华北克拉通条带状铁建造中富铁矿成因类型的研究进展、远景和存在的科学问题
Progress, prospecting and key scientific problems in origin researches of high-grade iron ore of the banded iron formation (BIF) in the North China Craton
-
摘要: 本文在查阅前人大量资料的基础上,对华北克拉通条带状铁建造中富铁矿的研究历史进行了回顾和总结,将研究历史分为1949年以前,1950~1965年期间,1978~1986年期间,1987~1994年期间和2009年以来5个阶段。重点介绍了鞍本地区、冀东-吕梁地区和河南舞阳地区富铁矿的基本地质特征以及典型富铁矿的研究概况,针对鞍本地区弓长岭二矿区磁铁富矿成因的复杂性,对不同成因观点以及目前已取得的共识进行了详细阐述。目前大多数学者不支持接触交代假说和菱铁矿经变质转化为富铁矿成矿假说,近半数学者支持变质热液成矿假说,半数学者支持混合岩化热液成矿假说。作者在综合分析前人大量资料后,认为变质热液成矿说依据不足,理由有四点:(1)磁铁富矿中往往见有磁铁贫矿的残体;(2)磁铁富矿与蚀变岩紧密伴生,蚀变矿物石榴子石、部分角闪石(透闪石)和部分绿泥石均属非变质热液成因;(3)研究区遭受区域高绿片岩相至低角闪岩相变质作用的时间为2500~2450Ma,而与蚀变矿物石榴石紧密伴生的热液锆石SHRIMP U-Pb定年结果为1840±7Ma,明显小于区域变质作用年龄,据此可将热液作用时间限定于古元古代晚期,相当于大陆地壳伸展阶段;(4)部分热液成因富铁矿利用Re-Os方法定年,除一种属原生沉积成矿外,年龄范围也在古元古代晚期,可作为参考。此种热液是否为混合岩化热液尚缺乏足够证据,故本文暂将其作为古元古代晚期热液。此外,本文对华北克拉通条带状铁建造中富铁矿成因类型及其远景进行了初步总结,认为古元古代晚期形成的磁铁富矿规模属大型矿床,有较好远景;原生较富贫铁矿因褶皱构造产生磁铁矿流变而形成的富铁矿(可能尚有热液叠加)规模较大,具有一定远景;其他类型均为小型规模,不具工业意义。最后,本文指出富铁矿成因研究中尚存在的主要问题,包括早元古代晚期热液的来源;热液的形成是一期还是多期;铁建造遭受区域变质达高绿片岩相时,贫铁矿的围岩变质演化机理等,尚需进一步探讨。Abstract: Basing on a large number of existing data, history of study on several typical high-grade iron ore deposits of banded iron formation (BIF) in the North China Craton is reviewed and summarized. The history can be divided into five stages: (1) before 1949; (2) between 1950 and 1965; (3) between 1978 and 1986; (4) between 1987 and 1994; (5) after 2009. Then basic geological characters of iron rich ore in Anshan area, Jidong-Lvliang area and Wuyang area are introduced. Meanwhile, study status of iron rich ore in the several areas above are emphatically introduced. In view of the complex origin of the magnetite rich ore in the No.2 mining district in Gongchangling area, researches and common viewpoints on them are introduced in detail. Up to now, most researchers are not agreeable on the iron rich deposit hypothesis of contact metasomatism or transformation from siderite through metamorphism. Nearly half of the researchers agree with the theory of metamorphic hydrothermal mineralization and another half the theory of migmatized hydrothermal mineralization. According to comprehensive analysis of voluminous data from the literature, the authors think there is no enough evidence for the contention of metamorphic hydrothermal mineralization. There are four arguments for the viewpoint: the first is that residual magnetite lean ore can be frequently found in the iron rich ore. The second is that magnetite-rich ore is intimately associated with alteration rocks in which the alteration minerals like garnet, some hornblende (tremolite) and chlorite are not metamorphic hydrothermal origin. The third, age of regional (upper greenschist to lower amphibolite facies) metamorphism is bracketed in the range of 2500Ma and 2450Ma, while the hydrothermal zircons accompanied with the alteration garnet give the U-Pb age of 1840±7Ma (dating by SHRIMP), which is younger than the metamorphism age. Thus the hydrothermal activity was constrained to occur in the Late Paleoproterozoic when the continental crust of the Craton was in extension period. The fourth, Late Paleoproterozoic age has been obtained through Re-Os dating from the high-grade iron ore of hydrothermal origin. As no enough evidence to prove the hydrothermal fluid migmatitic, we tentatively regard it as Late Paleoproterozoic hydrothermal fluid. In addition, origin types and prospecting potential of the high-grade iron ore of the BIF in the North China Craton are discussed. The authors deduce that the magnetite-rich iron ores of Late Paleoproterozoic may form to large scale and are of great potentials. The magnetite-rich ores through rheological deformation due to fold structures in primary higher-grade magnetite-poor ores (probably accompanied with hydrothermal superposition) may reach to biggish scale and of certain potential. Others are generally in small scale and of no economical significance. Finally, the authors put forward some problems in high-grade iron ore research, such as the source of the hydrothermal fluid of Late Paleoproterozoic, single or multistages of the hydrothermal fluid formation, and metamorphic mechanism of the wall rocks of the lean iron ores. All these problems need further theoretical investigation.
