Journal of Jilin University(Earth Science Edition) ›› 2016, Vol. 46 ›› Issue (4): 1100-1123.doi: 10.13278/j.cnki.jjuese.201604111

Previous Articles     Next Articles

Poly-Metal Mineralization and Exploration Potential in Southern Segment of the Da Hinggan Mountains

Zeng Qingdong, Liu Jianming, Chu Shaoxiong, Guo Yunpeng, Gao Shuai, Guo Lixiang, Zhai Yuanyuan   

  1. Key Laboratory of Mineral Resources/Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
  • Received:2016-04-06 Online:2016-07-26 Published:2016-07-26
  • Supported by:

    Supported by National Key Basic Research Program Project (2013 CB429804) and National Natural Science Foundating of China(41390443)

Abstract:

The southern segment poly-metal metallogenic belt of the Da Hinggan Mountains (DHM) is located at the area between the Hegenshan fault and the Xilamulun fault in eastern Central Asia Orogenic belt, and also situated the superposition area caused by the paleo-Asia ocean tectonic system and paleo-Pacific ocean tectonic system. The southern segment poly-metal metallogenic belt of DHM is characterized by the bilayer structure (Permian basement,Jurassic-Early Cretaceous covers), poly-stage tectonic-magma activities and numerous poly-metal deposits. The metal deposits are characterized by the associated poly elements. The metal deposits can be classified to four ore-forming system by the mineralization features: porphyry, skarn, hydrothermal vein and alkaline granite ore-forming systems. Porphyry ore-forming system includes Mo-poly metal and Sn-poly metal subsystems, skarn ore-forming system includes Fe-Sn and Pb-Zn-Ag subsystems, hydrothermal vein ore-forming system includes Ag-poly metal, Cu-poly metal and Sn-poly metal subsystems. Alkaline granite ore-forming system is the rare and rare earth metal ore-forming system. The metal deposits in southern segment of DHM were mainly formed in two periods: Late Permian to Triassic and Late Jurassic to Early Cretaceous. Both periods mineralization is related to the granitic magmatism. The ore-forming materials were derived from multi-sources which including deep and strata sources. The Late Permian and Triassic poly metal deposits were formed in the paleo-Asia tectonic setting, the Late Jurassic and Early Cretaceous poly metal deposits were formed in the paleo-Pacific tectonic setting. The favorable metallogenic geological conditions, the good geophysical and geochemical anomalies indicate that the southern segment has still huge exploration potential.

Key words: nonferrous metal, poly-metal deposit, ore-forming system, superposition, Mesozoic, southern segment of the Da Hinggan Mountains

CLC Number: 

  • P618. 4

[1] 刘建明,张锐,张庆洲.大兴安岭地区的区域成矿特征[J]. 地学前缘, 2004, 11(1): 269-277. Liu Jianming, Zhang Rui, Zhang Qingzhou. The Regional Metallogeny of the Da Hinggan Ling, China[J]. Earth Science Frontiers, 2004, 11(1): 269-277.

[2] Zeng Q D, Liu J M, Yu C M, et al. Metal Deposits in the Da Hinggan Mountains, NE China: Styles, Characteristics, and Exploration Potential[J]. International Geology Review, 2011, 53(7): 846-878.

[3] Zeng Q D, Liu J M, Qin K Z, et al. Types, Characteristics, and Time-Space Distribution of Molybdenum Deposits in China[J]. International Geology Review, 2013, 55(11): 1311-1358.

[4] Zeng Q D, Sun Y, Chu S X, et al. Geochemistry and Geochronology of the Dongshanwan Porphyry Mo-W Deposit, Northeast China: Implications for the Late Jurassic Tectonic Setting[J]. Journal of Asian Earth Sciences, 2015, 97: 472-485.

[5] Zeng Q D, Qin K Z, Liu J M, et al. Porphyry Molybdenum Deposits in the Tianshan-Xingmeng Orogenic Belt, Northern China[J]. International Journal of Earth Science, 2015, 104(4): 991-1023.

[6] 芮宗瑶,施林道,方如恒.华北陆块北缘及邻区有色金属矿床地质[M].北京:地质出版社, 1994. Rui Zongyao, Shi Lindao, Fang Ruheng. Geology and Nonferrous Metallic Deposits in the Northern Margin of the North China Landmass and Its Adjacent Area[M]. Beijing: Geological Publishing House, 1994.

[7] Ouyang H, Wu X L, Mao J W, et al. The Nature and Timing of Ore Formation in the Budunhua Copper Deposit, Southern Great Xing'an Range: Evidence from Geology, Fluid Inclusions, and U-Pb and Re-Os Geochronology[J]. Ore Geology Reviews, 2014, 63: 238-251.

[8] 李文国, 李庆富, 姜万德. 内蒙古自治区岩石地层[M]. 武汉:中国地质大学出版社, 1996. Li Wenguo, Li Qingfu, Jiang Wande. Lithostratigraphy in Inner Mongolia[M]. Wuhan: China University of Geosciences Press, 1996.

[9] 鲍庆中, 张长捷, 吴之理, 等. 内蒙古东南西乌珠穆沁旗地区石炭纪二叠纪岩石地层和层序地层[J]. 地质通报, 2006, 25(5): 572-579. Bao Qingzhong, Zhang Changjie, Wu Zhili, et al. Carboniferous-Permian Marine Lithostratigraphy and Sequence Stratigraphy in Xi Ujimqin Qi, Southeastern Inner Mongolia, China[J]. Geological Bulletin of China, 2006, 25(5): 572-579.

[10] 黄本宏. 大兴安岭地区石炭、二叠系植物群[M]. 北京: 地质出版社, 1993. Huang Beihong. Carboniferous and Permian Flora in Da Hinggan Mountains[M]. Beijing: Geological Publishing House, 1993.

[11] 邵济安,张履桥,牟保垒,等.大兴安岭的隆起与地球动力学背景[M]. 北京: 地质出版社, 2007. Shao Ji'an, Zhang Lüqiao,Mu Baolei, et al.The Uplift of Daxinganling and Its Geodynamic Setting[J].Beijing: Geological Publishing House, 2007.

[12] 内蒙古自治区地质矿产局.内蒙古自治区区域地质志[M] .北京:地质出版社, 1991. Bureau of Geology and Mineral Resources of Nei Mongol Autonomous Region. Regional Geology Records of Nei Mongol Autonomous Region[M]. Beijing: Geological Publishing House, 1991.

