矿成矿的约束与响应[M].济南:山东省地图出版社,2012.
[4]李洪奎,杨永波,耿科,等.山东重大基础地质问题研究进展[J].岩石学报,2013,29(2):594-606.
[5]李洪奎,耿科,禚传源,等.山东省优势大地构造相划分初步方案[J].山东国土资源,2010,26(6):1-6.
[6]李洪奎,于学峰.山东省大地构造相研究[M].北京:地质出版社,2012.
[7]李洪奎,耿科,禚传源,等.胶东金矿构造环境与成矿作用[M].北京:地质出版社,2016.
[8]胡芳芳,范宏瑞,杨进辉.胶东乳山含金石英脉型金矿的成矿年龄:热液锆石SHRIMP法U-Pb测定[J].科学通报,2004,49(12):1191-1198.
[9]胡芳芳,范宏瑞,杨进辉.鲁东昆嵛山地区宫家辉长闪长岩成因:岩石地球化学、锆石U-Pb年代学与Hf同位素制约[J].岩石学报,2007,23(2):369-380.
[10]丁正江,孙丰月,刘建辉,等.胶东邢家山钼钨矿床辉钼矿ReOs同位素测年及其地质意义[J].岩石学报,2012,28(9):2721-2732.
[11]丁正江,孙丰月,刘殿浩,等.烟台福山北部地区金及多金属矿成矿系列[J].山东国土资源,2011,27(1):1-6.
[12]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[J].岩石学报,2004,20(4):907-922.
[13]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.
[14]毛景文,张作衡,余金杰,等.华北及邻区中生代大规模成矿的地球动力学背景:从金属矿床年龄精测得到启示[J].中国科学(D辑),2003,33(4):289-299.
[15]毛景文,王忠良.中国东部大部分成矿时限及其动力学背景的初步探讨[J].矿床地质,2000,19(4):289-296.
[16]周新华,杨进辉,张连昌.胶东超大型金矿的形成与中生代华北大陆岩石圈深部过程[J].中国科学(D辑),2002,32(增刊):11-20.
[17]杨金中,沈远超,刘铁兵.大型-超大型金矿密集区的形成条件[J].地质与勘探,2001,37(1):30-32.
[18]李洪奎,杨永波,杨锋杰.山东沂沭断裂带构造演化与成矿作用[M].北京:地质出版社,2009.
[19]董树文,张岳桥,龙长兴,等.中国侏罗纪构造变革与燕山运动新诠释[J].地质学报,2007,81(11):1449-1461.
[20]毛景文,李厚民,王义天,等.地幔流体参与胶东金矿成矿作用的氢氧碳硫同位素证据[J].地质学报,2005,79(6):839-857.
[21]李洪奎,于学峰,沈昆,等.胶东玲珑矿田石英脉型金矿床中流体包裹体特征研究[J].山东国土资源,2012.28(11):1-8.
[22]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[M].长春:吉林人民出版社,1995.
[23]孙景贵,胡受奚,沈昆,等.胶东金矿区矿田体系中基性-中酸性脉岩的碳、氧同位素地球化学研究[J].岩石矿物学,2001,20(1):47-56.
[2]李洪奎,时文革,李逸凡,等.山东胶东地区金矿成矿时代研究[J].黄金科学技术,2013,21(3):1-9.
[3]李洪奎,禚传源,耿科.胶东地区构造热事件对金矿成矿的约束与响应[M].济南:山东省地图出版社,2012.
[4]李洪奎,杨永波,耿科,等.山东重大基础地质问题研究进展[J].岩石学报,2013,29(2):594-606.
[5]李洪奎,耿科,禚传源,等.山东省优势大地构造相划分初步方案[J].山东国土资源,2010,26(6):1-6.
[6]李洪奎,于学峰.山东省大地构造相研究[M].北京:地质出版社,2012.
[7]李洪奎,耿科,禚传源,等.胶东金矿构造环境与成矿作用[M].北京:地质出版社,2016.
[8]胡芳芳,范宏瑞,杨进辉.胶东乳山含金石英脉型金矿的成矿年龄:热液锆石SHRIMP法U-Pb测定[J].科学通报,2004,49(12):1191-1198.
[9]胡芳芳,范宏瑞,杨进辉.鲁东昆嵛山地区宫家辉长闪长岩成因:岩石地球化学、锆石U-Pb年代学与Hf同位素制约[J].岩石学报,2007,23(2):369-380.
[10]丁正江,孙丰月,刘建辉,等.胶东邢家山钼钨矿床辉钼矿ReOs同位素测年及其地质意义[J].岩石学报,2012,28(9):2721-2732.
[11]丁正江,孙丰月,刘殿浩,等.烟台福山北部地区金及多金属矿成矿系列[J].山东国土资源,2011,27(1):1-6.
[12]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[J].岩石学报,2004,20(4):907-922.
[13]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.
[14]毛景文,张作衡,余金杰,等.华北及邻区中生代大规模成矿的地球动力学背景:从金属矿床年龄精测得到启示[J].中国科学(D辑),2003,33(4):289-299.
[15]毛景文,王忠良.中国东部大部分成矿时限及其动力学背景的初步探讨[J].矿床地质,2000,19(4):289-296.
[16]周新华,杨进辉,张连昌.胶东超大型金矿的形成与中生代华北大陆岩石圈深部过程[J].中国科学(D辑),2002,32(增刊):11-20.
[17]杨金中,沈远超,刘铁兵.大型-超大型金矿密集区的形成条件[J].地质与勘探,2001,37(1):30-32.
[18]李洪奎,杨永波,杨锋杰.山东沂沭断裂带构造演化与成矿作用[M].北京:地质出版社,2009.
[19]董树文,张岳桥,龙长兴,等.中国侏罗纪构造变革与燕山运动新诠释[J].地质学报,2007,81(11):1449-1461.
[20]毛景文,李厚民,王义天,等.地幔流体参与胶东金矿成矿作用的氢氧碳硫同位素证据[J].地质学报,2005,79(6):839-857.
[21]李洪奎,于学峰,沈昆,等.胶东玲珑矿田石英脉型金矿床中流体包裹体特征研究[J].山东国土资源,2012.28(11):1-8.
[22]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[M].长春:吉林人民出版社,1995.
[23]孙景贵,胡受奚,沈昆,等.胶东金矿区矿田体系中基性-中酸性脉岩的碳、氧同位素地球化学研究[J].岩石矿物学,2001,20(1):47-56.