-
Key words:
- Banded iron formation /
- High-grade iron deposits /
- Origin type /
- North China Craton
-
-
[1] Cai YM. 1992. Occurrence rule and exploration guide of the high-grade iron ore in Gongchangling area. In: Wang KN and Yao PH (eds.). The Summary of Iron Ore Deposits of China. Beijing: Metallurgical Industry Press, 194-200 (in Chinese)
[2] Chen GY, Li MH, Wang XF, Sun DS, Sun CM, Wang ZF, Su YX and Lin JX. 1984. Genetic mineralogy of Gongchangling iron mine. Minerals and Rocks, 4(2): 1-254 (in Chinese)
[3] Chen HJ and Xu GR. 1984. Characteristics of genetic mineralogy of magnetite in the II mining area of the Gongchangling iron deposit and its signification. Jilin Geology, (1): 22-30 (in Chinese with English abstract)
[4] Chen J, Li HM, Li LX, Yang XQ, Liu MJ, Yao T, Hu B and Zhang JY. 2014. Fluid inclusions and oxygen isotope study of the Sijiaying BIF in the eastern Hebei Province. Acta Petrologica Sinica, 30(5): 1253-1268 (in Chinese with English abstract)
[5] Chen JF, Yang YL, Li P, Cheng WJ, Zhou TX and Liu YP. 1985. Study on sulfur isotope of rich magnetite in Anshan-Benxi area, Liaoning Province. Geology and Prospecting, 21(1): 32-37 (in Chinese)
[6] Chen ZL, Ding WJ, Cui LL, Chen BL, Han FB, Zhou YG, Dong FX and Yang N. 2010. Preliminary study on origin of Xingshan large iron rich ore in Qian'an, Hebei Province. Mineral Deposits, 29(Suppl.): 71-72 (in Chinese)
[7] Cheng YQ. 1957. Problems on the genesis of the high-grade ore in the pre-Sinian (pre-Cambrian) banded iron ore deposits of the Anshan-type of Liaoning and Shandong Provinces. Acta Geologica Sinica, 37(2): 153-180 (in Chinese)
[8] Dai CY. 1942. Study on garnet in Gongchangling No.4: Output state. Journal of Rock-Mineral-Deposit Academy of Japan, 27(1) (in Japanese)
[9] Dai YP, Zhang LC, Zhu MT, Wang CL and Liu L. 2013. Mineralizationg, crustal growth and origin of iron rich ore in Anshan-Benxi area. Acta Mineralogica Sinica, (Suppl. 2): 386-388 (in Chinese)
[10] Ding WJ, Chen ZL, Chen BL, Dong FX and Cui LL. 2009. Geochemical characters of band iron formations from Xingshan iron deposit in Qian'an area, Hebei Province: Implication for their origin. Journal of Geomechanics, 15(4): 363-373 (in Chinese with English abstract)
[11] Dong SB, Zhang QS and Li SX. 1972. Migmatic Metallogonesis in Presinian of Liaoning Peninsula. Changchun: Changchun Geological College Publishing House, 21-25 (in Chinese)
[12] Duliu YX. 1931. Geology and deposit of Tieshan in Miaoergou. Report of Lvshun College of Engineering, 1(3) (in Japanese)
[13] Duliu YX. 1932. Geology and deposit of Waitoushan. Report of Lvshun College of Engineering, 2(3) (in Japanese)
[14] Duliu YX. 1935. About Gongchangling Tieshan and similar deposit. Report of Lvshun College of Engineering, 5(39): 1-19 (in Japanese)