[13] 王友,樊志勇,方曙,等.西拉木伦河北岸新发现地质资料及其构造意义[J].内蒙古地质,1999 (1):6-28. Wang You, Fan Zhiyong, Fang Shu, et al. Geological Information Were Discovered and Their Plate Tectonic Significance on the Northern Bank of Xarmoron River[J].Inner Mongolia Geology, 1999 (1): 6-28.

[14] 李春昱,汤耀庆. 亚洲古板块划分以及有关问题[J]. 地质学报,1983(1):1-10. Li Chunyu, Tang Yaoqing. Some Problems on Subdivision of Paleo-Plates in Asia[J]. Acta Geologica Sinica, 1983 (1): 1-10.

[15] 杨宝俊, 唐建人, 李勤学,等. 松辽盆地隆起区地壳反射结构与" 断开" 莫霍界面[J]. 中国科学:D辑, 2003, 33(2): 170-176. Yang Baojun, Tang Jianren, Li Qinxue, et al. Crustal Reflection Structure in the Uplifting Zone of Songliao Basin and Disconnecting Moho Interface[J]. Science in China: Series D, 2003, 33(2): 170-176.

[16] 杨宝俊, 刘万扁, 王喜臣, 等. 中国东部大兴安岭重力梯级带域地球物理场特征及其成因[J]. 地球物理学报, 2005 , 4 8 (1): 86-97. Yang Baojun, Liu Wanbian, Wang Xichen, et al. Geophysical Characteristics of Daxinganling Gravitational Gradient Zone in the East China and Its Geodynamic Mechanism[J]. Chinese Journal Geophysics, 2005, 48(1): 86-97.

[17] 徐备, 陈斌. 内蒙古北部华北板块与西拍利亚板块之间中古生代造山带的结构及演化[J]. 中国科学:D辑, 1997, 27(3): 227-232. Xu Bei, Chen Bin. Framework and Evolution of the Middle Paleozoic Orogenic Belt Between Siberia and North China Plates in Northern Inner Mongolia[J]. Science in China: Series D, 1997, 27(3): 227-232.

[18] 刘财, 杨宝俊, 王兆国,等. 松辽盆地西边界带深部构造:地电学证据[J].地球物理学报, 2011, 54(2): 401-406. Liu Cai, Yang Baojun, Wang Zhaoguo, et al. The Deep Structure of the Western Boundary Belt of the Songliao Basin: The Geoelectric Evidence[J]. Chinese Journal Geophysics, 2011, 54(2): 401-406.

[19] Wu F Y, Sun D Y, Ge W C, et al. Geochronology of the Phanerozoic Granitoids in Northeastern China[J]. Journal of Asian Earth Sciences, 2011, 41: 1-30.

[20] Zeng Q D, Sun Y, Duan X X, et al. U-Pb and Re-Os Geochronology of the Haolibao Porphyry Mo-Cu Deposit, NE China: Implications for a Late Permian Tectonic Setting[J]. Geological Magazine, 2013, 150(6): 975-985.

[21] 曾庆栋,刘建明,褚少雄,等. 西拉沐伦成矿带中生代花岗岩浆活动与钼成矿作用[J]. 吉林大学学报(地球科学版), 2011,41(6): 1705-1714. Zeng Qingdong Liu Jianming, Chu Shaoxiong, et al. Mesozoic Granitic Magmatism and Molybdenum Ore-Forming Process in the Xilamulun Metallogenic Belt[J]. Journal of Jilin University (Earth Science Edition), 2011, 41(6): 1705-1714.

[22] 江思宏, 聂凤军, 白大明, 等. 内蒙古白音诺尔铅锌矿床印支期成矿的年代学证据[J].矿床地质,2011, 30 (5): 787-799. Jiang Sihong, Nie Fengjun, Bai Daming, et al. Geochronology Evidence for Indosinian Mineralization in Baiyinnuoer Pb-Zn Deposit of Inner Mongolia[J]. Mineral Deposits, 2011, 30(5):787-799.

[23] Zeng Q D, Liu J M, Chu S X, et al. Mesozoic Molybdenum Deposits in the East Xingmeng Orogenic Belt, Northeast China: Characteristics and Tectonic Setting[J]. International Geology Review, 2012, 54(16):1843-1869.

[24] Duan X X, Zeng Q D, Yang Y H, et al. Triassic Magmatism and Mo Mineralization in Northeast China: Geochronological and Isotopic Constraints from the Laojiagou Porphyry Mo Deposit[J]. International Geology Review, 2015, 57(1): 55-75.

[25] 郭志军,周振华, 李贵涛,等.内蒙古敖尔盖铜矿中-酸性侵入岩体SHRIMP锆石U-Pb 定年与岩石地球化学特征研究[J].中国地质,2012,39(6): 1487-1500. Guo Zhijun, Zhou Zhenhua, Li Guitao, et al. SHRIMP U-Pb Zircon Dating and Petrogeochemistral Characteristics of the Intermediate-Acid Intrusive Rocks in the Aoergai Copper Deposit of Inner Mongolia[J]. Geology in China, 2012, 39(6): 1487-1500.

[26] Zeng Q D, Guo W K, Chu S X, et al. Late Jurassic Granitoids in the Xilamulun Mo Belt, Northeastern China: Geochronology, Geochemistry, and Tectonic Implications[J]. International Geology Review, 2015, DOI: 10.1080/00206814.2015.1099479.

[27] Zeng Q D, Liu J M, Zhang Z L. Re-Os Geochronology of Porphyry Molybdenum Deposit in South Segment of Da Hinggan Mountains, Northeastern China[J]. Journal of Earth Sciences, 2010, 21(4): 390-401.

[28] Zeng Q D, Yang J H, Zhang Z L, et al. Petrogenesis of the Yangchang Mo-Bearing Granite in the Xilamulun Metallogenic Belt, NE China: Geochemistry, Zircon U-Pb Ages, and Sr-Nd-Pb Isotopes[J]. Geological Journal, 2014, 49: 1-14.

[29] 吴冠斌, 刘建明, 曾庆栋,等. 内蒙古大兴安岭双尖子山铅锌银矿床成矿年龄[J]. 矿物学报, 2013,33(增刊):619. Wu Guanbin, Liu Jianming, Zeng Qingdong, et al. The Ore-Forming Age of the Shuangjianzishan Pb-Zn-Ag Deposit in Da Hinggan Mountains, Inner Mongolia[J]. Acta Mineralogica Sinica, 2013,33 (Sup.): 619.

