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矿床地质  2005 

胶东中生代花岗岩及大型-超大型金矿床形成的地球动力学环境

Keywords: 地质学,地球动力学环境,后碰撞,花岗岩,大型_超大型金矿床,胶东地区

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Abstract:

文章通过对大量前人构造地质学、同位素年代学等多元信息资料的分析,认为胶东中生代花岗岩和大型_超大型金矿床形成于华南_华北克拉通后碰撞挤压和伊泽奈崎板块快速斜冲剪切的双重构造环境及其后的拉张构造环境。胶东大型_超大型金矿床受控于经历了韧_脆性剪切、挤压_拉张复杂变形叠加的大型构造岩带,同时也受控于被断裂叠加的花岗岩接触带。根据铅、硫等同位素组成特征及地质构造环境的综合分析,认为成矿物质主要来自以太古宙胶东岩群绿岩和深成岩组成的结晶基底,不排除煌斑岩浆带来部分深源物质;根据流体包裹体的氢、氧、碳同位素组成,判断成矿流体为大气水和岩浆水的混合流体;成矿条件为中低温(380~100℃),低压(86~5.4MPa);成矿时代为燕山晚期(125~100Ma),成矿与燕山晚期拉张环境下的岩浆活动有成因联系,属环太平洋成矿带中温热液金矿床。

References

[1]  Bureau of Geology and Mineral Resources of Shandong Province. 1991. Regional geology of Shandong[M]. Beijing: Geol. Pub. House. 6~224(in Chinese with English abstract). 
[2]  Cao G Q. 1990. On Jiaonan terrain in Shandong Province[J]. Geology of Shandong, 6 (2): 1~9 (in Chinese).
[3]  Cao G Q, Wang Z B and Zhang C J. 1990. Jiaonan terrain in Shandong Province and tectonics significance of the Wulian_Rongchen fracture[J]. Geology of Shandong, 6 (1): 1~14(in Chinese).
[4]  Cheng P J. 1988. Huge wrench displacement timing and framwork of Tan-Lu fault zone[J]. Chinese Bulletin Science, 33(4): 289~293 (in Chinese).
[5]  Groves D I, Goldfarb R J, Robert F, et al. 2003. Gold deposits in metamorphic belts: Overview of understanding and outstanding problems, future research, and exploration significance[J]. Econ. Geol., 98: 1~29.
[6]  Hu S L, Wang S S, Sang H Q, et al. 1987. Isotopic ages of Linglong and Guojialing batholiths in Shandong Province and their geological implication[J]. Acta Petrologica Sinica, (3): 83~89 (in Chinese with English abstract).
[7]  Hu S X, Wang H N, Wang D Z, et al. 1994. Geology and geochemistry of gold deposits in East China[M]. Beijing: Science Press. 27~49 (in Chinese).
[8]  Huang D Y. 1994. Sulfur isotope studies of the metallogenic series of gold deposits in Jiaodong area[J] . Mineral Deposits, 13(1): 75~87(in Chinese with English abstract) .
[9]  Li H M, Miao J W, Shen Y C, et al. 2003. Ar-Ar ages of K-feldspar and quartz from Dongji gold deposit, Northwest Jiaodong and their signification[J]. Mineral Deposits, 22(1): 72~77(in Chinese with English abstract).
[10]  Li S G, Jagoutz E, Xiao Y L, et al. 1996. Ultrahigh metamorphic chronology of Dabieshan-Sulu terrane: Sm-Nd isotopic system[J]. Science in China (Series D), 26(3): 249~256(in Chinese).
[11]  Li Z L and Yang M Z.1993. The geology-geochemistry of gold deposits in Jiaodong Region[M]. Tianjin: Tianjin Science and Technology Press (in Chinese with English abstract).
[12]  Liu F C, Lu Z X, Fan Y X, et al. 1984. On the relation between intermediate-basic dykes and mineralization in Linglong gold ore field[J]. Earth Science, (4): 37~46(in Chinese with English abstract).
[13]  Liu F L, Xu Z Q and Song B. 2003. Determination of UHP and retrograde metamorphic ages of the Sulu Terrane: Evidence from SHRIMP U-Pb dating on zircon of gneisis rocks[J]. Atca geologica Sinica, 77(2): 227~237 (in Chinese with English abstract).
[14]  Liu H T, Sun S H, Liu J M, et al. 2002. The Mesozoic high-Sr granitoids in the northern marginal region of North China Craton: Geochemistry and source region[J]. Atca Petrologica Sinica, 18(3): 257~274 (in Chinese with English abstract).