[15] Guan GY. 1961. The significance of metamorphic on the forming of Anshan-type rich iron ore deposit. Acta Geologica Sinica, 41(1): 65-76 (in Chinese with Russian abstract)
[16] Guan GY. 1992. The significance of metamorphic on the forming of Anshan-type rich iron ore deposit. In: Wang KN and Yao PH (eds.). The Summary of Iron Ore Deposits of China. Beijing: Metallurgical Industry Press, 183-193 (in Chinese)
[17] Jv ZN, Wei GY and Liu FY. 2009. The genesis of Gongchangling rich iron deposit in Liaoyang, Liaoning Province. Heilongjiang Science and Technology Information, (16): 53 (in Chinese)
[18] Li BL, Li XM, Cui XF, Wang ZL and Liu YM. 1977. The genesis and indicator of magnetite rich ore in Gongchangling No.2 area, according to the research on mineral inclusion. Geology and Prospecting, (6): 3-11 (in Chinese)
[19] Li HM, Liu MJ, Li LX, Yang XQ, Chen J, Yao LD, Hong XK and Yao T. 2012. Geology and geochemistry of the marble in the Gongchangling iron deposit in Liaoning Province and their metallogenic significance. Acta Petrologica Sinica, 28(11): 3497-3512 (in Chinese with English abstract)
[20] Li HM, Liu MJ, Li LX, Yang XQ, Yao LD, Chen J and Yao T. 2014. SHRIMP U-Pb geochronology of zircons from the garnet-rich altered rocks in the mining area II of the Gongchangling iron deposit: Constraints on the ages of the high-grade iron deposit. Acta Petrologica Sinica, 30(5): 1025-1217 (in Chinese with English abstract)
[21] Li HY. 1992. On the problems of metallogug enrichment and oxidation of Anshan type iron deposit. In: Wang KN and Yao PH (eds.). The Summary of Iron Ore Deposits of China. Beijing: Metallurgical Industry Press, 46-66 (in Chinese)
[22] Li JJ, Shen BF and Luo H. 1995. The genetic types and geological feature of rich iron deposits of Precambrian banded iron formation in north China. Bulletin Tianjin Institute Geology Mineralogy Resource, (29): 77-87 (in Chinese with English abstract)
[23] Li SB. 1979. A contribution to the genesis of rich magnetite deposit of the Gongchangling Type-in the light of graphite discovered in it. Geochimica, (2): 170-177 (in Chinese with English abstract)
[24] Li SG. 1982. Geochemical model for the genesis of Gongchangling rich magnetite deposit in China. Geochimica, (2): 113-121 (in Chinese with English abstract)
[25] Li SG, Zhi XC, Chen JF, Wang JX and Deng YY. 1983. Origin of graphites in Early Precambrian banded iron formation in Anshan, Chian. Geochimica, (2): 162-169 (in Chinese with English abstract)
[26] Li YH, Zhang ZJ, Hou KJ, Duan C, Wan DF and Hu GY. 2014. The genesis of Gongchangling high-grade-iron ores, Anshan-Benxi area, Liaoning Province, NE China: Evidence from Fe-Si-O-S isotopes. Acta Geologica Sinica, 88(12): 2351-2372 (in Chinese with English abstract)