[30] 王喜龙, 刘家军, 翟德高,等. 内蒙古边家大院铅锌银矿区侵入岩LA-ICP-MS锆石U-Pb年龄、地球化学特征及其地质意义[J]. 大地构造与成矿学, 2013, 37(4):730-742. Wang Xilong, Liu Jiajun, Zhai Degao, et al. LA-ICP-MS Zircon U-Pb Dating, Geochemistry of the Intrusive Rocks from the Bianjiadayuan Pb-Zn-Ag Deposit, Inner Mongolia, China and Tectonic Implications[J]. Geotectonica et Metallogenia, 2013, 37(4): 730-742.

[31] 刘翼飞,樊志勇,蒋胡灿,等.内蒙古维拉斯托拜仁达坝斑岩-热液脉状成矿体系研究[J].地质学报,2014,88(12): 2373-2385. Liu Yifei, Fan Zhiyong, Jiang Hucan, et al. Genesis of the Weilasituo-Bairendaba Porphyry-Hydrothermal Vein Type System in Inner Mongolia, Chin[J].Acta Geologica Sinica, 2014, 88(12): 2373-2395.

[32] 周振华,吕林素,冯佳睿,等. 内蒙古黄岗夕卡岩型锡铁矿床辉钼矿Re-Os年龄及其地质意义[J].岩石学报, 2010, 26(3): 667-679. Zhou Zhenhua, Lǜ Linsu, Feng Jiarui, et al. Molybdenite Re-Os Ages of Huanggang Skarn Sn-Fe Deposit and Their Geological Significance, Inner Mongolia[J]. Acta Petrologica Sinica, 2010, 26(3): 667-679.

[33] 赵一鸣,王大畏,张德全,等.内蒙古东南部铜多金属成矿地质条件及找矿模式[M].北京:地震出版社,1994. Zhao Yiming, Wang Dawei, Zhang Dequan, et al. Ore-Controlling Factors and Ore-prospecting Models for Copper-Polymetallic Ore Deposits in Southeastern Inner Mongolia[M].Beijing:Seismological Publishing House, 1994.

[34] 王国政.内蒙古安乐锡铜矿产地质特征及成因[J]. 矿床地质, 1997,16(3): 260-271. Wang Guozheng. Geological Characteristics and Genesis of the Anle Tin-Copper Deposit, Inner Mongolia[J]. Mineral Deposits, 1997, 16(3): 260-271.

[35] Wu H Y, Zhang L C, Wan B, et al. Geochronological and Geochemical Constraints on Aolunhua Porphyry Mo-Cu Deposit, Northeast China, and Its Tectonic Significance[J].Ore Geology Reviews, 2011, 43: 78-91.

[36] 郭利军, 谢玉玲, 侯增谦, 等. 内蒙古拜仁达坝银多金属矿矿床地质及成矿流体特征[J]. 岩石矿物学杂志, 2009, 28(1):26-36. Guo Lijun, Xie Yuling, Hou Zengqian, et al. Geology and Ore Fluid Characteristics of the Bairendaba Silver Polymetallic Deposit in Inner Mongolia[J]. Acta Petrologica et Mineralogica, 2009, 28(1):26-36.

[37] 江思宏, 聂凤军, 刘翼飞, 等. 内蒙古拜仁达坝及维拉斯托银多金属矿床的硫和铅同位素研究[J]. 矿床地质, 2010, 29(2):101-112. Jiang Sihong, Nie Fengjun, Liu Yifei, et al. Sulfur and Lead Isotopic Compositions of Bairendaba and Weilasituo Silver-Polymetallic Deposits, Inner Mongolia[J].Mineral Deposits, 2010,29(2):101-112.

[38] 孙丰月, 王力.内蒙古拜仁达坝银铅锌多金属矿床成矿条件[J]. 吉林大学学报(地球科学版), 2008, 38(3):269-276. Sun Fengyue, Wang Li. Ore-Forming Conditions of Bairendaba Ag-Pb-Zn Polymetallic Ore Deposit, Inner Mongolia[J]. Journal of Jilin University (Earth Science Edition), 2008, 38 (3): 269-276.

[39] 郭令芬.内蒙古花敖包特银铅锌多金属矿床地球化学及成因研究[D]. 北京:中国地质大学, 2010. Guo Lingfen. Geochemical Characteristics and Genesis of the Huaaobaote Silver-Lead-Zic Polymetaalic Deposit, Inner Mongolia, China[D]. Beijing :China University of Geosciences, 2010.

[40] 潘小菲, 郭利军, 王硕, 等.内蒙古维拉斯托铜锌矿床的白云母39Ar/40Ar年龄探讨[J]. 岩石矿物学杂志, 2009, 28(5):473-479. Pan Xiaofei, Guo Lijun, Wang Shuo, et al. Laser Microprobe Ar-Ar Dating of Biotite from the Weilasituo Cu-Zn Polymetallic Deposit in Inner Mongolia[J]. Acta Petrologica et Mineralogica, 2009, 28(5): 473-479.

[41] 储雪蕾,霍卫国,张巽.内蒙古林西县大井铜多金属矿床的硫、碳和铅同位素及成矿物质来源[J].岩石学报, 2002, 18(4): 566-574. Chu Xuelei, Huo Weiguo, Zhang Xun. S, C, and Pb Isotopes and Sources of Metallogenetic Elements of the Dajing Cu-Polymetallic Deposit in Linxi County, Inner Mongolia, China[J]. Acta Petrologica Sinica, 2002, 18(4): 566-574.

[42] 王玉往,王京彬,龙灵利,等.内蒙古大井矿床成矿作用[M].北京:科学出版社,2014. Wang Yuwang, Wang Jingbin, Long Lingli, et al. Metallogeny of the Dajing Deposit, Inner Mongolia[M]. Beijing: Science Press, 2014.

[43] 冯建忠,艾霞,吴俞斌,等.内蒙大井多金属矿床稳定同位素地球化学特征[J].吉林地质,1994,13(3): 60-66. Feng Jianzhong, Ai Xia, Wu Yubin, et al. The Stable Isotopic Geochemistry of the Dajing Poly Metallic Deposit, Inner Mongolia[J]. Jilin Geology, 1994, 13(3): 60-66.