[15]  Liu J M, Ye J, Xu J H, et al. 2003a. C-O and Sr-Nd isotopic geochemistry of carbonate minerals from gold depoaits in east Shandong, China[J]. Acta Petrologica Sinica, 19(4): 775[J]784 (in Chinese with English abstract).
[16]  Maruyama S, Isozaki Y, Kimura G, et al. 1997. Paleogeographic maps of the Japanese Island: Plate tectonic synthesis from 750 Ma to the present[J]. Island Arc, 6: 121~142.
[17]  Müler D and Groves D I. 1997. Potassic igneous rocks and associated gold-copper mineralization[M]. London: Springer. 85~133.
[18]  Qiu J S, Wang D Z, Zhou J C, et al. 1996. Geology, geochemistry and genesis of the Mesozoic shoshonitic volcanic rocks in Shandong Province[J]. Earth Science (Journal of China University of Geosciences), 21(5): 546~552 (in Chinese with English abstract).
[19]  Qu X M and Wang H N. 1997. Dynamic study on the crust-mantle magma mixing and emplecement mechanism of Guojialing granite[J]. Scientic Geology Sinica, 32(2): 443~454 (in Chinese with English abstract).
[20]  Ren J S, Jiang C F, Zhang Z K, et al. 1981. The tectonics of China and its evolution-illutration of 1∶4000,000 tectonic map of China[M]. Beijing: Science Press. 29~98 (in Chinese).
[21]  Rock N M S, Groves D I, Perring C S, et al. 1988a. Gold, lamprophyres and porphyries:What does their association mean? [A]. In: Keays R R, Ramsay W R H, Groves D I, eds. The geology of gold deposits:the perspective in 1988 [C]. EI Paso: The Ecnomic Geology Publishing Company. 1989. 609~625.
[22]  Rock N M S and Groves D I. 1988b. Do lamprophyres carry gold as well as diamonds[J]? Nature, 332: 253~255.
[23]  Rock N M S and Groves D I. 1988c. Can lamprophyres resolve the genetic controversy over mesothermal gold deposits[J]? Geology, 16: 538~541.
[24]  李曙光, Jagoutz E, 肖益林, 等. 1996. 苏鲁-大别高压地体变质年代学--Sm-Nd同位素体系[J]. 中国科学(D辑), 26(3): 249~257.
[25]  李兆龙, 杨敏之. 1993. 胶东金矿床地质地球化学[M]. 天津: 天津科学技术出版社.
[26]  刘辅臣, 卢作祥, 范永香, 等. 1984. 玲珑金矿中基性岩脉与矿化的关系探讨[J]. 地球科学, (4): 37~46.
[27]  刘福来, 许志琴, 宋彪. 2003. 苏鲁地体超高压和退变质时代的厘定: 来自片麻岩锆石微区SHRIMP U-Pb定年证据[J]. 地质学报, 77(2): 227~237.
[28]  邱检生, 王德滋, 周金城, 等.1996.山东中生代橄榄安粗岩系火山岩的地质地球化学特征及岩石成因[J]. 地球科学, 21(5): 546~552.
[29]  曲晓明, 王鹤年. 1997. 郭家岭岩体壳幔岩浆混合作用与侵位机制的动力学研究[J]. 地质科学, 32(4): 443~454.
[30]  任纪舜, 姜春发, 张正坤, 等. 1981. 中国大地构造及其演化--1∶400万中国大地构造图说明书[M]. 北京: 科学出版社. 29~37.
[31]  山东省地质矿产局. 1991. 山东省区域地质志[M]. 北京: 地质出版社. 6~224.
[32]  Simon A W, 张小鸥. 2002. 胶东金矿的成因和时代的基本控制[A]. 见: 山东招远金矿集团有限公司编. 中国金都招远国际金矿地质与勘查学术论坛论文集[C]. 北京: 地震出版社. 42~44.
[33]  孙希贤, 易顺华, 曾佐勋, 等. 1986. 断裂叠加-复合接触带及其对充填热液矿床成矿的控制作用[J]. 中国区域地质, (3): 249~255.
[34]  涂光炽. 2000. 中国超大型矿床(1)[M]. 北京: 科学出版社. 1~7, 91~94.
[35]  万天丰, 朱鸿, 赵磊, 等. 1996. 郯庐断裂带的形成与演化: 综述[J]. 现代地质, 10(2): 159~168.
[36]  王小凤, 李中坚, 陈伯林, 等. 2001. 郯庐断裂带[M]. 北京: 地质出版社.
[37]  王义文. 1988. 胶东西北部地区金矿床铅同位素特征及其地质意义[J]. 长春地质学院学报, 18(3): 277~286.