[27] Li ZH, Zhu XK and Tang SH. 2008. Characters of Fe isotopes and rare earth elements of banded iron formations from Anshan-Benxi area: Implications for Fe source. Acta Petrologica et Mineralogica, 27(4): 285-290 (in Chinese with English abstract)
[28] Liu J and Jin SY. 2010. Genesis study of magnetite-rich ore in Gongchangling iron deposit, Liaoning. Geoscience, 24(1): 80-88 (in Chinese with English abstract)
[29] Liu MJ, Li HM, Li LX, Yang XQ, Yao LD, Hong XK and Chen J. 2012. Petrological and Mineralogical characteristics of the skarnoid in No.2 mining area of the Gongchangling iron deposit, Liaoning, China. Rock and Mineral Analysis, 31(6): 1067-1076 (in Chinese with English abstract)
[30] Liu MJ, Li HM, Yao LD, Wen L and Xu ZX. 2014. Re-Os isotopic dating of pyrite and molybdenite from the iron deposits in Anshan-Benxi area of Liaoning Province and its geological significances. Geology in China, 41(6): 1821-1832 (in Chinese with English abstract)
[31] Luo YX. 1957. Discussion on the genesis of Anshan-type iron deposit. Journal of Geological Society of China, (10): 26-30 (in Chinese)
[32] Qian XL, Cui WY, Wang SL and Wang GY. 1985. Geology of Precambrian Iron Ores in Eastern Hebei Province, China. Shijiazhuang: Hebei Science and Technology Press (in Chinese)
[33] Qianye WL and Gangtian ZG. 1940. About almandite in Gongchangling. Report of Manchukuo Geological Survey Institute, 51-56 (in Japanese)
[34] Ren YC. 1981. Characters of iron oxide minerals and the genesis of rich iron deposits Anshan-Benxi area, Northeast China. Acta Mineralogica Sinica, (4): 245-248 (in Chinese with English abstract)
[35] Shen BF, Peng XL, Luo H, Jin WS, Hu XD, Li SB, Li JJ and Chen YH. 1994. Archean greenstone belt and ore deposits. In: Zhang YX and Liu LD (eds.). Precambrian Ore Deposits and Techtonics in China. Beijing: Seism Publishing House (in Chinese)
[36] Shi JX and Li BC. 1980. Origin of rich magnetite ores in the Gongchangling area as evidenced by fluid inclusion studies from the Anshan-Benxi region, Northeast China. Geochimica, (1): 43-53 (in Chinese with English abstract)
[37] Tian YQ, Yuan GP, Lu JR, Jing Y, Yu JH and Li MM. 1986. Study on the geological tectonic characters and formation condition of Precambrian meta-sediment iron deposit in Yuanjiacun, Lanxian County, Shanxi Province. Ferrous Mineral Resource, (5): 1-270 (in Chinese)
[38] Wan YS. 1993. The Formation and Evolution of the Iron-Bearing Rock Series of the Gongchangling Area, Liaoning Province. Beijing: Beijing Science and Technology Press (in Chinese)
[39] Wang ED, Xia JM, Zhao CF, Fu JF and Hou GQ. 2012. Forming mechanism of high-grade magnetite bodies in Gongchangling, Liaoning Province. Acta Geologica Sinica, 86(11): 1761-1773 (in Chinese with English abstract)