[44] 徐佳佳, 赖勇,崔栋,等.内蒙古道伦达坝铜多金属矿床成矿流体特征及其演化[J]. 岩石学报,2009, 25(11): 2957-2972. Xu Jiajia,Lai Yong,Cui Dong,et al.Characteristics and Evolution of Ore-Forming Fluids of the Daolundaba Copper-Poly-Metal Deposit, Inner Mongolia[J]. Acta Petrologica Sinica, 2009, 25(11): 2957-2972.

[45] 潘小菲, 王硕, 侯增谦, 等.内蒙古道伦达坝铜多金属矿床特征研究[J].大地构造与成矿学, 2009,33(3): 402-410. Pan Xiaofei, Wang Shuo, Hou Zengqian, et al. Geology and Metallogenesis of Daolundaba Copper Polymetallic Deposits, Inner Mongolia[J]. Geotectonica et Metallogenia, 2009, 33(3): 402-410.

[46] Zeng Q D, Liu J M, Liu H T. Geology and Geochemistry of the Bianbianshan Au-Ag-Cu-Pb-Zn Deposit, Southern Da Hinggan Mountains, Northeastern China[J]. Acta Geologica Sinica (English Edition), 2012, 86(3): 630-639.

[47] 王国政.宝盖沟锡矿:黑英岩钠长岩型高温热液矿床[J]. 地质与勘探,2002,38(2): 42-45. Wang Guozheng. Baogaigou Tin Deposit-A Higher Temperature Hydrothermal Deposit of Albitite and Biotite Quartzite Types[J]. Geology and Prospecting, 2002, 38(2): 42-45.

[48] 沈存利,高有库,张天平,等.内蒙古罕山林场铜银锡多金属矿床的发现及意义[J]. 矿产勘查,2013,4(5): 475-484. Shen Cunli, Gao Youku, Zhang Tianping, et al. Discovery of the Hanshanlinchang Cu-Ag-Sn Polymetallic Deposit and Its Significance for Prospecting, Inner Mongolia[J].Mineral Exploration, 2013, 4(5): 475-484.

[49] Zeng Q D, Liu J M, Zhang Z L, et al. Geology and Lead-Isotope Study of the Baiyinnuoer Zn-Pb-Ag Deposit, South Segment of the Da Hinggan Mountains, Northeastern China[J]. Resource Geology, 2009, 59(2): 170-180.

[50] 张德全, 雷蕴芬, 罗太阳, 等. 内蒙古白音诺铅锌矿床地质特征及成矿作用[J]. 矿床地质, 1991, 10(3):204-216. Zhang Dequan, Lei Yunfen, Luo Taiyang, et al. Geological Characteristics and Metallogeny of the Baiyinnuoer Lead-Zinc Deposit, Inner Mongolia[J]. Mineral Deposits, 1991, 10(3): 204-216.

[51] 李剑锋, 王可勇, 陆继胜,等.内蒙古红岭铅锌矿床成矿流体地球化学特征及矿床成因[J]. 地球科学:中国地质大学学报,2015,40(6): 995-1005. Li Jianfeng, Wang Kengyong, Lu Jisheng, et al. Ore-Forming Fluid Geochemical Characteristics and Genesis of Pb-Zn Deposit in Hongling, Inner Mongolia[J].Earth Science:Journal of China University of Geosciences, 2015, 40(6): 995-1005.

[52] 翟德高,刘家军,杨永强,等.内蒙古黄岗梁铁锡矿床成岩、成矿时代与构造背景[J]. 岩石矿物学杂志,2012, 31(4): 513-523. Zhai Degao, Liu Jiajun, Yang Yongqiang, et al. Petrogenetic and Metallogentic Ages and Tectonic Setting of the Huanggangliang Fe-Sn Deposit, Inner Mongolia[J]. Acta Petrologica et Mineralogica, 2012, 31(4): 513-523.

[53] 牛贺才,单强,罗勇,等.巴尔哲超大型稀有稀土矿床富晶体的流体包裹体的初步研究[J].岩石学报,2008,24(9): 2149-2154. Niu Hecai, Shan Qiang, Luo Yong, et al. Study on the Crystal-Rich Fluid Inclusions from the Baerzhe Super-Large Rare Elements and REE Deposit[J]. Acta Petrologica Sinica, 2008, 24(9): 2149-2154.

[54] 杨武斌,牛贺才,单强,等.巴尔哲超大型稀有稀土矿床成矿机制研究[J].岩石学报,2009, 25(11): 2924-2932. Yang Wubin, Niu Hecai, Shan Qiang, et al. Ore-Forming Mechanism of the Baerzhe Super-Large Rare and Rare Earth Elements Deposits[J]. Acta Petrologica Sinica, 2009, 25(11): 2924-2932.

[55] 杨武斌,单强,赵振华, 等. 巴尔哲地区碱性花岗岩的成岩和成矿作用:矿化和未矿化岩体的比较[J]. 吉林大学学报(地球科学版),2011, 41(6): 1689-1704. Yang Wubin, Shan Qiang, Zhao Zhenhua, et al. Petrogenic and Metallogenic Action of the Alkaline Granitoids in Baerzhe Area: A Comparison Between Mineralized and Barren Plutons[J]. Journal of Jilin University (Earth Science Edition), 41 (6): 1689-1704.

[56] 王喜龙,刘家军,翟德高,等.内蒙古边家大院矿区石英斑岩年代学、岩石地球化学特征及其地质意义[J].矿物岩石地球化学通报,2014, 33(5):654-663. Wang Xilong, Liu Jiajun, Zhai Degao, et al. U-Pb Dating, Geochemistry and Tectonic Implications of Bianjiadayuan Quartz Porphyry, Inner Mongolia, China[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 2014, 33(5): 654-663.

[57] 王喜龙,刘家军,翟德高,等.内蒙古林西边家大院银多金属矿床同位素地球化学特征及成矿物质来源探讨[J].中国地质, 2014, 41(4): 1288-1303. Wang Xilong, Liu Jiajun, Zhai Degao, et al. A Study of Isotope Geochemistry and Sources of Ore-Forming Materials of the Bianjiadayuan Silver Polymetallic Deposit in Linxi, Inner Mongolia[J]. Geology in China, 2014, 41(4): 1288-1303.