[38]  徐嘉炜. 1992. 郯庐断裂带研究的十年回顾[J]. 地质论评, 38(4): 316~325.
[39]  徐嘉炜. 1984. 郯城-庐江平移断裂系统[J]. 构造地质论丛, (3): 18~22.
[40]  徐九华, 谢玉玲, 申世亮. 1997. 小秦岭与胶东金矿床的成矿流体特征对比[J]. 矿床地质, 16(2): 149~162.
[41]  许文良, 王清海, 杨德彬, 等. 2004. 蚌埠荆山"混合花岗岩"SHRIMP 锆石U-Pb年龄及其地质意义[J]. 中国科学(D辑), 34(5): 423-428.
[42]  许志琴. 1984. 郯庐裂谷概述[J]. 构造地质论丛: (3): 39~46.
[43]  杨进辉, 周新华, 陈立辉. 2000. 胶东地区破碎蚀变岩型金矿时代的确定及其地质意义[J]. 岩石学报, 16(3): 454-458.
[44]  杨进辉, 朱美妃, 刘伟, 等. 2003. 胶东地区郭家岭花岗闪长岩的地球化学特征及成因[J]. 岩石学报, 19(4): 692~700.
[45]  杨敏之, 吕古贤. 1996. 胶东地区绿岩型金矿床地质地球化学[M]. 北京: 地质出版社.
[46]  姚凤良, 刘连登, 孔庆存, 等. 1990. 胶西北部脉状金矿[M]. 长春: 吉林科学技术出版社.
[47]  翟明国, 范宏瑞, 杨进辉, 等. 2004. 非造山带型金矿--胶东型金矿的陆内成矿作用[J]. 地学前缘, 11(1): 85~98.
[48]  翟裕生, 张湖, 宋鸿林, 等. 2000. 大型构造与超大型矿床[A]. 见: 涂光炽等著. 中国超大型矿床(1)[M]. 北京: 科学出版社. 136~152.
[49]  张德全, 徐洪林, 孙桂英. 1995. 山东邓格庄金矿与昆嵛山花岗岩的定位时代及其地质意义[J]. 地质论评, 41(5): 415~425.
[50]  张连昌, 沈远超, 刘铁兵, 等. 2002. 山东招莱盆地北缘金矿床Ar-Ar法和Rb-Sr法等时线年龄与成矿时代[J]. 中国科学(D辑): 32(9): 727~734.
[51]  张理刚, 王炳成. 1994. 焦家式金矿水-岩交换作用[J]. 矿床地质, 13(3): 193-200.
[52]  曹国权, 王致本, 张成基. 1990. 山东胶南地体及其边界断层五莲-荣成断裂的构造意义[J]. 山东地质, 6(1): 1~14.
[53]  陈丕基. 1988. 郯庐断裂巨大平移的时代与格局[J]. 科学通报, 33(4): 289~293.
[54]  胡世玲, 王松山, 桑海清, 等. 1987. 山东玲珑和郭家岭岩体同位素年龄及其地质意义[J]. 岩石学报, (3): 83~89.
[55]  胡受奚, 王鹤年, 王德滋, 等. 1998. 中国东部金矿地质学及地球化学[M]. 北京: 科学出版社. 27~49.
[56]  黄德业. 1994. 胶东金矿成矿系列硫同位素研究[J]. 矿床地质, 13(1): 75~87.
[57]  李厚民, 毛景文, 沈远超, 等. 2003. 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, 22(1): 72~77.
[58]  刘红涛, 孙世华, 刘建明, 等.2002. 华北克拉通北缘中生代高锶花岗岩类: 地球化学与源区性质[J]. 岩石学报, 18(3): 257~274.
[59]  刘建明, 叶杰, 徐九华, 等. 2003a. 胶东金矿床碳酸盐矿物的碳-氧和锶-钕同位素地球化学研究[J]. 岩石学报, 19(4): 775~784.
[60]  刘建明, 张宏福, 孙景贵, 等. 2003b. 山东幔源岩的碳-氧和锶-钕同位素地球化学研究[J]. 中国科学(D辑), 33: 921~930.
[61]  刘连登, 姚凤良, 孔庆存, 等. 1984. 岩脉在热液矿床成因中的意义--以胶东西北部金矿床为例[J]. 长春地质学院院报, (4): 13~28.
[62]  吕古贤, 孔庆存. 1993. 胶东玲珑-焦家式金矿地质[M]. 北京: 科学出版社.