[40] Wang SL. 1986. The genetic type of rich iron deposits of Anshan Group in Anshan-Benxi area. Mineral Deposits, 5(4): 14-23 (in Chinese with English abstract)
[41] Wei JY, Zheng SH and Mo ZC. 1979. Oxygen isotopic composition of magnetite in Pre-Sinian, Fe-bearing quartzite in the area of Luanxian County, Hebei Province. Geochimica, (3): 195-202 (in Chinese with English abstract)
[42] Xia JM, Wang ED, Zhao CF and Men YK. 2011. The formation mechanism of the redox environment in the rich iron deposits of Gongchangling. Journal of Northeastern University (Natural Science), 32(11): 1643-1646 (in Chinese with English abstract)
[43] Xu GR and Chen HJ. 1984. Metallogenic characteristics of iron deposits in Archean greenstone basin of Anshan-Benxi area, Northeast China. Mineral Deposits, 3(2): 1-10 (in Chinese with English abstract)
[44] Xu GR and Chen HJ. 1992. The metallugenic characteristics of iron deposits in archean greenstone basin in Anshan-Benxi district, North-East China. In: Wang KN and Yao PH (eds.). The Summary of Iron Ore Deposits of China. Beijing: Metallurgical Industry Press, 107-114 (in Chinese)
[45] Xu YX, Zhang LF, Gao XM, Li HM, Jia DS and Li LX. 2014. Metallogenic conditions of high-grade ores in the Sijiaying sedimentary metamorphic iron deposit, eastern Hebei Province. Geology and Exploration, 50(4): 675-688 (in Chinese with English abstract)
[46] Yang XQ, Li HM, Li LX, Liu MJ, Chen J and Bai Y. 2012. Characteristics of rare earth elements and the geological significance of magnetite from Gongchangling iron deposit in Liaoning Province. Rock and Mineral Analysis, 31(6): 1058-1066 (in Chinese with English abstract)
[47] Yang XQ, Li HM, Xue CJ, Li LX, Liu MJ and Chen J. 2013. Geochemical characteristics of two iron ores from the Waitoushan iron deposit, Liaoning Province: Constraints on ore-forming mechinisam. Acta Geologica Sinica, 87(10): 1580-1592 (in Chinese with English abstract)
[48] Yang XQ, Li HM, Li LX, Ma YB, Chen J, Liu MJ, Yao T, Chen WS and Yao LD. 2014. Characteristics of fluid inclusion, S, H and O isotope of iron deposit in Anshan-Benxi area, Liaoning Province. Acta Geologica Sinica, 88(10): 1917-1931 (in Chinese with English abstract)
[49] Zeng JW, Chen SH, Wang MZ et al. 1992. Mineralization feature of iron rich ore in Taihua Group's metamorphic series and weathering crust in Wuyang area, Henan Province. In: Wang KN and Yao PH (eds.). The Summary of Iron Ore Deposits of China. Beijing: Metallurgical Industry Press, 280-300 (in Chinese)
[50] Zhang H. 1982. Vertical zoning of metallization in the high-grade iron deposits of Gongchangling type, Anshan-Benxi area, Liaoning Province. Geochimica, (3): 260-269 (in Chinese with English abstract)