[58] 王宇, 蔡彤, 包乃柱,等.内蒙古边家大院铅锌银矿地质特征和控矿因素[J]. 东华理工大学学报(自然科学版), 2014, 37(2):212-219. Wang Yu, Cai Tong, Bao Naizhu, et al. Geological Characteristic and Control Factors in Bianjiadayuan Pb-Zn-Ag Deposit, Inner Mongolia[J]. Journal of East China Institute of Technology(Natural Science), 2014, 37(2): 212-219.

[59] 郑翻身, 蔡红军, 张振法. 内蒙古拜仁达坝维拉斯托超大型银铅锌矿的发现及找矿意义[J]. 物探与化探, 2006, 30(1):13-25. Zheng Fanshen, Cai Hongjun, Zhang Zhenfa. Discovery of Superlarge Silver-Lead-Zinc Deposits in Bairendaba and Weilasituo, Inner Mongolia, and Its Ore-Prospecting Significance[J]. Geophysical and Geochemical Exploration, 2006, 30(1): 13-25.

[60] 郭利军,葛昌宝,冯贞,等. 内蒙古锡林浩特东部拜仁达坝银铅多金属矿勘查过程及远景评述[J]. 物探与化探, 2004, 28(5):394-401. Guo Lijun, Ge Changbao, Feng Zhen, et al. The Exploration Process and Prospects of the Bairendaba Ag-Pb Polymetallic Deposit in Eastern Xilin Hot, Inner Mongolia[J]. Geophysical and Geochemical Exploration, 2004, 28(5): 394-401.

[61] 欧阳荷根.大兴安岭南段拜仁达坝-维拉斯托银多金属矿床成矿作用及动力学背景[D]. 北京:中国地质大学(北京), 2013. Ouyang Hegen. Metallogenesis of Bairendaba-Weilasituo Silver-Polytmetallic Deposit and Its Geodynamic Setting, in the Southern Segment of Great Xing'an Range, NE China[D]. Beijing :China University of Geosciences (Beijing), 2013.

[62] 钟日晨, 杨永飞, 石英霞, 等. 内蒙古拜仁达坝银多金属矿区矿石矿物特征及矿床成因[J]. 中国地质, 2008, 35(6): 1274-1285. Zhong Richen, Yang Yongfei, Shi Yingxia, et al. Ore Characters and Ore Genesis of the Bairendaba Ag Polymetallic Ore Deposit in Keshiketeng Banner, Inner Mongolia[J]. Geology in China, 2008, 35(6): 1274-1285.

[63] 常勇, 赖勇.内蒙古银都银铅锌多金属矿床成矿流体特征及成矿年代学研究[J]. 北京大学学报(自然科学版), 2010, 46(4): 581-593. Chang Yong, Lai Yong. Study on Characteristics of Ore-Forming Fluid and Chronology in the Yindu Ag-Pb-Zn Polymetallic Ore Deposit, Inner Mongolia[J]. Acta Scientiarum Naturalium Universitatis Pekinesis, 2010, 46(4): 581-593.

[64] 储雪蕾,刘伟. 大井铜-锡多金属矿床成矿作用与岩浆流体的关系[J]. 地质论评,1999, 45(增刊1): 1166-1172. Chu Xuelei,Liu Wei. The Relationship Between Mineralization of the Dajing Cu-Sn Polymetallic Deposit and Magmatic Fluid[J]. Geological Review,1999,45(Sup.l): 1166-1172.

[65] 王玉往,王京彬,龙灵利,等.内蒙古大井矿床成矿作用[M].北京:科学出版社,2014. Wang Yuwang, Wang Jingbin, Long Lingli, et al. Metallogenesis of the Dajing Deposit, Inner Mongolia[M]. Beijing: Science Press, 2014.

[66] 江思宏,梁清玲,刘翼飞,等.内蒙古大井矿区及外围岩浆岩锆石U-Pb 年龄及其对成矿时间的约束[J]. 岩石学报,2012, 28(2):495-513. Jiang Sihong,Liang Qingling,Liu Yifei, et al. Zircon U-Pb Ages of the Magmatic Rocks Occurring in and Around the Dajing Cu-Ag-Sn Polymetallic Deposit of Inner Mongolia and Constrains to the Ore-Forming Age[J]. Acta Petrologica Sinica,2012,28(2):495-513.

[67] 廖震, 王玉往,王京彬, 等.内蒙古大井锡多金属矿床岩脉LA-ICP-MS锆石U-Pb定年及其地质意义[J]. 岩石学报,2012, 28(7):2292-2306. Liao Zhen,Wang Yuwang,Wang Jingbin,et al.LA-ICP-MS Zircon U-Pb Dating of Dykes of Dajing Tin-Polymetallic Deposit,Inner Mongolia,China,and Its Geological Significance[J].Acta Petrologica Sinica,2012, 28(7): 2292-2306.

[68] 艾永富,张晓辉.内蒙大井矿床的脉岩与成矿[C]//中国地质学会编."八五"地质科技重要成果学术交流会议论文集.北京:冶金工业出版社,1996: 231-234. Ai Yongfu, Zhang Xiaohui. The Dykes and Metallogenesis of the Dajing Deposit, Inner Mongolia[C]// Geological Society of China.The Academic Exchange Conference Proceedings of the Important Achievement of the Geological Science and Technology in Eighth Five Program. Beijing: Metallurgical Industry Press,1996: 231-234.

[69] 曾庆栋,刘建明,万志民,等.内蒙古赤峰市白音诺尔铅锌矿床构造控制与找矿方向[J].大地构造与成矿,2007,31(4): 430-434. Zeng Qingdong, Liu Jianming, Wan Zhimin, et al. Structural Controls and Exploration Targets of the Baiyinnuoer Zinc-Lead Deposit, Chifeng, Inner Mongolia[J]. Geotectonica et Metallogenia, 2007, 31(4): 430-434.

[70] 周振华,刘宏伟,常帼雄,等.内蒙古黄岗锡铁矿床夕卡岩矿物学特征及其成矿指示意义[J]. 岩石矿物学杂志,2011, 30(1): 97-112. Zhou Zhenhua, Liu Hongwei, Chang Guoxiong, et al. Mineralogical Characteristics of Skarns in the Huanggang Sn-Fe Deposit of Inner Mongolia and Their Metallogenic Indicating Significance[J]. Acta Petrologica et Mineralogica, 2011, 30(1): 97-112.