[63]  卢焕章, J Guha, 方根保. 1999. 山东玲珑金矿的成矿流体特征[J]. 地球化学, 28(5): 421~437.
[64]  骆万成, 伍勤生. 1987. 应用蚀变矿物测定胶东金矿的成矿年龄[J]. 科学通报, 33(6): 1245~1248.
[65]  罗镇宽, 苗来成. 2002. 胶东招莱地区花岗岩和金矿床[M]. 北京: 冶金工业出版社.
[66]  张旗, 王焰, 钱青, 等. 2001. 中国东部埃达克岩的特征及其构造-成矿意义[J]. 岩石学报, 17(2): 236-244.
[67]  张振海, 张景鑫, 叶素芝. 1994. 胶东金矿同位素年龄厘定[M]. 北京: 地震出版社.
[68]  朱光, 刘国生, Dunlap W J, 等. 2004a. 郯庐断裂带同造山走滑的40Ar- 39Ar年代学证据[J]. 科学通报, 49(2): 190-198.
[69]  朱光, 王道轩, 刘国生, 等. 2004b. 郯庐断裂带的演化及对西太平洋板块运动的响应[J]. 地质科学, 39(1): 36-49.
[70]  马志红. 1991. 玲珑塑变花岗岩与金矿. 见:胶东金矿地质科技研讨会论文选编. 105~110(内部资料).
[71]  Liu J M, Zhang H F, Sun J G, et al. 2003b. Geochemical research on C-O and Sr-Nd isotopics of mantal-derived rocks from Shandong Province[J]. Science in China ( Series D), 33: 921 Series 930 (in Chinese).
[72]  Liu L D, Yao F L, Kong Q C, et al. 1984. The significance about the vein in the studing the genesis of hydrothermal ore deposits[J]. Journal of Changchun College of Geology, (4): 13~27 (in Chinese with English abstract).
[73]  Lu G X and Kong Q C. 1993. Geology on the Linglong-Jiaojia type golod deposits in the Jiaodong area, China[M]. Beijing: Science Press. 170~179 (in Chinese).
[74]  Lu H Z, J Guha and Fang G B. 1999. Characteristics of ore-formation fluid in Linglong gold mine, Shandong, China[J]. Geochemica, 28(5): 421~437 (in Chinese with English abstract).
[75]  Luo W C and Wu Q S. 1987. Application of alteration minerals to gold ore formation dating of Jiaodong, Shandong Province[J]. Chinese Bulletin Science, 32(6): 1245~1248 (in Chinese).
[76]  更多...
[77]  Luo Z K and Miao L C. 2002. Granites and gold diposits in the Zhaolai area, Eastern Shandong Privence[M]. Beijing: Mitallurgical Industry Press (in Chinese).
[78]  Simon A W and Zhang X O. 2002. Fundamention control on the timing and genesis of gold deposits in the Jiaodong Peninsula, North China Craton[A]. In: International Symposium on gold geology and exploration in Zhaoyuan, thg gold city of China [C]. Beijing: Seismological Press. 13~18.
[79]  Sun X X, Yi S X, Zeng Z X, et al. 1986. The fracture overlapping-compounding contact zone and its corntrol on the formation of hydrothermal fluid filling deposits[J]. Regional Geology of China, (3): 249~255 (in Chinese with English abstract).
[80]  Taylor W R, Rock N M S and Groves D I. 1993. Geochemistry of Archaean shoshonitic lamprophyres from the Yilgarn Block, Western Australia: Au abundance and association with gold mineralization[J]. Applied geochemistry, (9): 197~222.
[81]  Tu G C. 2000. The surperlarge deposits in China[M]. Beijing: Science Press. 91~94 (in Chinese).
[82]  Wan T F, Zhu H, Zhao L, et al. 1996. Formation and evolution of Tancheng-Lujiang fault zone: a review[J]. Geoscience, 10(2): 159~168 (in Chinese with English abstract) .
[83]  Wang X F, Li Z J, Chen B L, et.al. 2001. Tan-Lu fualt zone[M]. Beijing: Geol. Pub. House (in Chinese with English abstract).
[84]  Wang Y W. 1988. Lead isotope composition of gold deposits, North-western Jiaodong, Shandong, and its geological signification[J]. Journal of Changchun University of Earth Science, 18(3): 277~286 (in Chinese with English abstract).
[85]  Xu J W. 1984. Tancheng-Lujiang wrench fault system[J]. Collection of Structeral of Geology, (3): 18~22 (in Chinese).
[86]  Xu J W. 1992. Review of the ten years (1981~1991) of the Tancheng-Lujiang Fault Zone[J]. Geological Review, 38(4):316~325 (in Chinese with English abstract).