[51] Zhang LC, Dai YP, Wang CL, Liu L and Zhu MT. 2014. Age, material sources and formation setting of Procambrian BIFs iron deposits in Anshan-Benxi area. Journal of Earth Sciences and Environment, 36(4): 1-15 (in Chinese with English abstract)
[52] Zhang LF, Xu YX, Gao XM, Jia DS and Wang Y. 2015. Genesis of high-grade ores in the Xingshan sedimentary metamorphic iron deposit of eastern Hebei Province. Geology and Exploration, 51(3): 405-413 (in Chinese with English abstract)
[53] Zhang QS. 1984. Geology and Metallogeng of the Early Precambrian in China. Jilin: Jilin People Publishing House, 1-535 (in Chinese)
[54] Zhang QS. 1988. Early Crustal and Mineral Deposits of Liaodong Peninsula, China. Beijing: Geological Publishing House, 1-574 (in Chinese)
[55] Zhao B and Li TJ. 1980. A preliminary study on the mechanism and physicochemical conditions of formation of Gognchangling rich iron deposit. Geochimica, (4): 333-344 (in Chinese with English abstract)
[56] Zheng BD. 1992. Stratabound rich ore (magnetite) deposits in the Archeanozoic granite greenstone terrane in Anshan-Benxi district, Liaoning. In: Wang KN and Yao PH (eds.). The Summary of Iron Ore Deposits of China. Beijing: Metallurgical Industry Press, 160-171 (in Chinese)
[57] Zheng MT, Zhang LC, Wang CL, Zhu MT, Li ZQ and Wang YT. 2015. Formation age and origin of the Xingshan BIF-type iron deposit in eastern Hebei Province. Acta Petrologica Sinica, 31(6): 1636-1652 (in Chinese with English abstract)
[58] Zheng Z and Lan HY. 2009. Discussion on the genesis and geological characters of Gongchangling rich iron deposit. Modern Mining, (4): 67-70 (in Chinese)
[59] Zhou ST. 1992. The study of Archaean Anshan group in Anshan-Benxi district, Liaoning Province. In: Wang KN and Yao PH (eds.). The Summary of Iron Ore Deposits of China. Beijing: Metallurgical Industry Press, 84-93 (in Chinese)
[60] Zhou ST. 1994. Geology of Banded Iron Formation in Anshan-Benxi Area. Beijing: Geological Publishing House, 1-228 (in Chinese)
[61] Zhou YG, Chen ZL, Chen BL and Han FB. 2012. Genesis of rich and large ore body in Xingshan iron deposit of Qian'an ore field, Hebei Province. Journal of Jilin University (Earth Science Edition), 42(Suppl.3): 81-92 (in Chinese with English abstract)
[62] 才玉民. 1992. 弓长岭富铁矿的赋存规律与找矿标志. 见: 王可南, 姚培慧编. 中国铁矿床综论. 北京: 冶金工业出版社, 194-200
[63] 陈光远, 黎美华, 汪雪芳, 孙岱生, 孙传敏, 王祖福, 速玉萱, 林家湘. 1984. 弓长岭铁矿成因矿物学. 矿物岩石, 4(2): 1-250
[64] 陈洪江, 徐光荣. 1984. 弓长岭铁矿二矿区磁铁矿的成因矿物学特征及其意义. 吉林地质, (1): 22-30
[65] 陈靖, 李厚民, 李立兴, 杨秀清, 刘明军, 姚通, 胡彬, 张进友. 2014. 冀东司家营BIF铁矿流体包裹体及氧同位素研究. 岩石学报, 30(5): 1253-1268
[66] 陈江峰, 杨延龄, 李平, 程伟基, 周泰禧, 刘燕平. 1985. 辽宁鞍山-本溪地区富磁铁矿硫同位素地质研究. 地质与勘探, 21(1): 32-37
[67] 陈正乐, 丁文君, 崔玲玲, 陈柏林, 韩凤彬, 周永贵, 董法先, 杨农. 2010. 河北迁安杏山富大铁矿体成因初析. 矿床地质, 29(增刊): 71-72
[68] 程裕淇. 1957. 中国东北部辽宁山东等省前震旦纪鞍山式条带状铁矿中富矿的成因问题. 地质学报, 37(2): 153-180