[71] 王莉娟, 王京彬, 王玉往,等.内蒙黄岗梁矽卡岩型铁锡矿床稀土元素地球化学[J]. 岩石学报,2002, 18(4):575-584. Wang Lijuan, Wang Jingbin, Wang Yuwang, et al. REE Geochemistry of the Huangguangliang Skarn Fe-Sn Deposit, Inner Mongolia[J]. Acta Petrologica Sinica, 2002, 18(4):575-584.

[72] 叶杰,刘建明,张安立,等.沉积喷流型矿化的岩石学证据:以大兴安岭南段黄岗和大井矿床为例[J]. 岩石学报,2002, 18(4): 589-592. Ye Jie, Liu Jianming, Zhang Anli, et al. Petrological Evidence for Exhalative Mineralization: Case Studies of Huanggang and Dajing Deposits in the Southern Segment of the Da Hinggan Mountains, China[J]. Acta Petrologica Sinica, 2002, 18(4): 585-592.

[73] 王长明,张寿庭,邓军,等.内蒙古黄岗梁锡铁多金属矿床层状夕卡岩的喷流沉积成因[J]. 岩石矿物学杂志, 2007, 26(5): 409-417. Wang Changming, Zhang Shouting, Deng Jun. et al. The Exhalative Genesis of the Stratabound Skarn in the Huanggangliang Sn-Fe Polymetallic Deposit of Inner Mongolia[J]. Acta Petrologica et Mineralogica, 2007, 26(5): 409-417.

[74] Wang J B, Wang Y W, Wang L J, et al. Tin-Polymetallic Mineralization in the Southern Part of the Da Hinggan Mountains, China[J]. Resource Geology, 2001,51(4): 283-291.

[75] 刘伟, 李新俊, 谭骏. 内蒙古大井铜-锡-银-铅-锌矿床的流体混合作用:流体包裹体和稳定同位素证据[J]. 中国科学:D辑, 2002,32(5): 405-414. Liu Wei, Li Xinjun, Tan Jun. Fluid Mixing of the Dajing Cu-Sn-Ag-Pb-Zn Deposit, Inner Mongolia:Evidences from the Fluid Inclusions and Stable Isotopes[J]. Science in China :Series D, 2002, 32(5):405-414.

[76] 周振华.内蒙古黄岗锡铁矿床地质与地球化学[D]. 北京:中国地质科学院,2011. Zhou Zhenhua. Geology and Geochemistry of the Hanggan Sn-Fe Deposit, Inner Mongolia[D]. Beijing: Chinese Academy of Geological Sciences, 2011.

[77] 马星华,陈斌.大兴安岭南段敖仑花斑岩钼(铜)矿床成矿流体来源与成矿作用:稳定同位素C、H、O、S和放射性Pb同位素约束[J]. 吉林大学学报(地球科学版), 2011,41(6): 1770-1784. Ma Xinghua, Chen Bin. The Source of Hydrothermal Fluids and Mineralization in the Aolunhua Porphyry Mo-Cu Deposit, Southern Da Hinggan Mountains: Constraint from Stable (C, H, O and S) and Radiogenic (Pb) Isotopes[J]. Journal of Jilin University (Earth Science Edition), 2011, 41(6):1770-1784.

[78] 武新丽, 毛景文, 周振华,等.大兴安岭中南段布敦化铜矿床H-O-S-Pb同位素特征及成矿指示[J]. 中国地质,2012,39(6):1812-1829. Wu Xinli, Mao Jingwen, Zhou Zhenhua, et al. H-O-S-Pb Isotopic Components of the Budunhua Cu Deposit in the Middle South Part of the Da Hinggan Mountains and Their Implications for the Ore-Forming Process[J]. Geology in China, 2012, 39(6):1812-1829.

[79] Zhu X Q, Zhang Q, He Y L, et al. Hydrothermal Source Rocks of the Meng'entaolegai Ag-Pb-Zn Deposit in the Granite Batholith, Inner Mongolia, China[J].Geochemical Journal, 2006, 40(3): 265-275.

[80] 曾庆栋,刘建明,贾长顺, 等.内蒙古赤峰市白音诺尔铅锌矿沉积喷流成因:地质和硫同位素证据[J].吉林大学学报(地球科学版),2007, 37(4):659-667. Zeng Qingdong, Liu Jianming, Jia Changshun, et al. Sedimentary Exhalative Origin of the Baiyinnuoer Zinc-Lead Deposit, Chifeng, Inner Mongolia: Geological and Sulfur Isotope Evidence[J]. Journal of Jilin University (Earth Science Edition), 2011, 37(4): 659-667.

[81] 要梅娟, 刘家军, 翟德高, 等. 大兴安岭南段多金属成矿带硫, 铅同位素组成及其地质意义[J]. 吉林大学学报(地球科学版), 2012, 42(2): 362-373. Yao Meijuan, Liu Jiajun, Zhai Degao, et al. Sulfur and Lead Isotopic Compositions of the Polymetallic Deposits in the Southern Daxinganling: Implications for Metal Sources[J]. Journal of Jilin University (Earth Science Edition), 2012, 42(2): 362-373.

[82] Wang L J, Hidehiko S, Wang J B, et al. Ore-Forming Fluid and Metallization of the Huanggangliang Skarn Fe-Sn Deposit, Inner Mongolia[J]. Science in China, 2001, 44(8): 735-747.

[83] 孙兴国. 内蒙古龙头山Ag-Pb-Zn多金属矿床成矿模式及找矿模型[D]. 北京:中国科学院研究生院,2008. Sun Xingguo. Ore-Forming Model and Exploration Model of the Longtoushan Ag-Pb-Zn Deposit, Inner Mongolia[D]. Beijing: Graduate School, Chinese Academy of Sciences, 2008.

[84] 张乾,战新志,裘愉卓,等.内蒙古孟恩陶勒盖银铅锌铟矿床的铅同位素组成及矿石铅的来源探讨[J]. 地球化学, 2002,31(3): 253-258. Zhang Qian, Zhan Xinzhi, Qiu Yuzhuo, et al. Lead Isotopic Composition and Lead Source of the Mengentaolegai Ag-Pb-Zn-In Deposit, Inner Mongolia[J]. Geochemica, 2002, 31(3): 253-258.