[87]  Xu J W. 1993. Tancheng-Lujiang wrench fualt system[M]. Chicheste: John Wiley & Sons Ltd. 17~149.
[88]  Xu J W, Zhu G and Tong W X. 1987. Formation and evolution of Tancheng-Lujiang wrench fault system: A major shear system to the norther of the Pacific Ocean[J]. Tectonophysics, 134: 273~310.
[89]  Xu J H, Xie Y L and Shen S L. 1997. A comparison of ore-formation fluids between gold deposits in Xiaoqingling Mountain and those deposits in Jiaodong Peninsula[J]. Mineral Deposits, 16(2): 149~162 (in Chinese with English abstract).
[90]  Xu W L, Wang Q H, Yang D B, et al. 2004. SHRIMP U-Pb zircon dating of the Jingshan "migmatized" granite, Bengbu, Anhui Province and their geological significance[J]. Science in China (Series D), 34(5): 423~428 (in Chinese).
[91]  Xu Z Q. 1984. Outline of Tan-Lu rift valley system[J]. Collection of Structural Geology, (3): 18~22 (in Chinese).
[92]  Yang J H, Zhou X H and Chen L H. 2000. Dating of gold mineralization for superlarge altered tectonite type gold deposits in the northwestern Jiaodong Peninsula and its implication for gold metallogeny [J]. Acta Petrologica Sinica, 16(3): 454~458 (in Chinese with English abstract).
[93]  Yang J H, Zhu M F, Liu W, et.al. 2003. Geochemistry and petrogenesis of Guojialing granodiorites from the northwestern Jiaodong Peninsula, eastern China[J]. Acta Petrologica Sinica, 19(4): 692~700 (in Chinese with English abstract).
[94]  Yang M Z and Lu G X. 1996. The geology-geochemistry of gold deposits of the greeston belt in the Jiaodong district, China[M]. Beijing: Geol. Pub. House (in Chinese with English abstract).
[95]  Yao F L, Liu L D, Kong Q C, et al. 1990. Vein gold deposits in northwestern Shandong Province[M]. Changchun: Jilin Science and Technongy Press (in Chinese).
[96]  Zhai M G, Fan H R, Yang J H, et al. 2004. Large-scale cluster of gold deposits in east Shandong: An orogenic metallogenesis[J]. Earth Science Frontiers, 11(1): 85~98 (in Chinese with English abstract).
[97]  Zhai Y S, Zhang H, Song H L, et al. 2000. Large stuctures and superlarge deposits[A]. In: Tu G C, eds. The surperlarge deposits in China [M]. Beijing: Science Press. 91~94 (in Chinese).
[98]  Zhang D Q, Xu H L and Sun G Y. 1995. Emplament ages of the Denggezhuang gold depodit and the Kunyushan granite and their geologecal implication[J]. Geological Review, 41(5): 415~425 (in Chinese with English abstract).
[99]  Zhang L C, Shen Y C, Liu T B, et al. 2002. Ar-Ar and Rb-Sr isochron ages and ore-forming time for gold deposits in northern margin of Zhaolai basin, Shandong Province [J]. Science in China (Series D), 32(9): 727~734 (in Chinese).
[100]  Zhang L G and Wang B C. 1994. Water-rock exchenge in the Jiaojia type gold deposits, a study of hydrogen and oxygen isotopic composition of ore-forming fluids[J]. Mineral Deposits, 13(4): 193~200 (in Chinese with English abstract).
[101]  Zhang Q, Wang Y, Qian Q, et al. 2001. The characteristics and tectinic-metalloginic signification of the edakites in the Yanshan period from eastern China[J]. Acta Petrologica Sinica, 17(2): 236~244 (in Chinese with English abstract).
[102]  Zhang Z H, Zhang J X and Ye S Z. 1994. Isotopic dating of gold deposits in East Shandong Province[M]. Beijing: Seismological Press (in Chinese).
[103]  Zhu G, Liu G S, Dunlap W J, et al. 2004a. 40Ar-39Ar thermchronology evidence on synorogic strike-slip motion of Tan-Lu fault zone[J]. Chinese Science Bulletin, 49(2): 190~198 (in Chinese).
[104]  Zhu G, Wang D X, Liu G S, et al. 2004b. Evolution of the Tan-Lu fault zone and its responses to plate movements in West Pacific Basin[J]. Chinese Journal of Geology, 39(1): 36~49 (in Chinese with English abstract).
[105]  曹国权. 1990. 试论胶南地体[J]. 山东地质, 6 (2): 1~9.

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