[85] 梅微,吕新彪,唐然坤,等.大兴安岭南段西坡拜仁达坝-维拉斯托矿床成矿流体特征及其演化[J]. 地球科学:中国地质大学学报,2015, 40(1): 145-162. Mei Wei, Lü Xinbiao, Tang Rankun, et al. Ore-Forming Fluid and Its Evolution of Bairendaba-Weilasituo Deposits in West Slope of Southern Great Xingan Range[J]. Earth Science:Journal of China University of Geosciences, 2015, 40(1):145-162.

[86] 李月臣, 陈柏林, 陈正乐,等. 阿尔金北缘红柳沟拉配泉一带铜金矿床硫同位素特征及其意义[J]. 地质力学学报,2007,13(2): 131-140. Li Yuechen, Chen Bolin, Chen Zhengle, et al. Sulfur Isotope Features of Cu-Au Polymetallic Deposits in the Hongliugou-Lapeiquan Area on the Northern Margin of the Altyntagh Mountains and Their Relation to the Tectonic Evolution[J]. Journal of Geomechanics, 2007, 13(2): 131-140.

[87] 牛树银, 聂凤军, 孙爱群, 等.大兴安岭幔枝构造与银多金属成矿作用[J]. 吉林大学学报(地球科学版), 2011, 41(6):1944-1958. Niu Shuyin, Nie Fengjun, Sun Aiqun, et al. Mantle Branch Structure and Silver-Polymetallic Mineralization in the Da Hinggan Mountains, Inner Mongolia[J]. Journal of Jilin University (Earth Science Edition),2011, 41(6):1944-1958.

[88] 赵一鸣, 张德全.大兴安岭及其邻区铜多金属矿床成矿规律与远景评价[M]. 北京:地震出版社, 1997. ZhaoYiming, Zhang Dequan. Metallogeny and Prospective Evolution of Copper-Polymetallic Deposits in the Da Hinggan Mountains and Its Adjacent Regions[M]. Beijing: Seismological Publishing House, 1997.

[89] Chu X L, Huo W G, Zhang X. Sulfur, Carbon and Lead Isotope Studies of the Dajing Polymetallic Deposit in Linxi County, Inner Mongolia, China-Implication for Metallogenic Elements from Hypomagmatic Source[J]. Resource Geology, 2001, 51(4): 333-344.

[90] 蔡剑辉, 阎国翰, 肖成东, 等. 太行山大兴安岭构造岩浆带中生代侵入岩Nd、Sr、Pb同位素特征及物质来源探讨[J]. 岩石学报, 2004, 20(5):1225-1242. Cai Jianhui, Yan Guohan, Xiao Chengdong, et al. Nd, Sr, Pb Isotopic Characteristics of the Mesozoic Intrusive Rocks in the Taihang-Da Hinggan Mountains Tectonomagmatic Belt and Their Source Region[J]. Acta Petrologica Sinica, 2004, 20(5): 1225-1242.

[91] 盛继福, 付先政, 李鹤年,等.大兴安岭中段成矿环境与铜多金属矿床地质特征[M]. 北京:地震出版社, 1999. Shen Jifu, Fu Xianzheng, Li Henian, et al. Ore-Forming Setting and Features of the Copper Poly-Metallic Deposits in Middle Segment of the Daxinganling[M]. Beijing: Seismological Publishing House, 1999.

[92] Zartman R E, Doe B R. Plumbotectonics:The Model[J]. Tectonophysic,1981, 75:135-162.

[93] Stacey J S, Kramers J D. Approximation of Terrestrial Lead Isotope Evolution by a Two-Stage Model[J]. Earth and Planetary Science Letters, 1975, 26:207-221.

[94] 马星华,陈斌,赖勇,等.内蒙古敖仑花斑岩钼矿床成岩成矿年代学及地质意义[J].岩石学报, 2009,25(11): 2939-2950. Ma Xinghua, Chen Bin, Lai Yong, et al. Petrogenesis and Mineralization Chronology Study on the Aolunhua Porphyry Mo Deposit, Inner Mongolia, and Its Geological Implications[J]. Acta Petrologica Sinica, 2009, 25(11): 2939-2950.

[95] Wang Y W, Wang J B , Uemoto T, et al. Geology and Mineralization at the Dajing Tin-Polymetallic Ore Deposit, Inner Mongolia, China[J]. Resource Geology ,2001, 51(4):307-320.

[96] Xiao W J, Windley B F, Hao J, et al. Accretion Leading to Collision and the Permian Solonker Suture, Inner Mongolia, China: Termination of the Central Asian Orogenic Belt[J]. Tectonics, 2003, 22(6):1069.

[97] Wu F Y, Zhao G C, Sun D Y, et al. The Hulan Group: Its Role in the Evolution of the Central Asian Orogenic Belt of NE China[J].Journal of Asian Earth Sciences, 2007, 30(3/4):542-556.

[98] 申伍军, 王学求, 聂兰仕.大兴安岭成矿带大型银多金属矿区域地球化学预测指标[J]. 地学前缘, 2012,19(3): 49-58. Shen Wujun, Wang Xueqiu, Nie Lanshi. Regional Geochemical Indicators of Large-Sized Silver Polymetallic Deposits in Daxinganling Metallogenic Belt[J]. Earth Science Frontiers, 2012, 19(3): 49-58.

[1] Li Jian, He Xinjian, Huang Jun. Adaptive Weight Density Inversion Method for Gravity Anomaly and Mesozoic Division of Diaobei Sag in East China Sea [J]. Journal of Jilin University(Earth Science Edition), 2022, 52(1): 229-.
[2] Yang Yuanjiang, Deng Changzhou, Li Chenglu, Zhang Li, Gao Yongzhi, Yu Xihuan. Geochronology,Geochemistry and Genesis of Igneous Rocks Associated with Dayangshan Mo Deposit in Great Xing'an Range [J]. Journal of Jilin University(Earth Science Edition), 2021, 51(4): 1064-1081.
[3] Qiu Shuwei, Wu Yamin, Ke Yuqi, Yan Baizhong. Optimization of Hydrogeological Parameters Based on Ergodic Search Algorithm [J]. Journal of Jilin University(Earth Science Edition), 2020, 50(6): 1854-1861.
[4] Wu Zhiqiang, Guo Xingwei, Zhao Weina, Zhang Xunhua, Qi Jianghao, Zhang Xiaohua, Cai Laixing. Site Selection of Scientific Drilling Well CSDP-2 for Marine Mesozoic-Paleozoic Strata in Central Uplift of South Yellow Sea Basin [J]. Journal of Jilin University(Earth Science Edition), 2019, 49(1): 13-25.
[5] Yang Changqing, Yang Chuansheng, Sun Jing, Yang Yanqiu. Mesozoic Evolution and Dynamics Transition in Southern Shelf Basin of the East China Sea [J]. Journal of Jilin University(Earth Science Edition), 2019, 49(1): 139-153.
[6] Wang Jiao, Li Zhigao, Cai Laixing, Gong Qiyong. Sedimentary Model of Mesozoic in the Southern Part of the East China Sea Shelf Basin [J]. Journal of Jilin University(Earth Science Edition), 2019, 49(1): 131-138.
[7] Guo Xingwei, Zhang Xunhua, Wu Zhiqiang, Xiao Guolin, Hou Fanghui, Liu Jian. Scientific Objectives and Preliminary Progresses of CSDP-2 Well in Continental Shelf Drilling Program [J]. Journal of Jilin University(Earth Science Edition), 2019, 49(1): 1-12.
[8] Yang Huaiyu. Developing Characteristics and Controlling Factors of Buried-Hill Residual Formation in Wangjiagang-Bamianhe Area [J]. Journal of Jilin University(Earth Science Edition), 2018, 48(6): 1625-1634.
[9] Song Mingchun, Li Jie, Li Shiyong, Ding Zhengjiang, Tan Xianfeng, Zhang Zhaolu, Wang Shijin. Late Mesozoic Thermal Upwelling-Extension Structure and Its Dynamics Background in Eastern Shandong Province [J]. Journal of Jilin University(Earth Science Edition), 2018, 48(4): 941-964.
[10] Gao Fei, Liu Yongjiang, Wen Quanbo, Li Weimin, Feng Zhiqiang, Fan Wenliang, Tang Chao. Zircon U-Pb Ages and Its Geological Implication of Mesozoic Granites in Tuquan-Keerqin Youyizhongqi Region [J]. Journal of Jilin University(Earth Science Edition), 2018, 48(3): 769-783.
[11] Cai Laixing, Wang Jiao, Guo Xingwei, Xiao Guolin, Zhu Xiaoqing, Pang Yumao. Characteristics of Sedimentary Facies and Source Rocks of Mesozoic-Paleozoic in Central Uplift of South Yellow Sea: A Case Study of CSDP-2 Coring Well [J]. Journal of Jilin University(Earth Science Edition), 2017, 47(4): 1030-1046.
[12] Yin Zhigang, Wang Wencai, Zhang Yuelong, Wang Yang, Han Yu, Cao Zhongqiang, Zheng Bei. Mesozoic Volcanic Rocks in Yilehuli Area: Zircon U-Pb Ages and Their Constraints on the Magmatic Events [J]. Journal of Jilin University(Earth Science Edition), 2016, 46(3): 766-780.
[13] Yang Haibin, Tian Xiaobo, Bai Zhiming, Zhang Zhongjie. Discussion on the Relationship Between Pan Pacific Plate Movement and Mesozoic Geological Evolution of Eastern Chinese Continent [J]. Journal of Jilin University(Earth Science Edition), 2016, 46(3): 781-797.
[14] Han Jun, Xue Wei, Song Qingnian. Characteristics of Volcanic-Type Uranium-Ore Forming and Sign for Uranium Searching at Hetaoba Area, Duolun County, Inner Mongolia [J]. Journal of Jilin University(Earth Science Edition), 2015, 45(3): 772-790.
[15] Sun Shouliang, Li Yongfei, Gao Xiaoyong. Mesozoic Volcanic Rocks Geochronology and Geochemical Characteristics in Wulangai Basin of Inner Mongolia and Their Geological Significance [J]. Journal of Jilin University(Earth Science Edition), 2015, 45(2): 441-452.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
[1] ZHU Hong-chen,ZHANG Jiong-fei,QUAN Heng. Two Stages of Mesozoic Lithogenesis and Mineralization in Daxing’anling Mountains[J]. J4, 2005, 35(04): 436 -0442 .
[2] WU Kong-yun,JIANG Zhong-cheng,YE Ye. Influence of Different Plant Communities On Erosion Rates of Limestone Rock Blocks[J]. J4, 2007, 37(5): 967 -0971 .
[3] ZHANG Yan-long, GE Wen-chun, LIU Xiao-ming, ZHANG Ji-heng. Isotopic Characteristics and Its Significance of the Xinlin Town Pluton,Great Hinggan Mountains[J]. J4, 2008, 38(2): 177 -0186 .
[4] ZHOU Yan-zhang, CHI Bao-ming, LIU Zhong-pei. Mode of Structural Control about Groundwater Pour-in Mechanism in Xiadian Gold Deposits in Shandong Province[J]. J4, 2008, 38(2): 255 -0260 .
[5] ZHANG Yuan, LIU Lian-deng,SUN Jing-gui,CHEN Guo-hua,ZHANG Hong-xi,YAN Fu-chuan, YANG Kai-chun. Two Phase Overprinting Mineralization in Huangbuling Gold Deposit in Northwestern Jiaodong Peninsula[J]. J4, 2008, 38(1): 21 -0026 .
[6] ZHANG Yu-ling,YAO Jun,ZHAO Xiao-bo,CAO Chun-ying,ZHENG Song-zhi. Optimum Conditions of Compound Bioflocculant Producing Bacterium YL3[J]. J4, 2008, 38(5): 864 -0868 .
[7] YU Qiang, REN Zhan-li. Comparison of Geothermal Fields in the Huangling and Dongsheng Areas, Ordos Basin[J]. J4, 2008, 38(6): 933 -0936 .
[8] ZHOU Xiao-dong,SUN Chun-lin,PENG Yu-jing. Reference Sections of Carboniferous and Permian Boundary in Xing’an-Mongolia and Jilin-Heilongjiang Orogenic Belt[J]. J4, 2009, 39(1): 72 -0079 .
[9] CUI Jian-jun, LIU Xiao-chun, HU Juan, QU Wei. Metamorphism of Indosinian Metamorphic Enclaves in the Tongbai Complex, Central China[J]. J4, 2009, 39(4): 618 -629 .
[10] CHEN Li, LIANG Hai-an,ZHANG Wen-juan,RONG Fan. Application of Fuzzy Mathematics in Division of Engineering Geo-Environment of Cities-An Example of Fushun City[J]. J4, 2008, 38(5): 837 -0840 .