[69] 待仓勇. 1942. 弓长岭石榴石之研究(四)产出状态. 日本岩石矿物矿床学会志, 27(1)(日文, 仅见扎录)
[70] 代堰锫, 张连昌, 朱明田, 王长乐, 刘利. 2013. 鞍本地区太古代BIF成矿作用、地壳增生及富矿成因. 矿物学报, (增刊): 386-388
[71] 丁文君, 陈正乐, 陈柏林, 董法先, 崔玲玲. 2009. 河北迁安杏山铁矿床地球化学特征及其对成矿物质来源的指示. 地质力学学报, 15(4): 363-373
[72] 董申保, 张秋生, 李树勋. 1972. 辽东半岛前震旦纪混合岩化成矿作用. 长春: 长春地质学院出版社, 21-25
[73] 都留一雄. 1931. 庙尔沟铁山之地质及矿床. 旅顺工科大学报告, 1(3)(日文)
[74] 都留一雄. 1932. 歪头山附近之地质及矿床. 旅顺工科大学报告, 2(3)(日文)
[75] 都留一雄. 1935. 关于弓长岭铁山及类似矿床. 旅顺工科大学报告, 5(39): 1-19(日文)
[76] 关广岳. 1961. 论变质作用在鞍山式铁矿床富矿形成上的意义. 地质学报, 41(1): 65-76
[77] 关广岳. 1992. 论变质作用在鞍山式铁矿床富矿形成上的意义. 见: 王可南, 姚培慧编. 中国铁矿床综论. 北京: 冶金工业出版社, 183-193
[78] 鞠振南, 卫广远, 刘风英. 2009. 辽阳弓长岭富铁矿的成因探讨. 黑龙江科技信息, (16): 53
[79] 李秉伦, 李学明, 崔贤富, 汪芝兰, 刘有梅. 1977. 根据矿物包裹体研究——试论弓长岭二矿区磁铁富矿的成因及找矿标志. 地质与勘探, (6): 3-11
[80] 李鸿业. 1992. 鞍山式铁矿的形成及其富化、氧化问题. 见: 王可南, 姚培慧编. 中国铁矿床综论. 北京: 冶金工业出版社, 46-66
[81] 李厚民, 刘明军, 李立兴, 杨秀清, 陈靖, 姚良德, 洪学宽, 姚通. 2012. 辽宁弓长岭铁矿区大理岩地质地球化学特征及其成矿意义. 岩石学报, 28(11): 3497-3512
[82] 李厚民, 刘明军, 李立兴, 杨秀清, 姚良德, 陈靖, 姚通. 2014. 弓长岭铁矿二矿区蚀变岩中锆石SHRIMP U-Pb年龄及地质意义. 岩石学报, 30(5): 1025-1217
[83] 李俊健, 沈保丰, 骆辉. 1995. 中国北方早前寒武纪富铁矿的成因类型和地质特征. 中国地质科学院天津地质矿产研究所所刊, (29): 77-87
[84] 李绍柄. 1979. 我国铁矿床的一种新类型——弓长岭式含石墨的富磁铁矿床及其成因. 地球化学, (2): 170-177
[85] 李曙光. 1982. 弓长岭富磁铁矿床成因的地球化学模型. 地球化学, (2): 113-121
[86] 李曙光, 支霞臣, 陈江峰, 王俊新, 邓衍尧. 1983. 鞍山前寒武纪条带状含铁建造中石墨的成因. 地球化学, (2): 162-169
[87] 李延河, 张增杰, 侯克军, 段超, 万德芳, 胡古月. 2014. 辽宁鞍本地区沉积变质型富铁矿床的成因: Fe、Si、O、S同位素证据. 地质学报, 88(12): 2351-2372
[88] 李志红, 朱祥坤, 唐索寒. 2008. 鞍山-本溪地区条带状铁建造的铁同位素与稀土元素及其对成矿物质来源的指示. 岩石矿物学杂志, 27(4): 285-290
[89] 刘军, 靳淑韵. 2010. 辽宁弓长岭铁矿磁铁富矿的成因研究. 现代地质, 24(1): 80-88
[90] 刘明军, 李厚民, 李立兴, 杨秀清, 姚良德, 洪学宽, 陈靖. 2012. 辽宁弓长岭铁矿床二矿区类矽卡岩的岩石矿物学特征. 岩矿测试, 31(6): 1067-1076
[91] 刘明军, 李厚民, 姚良德, 文岭, 许宗宪. 2014. 辽宁鞍本地区铁矿床黄铁矿和辉钼矿Re-Os同位素测年及其地质意义. 中国地质, 41(6): 1821-1832
[92] 罗耀星. 1957. 鞍山式铁矿成因问题的商榷. 中国地质学会会讯, (10): 26-30
[93] 钱祥麟, 崔文元, 王时麟, 王关玉. 1985. 冀东前寒武纪铁矿地质. 石家庄: 河北科学技术出版社
[94] 浅野五郎, 冈田重光. 1940. 关于弓长岭铁铝榴石. 伪满地质调查所报告, 51-56
[95] 任英忱. 1981. 鞍本地区铁的氧化矿物特征及富铁矿的成因. 矿物学报, (4): 245-248
[96] 沈保丰, 彭晓亮, 骆辉, 金文山, 胡小蝶, 李双保, 李俊建, 陈勇华. 1994. 华北陆台太古宙绿岩带及矿床. 见: 张贻侠, 刘连登编. 中国前寒武纪矿床和构造. 北京: 地震出版社
[97] 施继锡, 李本超. 1980. 根据鞍本地区包裹体研究试论弓长岭磁富铁矿的成因. 地球化学, (1): 43-53
[98] 田永清, 袁国屏, 路九如, 荆毅, 余建宏, 李敏敏. 1986. 山西省岚县袁家村前寒武纪变质-沉积铁矿床的地质构造特征与形成条件研究. 山西省地质矿产局测绘队黑色金属矿产, (5): 1-270
[99] 万渝生. 1993. 辽宁弓长岭含铁岩系的形成与演化. 北京: 北京科学技术出版社
[100] 王恩德, 夏建明, 赵纯福, 付建飞, 侯根群. 2012. 弓长岭铁矿床磁铁富矿形成机制探讨. 地质学报, 86(11): 1761-1773
[101] 王守伦. 1986. 鞍本地区鞍山群富铁矿成因类型的讨论. 矿床地质, 5(4): 14-23
[102] 魏菊英, 郑淑蕙, 莫志超. 1979. 冀东滦县一带前震旦纪含铁石英岩中磁铁矿的氧同位素组成. 地球化学, (3): 195-202
[103] 夏建明, 王恩德, 赵纯福, 门业凯. 2011. 弓长岭富铁矿氧化还原环境的形成机制. 东北大学学报(自然科学版), 32(11): 1643-1646
[104] 徐光荣, 陈洪江. 1984. 鞍本太古代绿岩盆地铁矿的成矿特征. 矿床地质, 3(2): 1-10
[105] 徐光荣, 陈洪江. 1992. 鞍本太古宙绿岩盆地铁矿的成矿特征. 见: 王可南, 姚培慧编. 中国铁矿床综论. 北京: 冶金工业出版社, 107-114
[106] 许英霞, 张龙飞, 高孝敏, 李厚民, 贾东锁, 李立兴. 2014. 冀东司家营铁矿床富矿成矿条件研究. 地质与勘探, 50(4): 675-688
[107] 杨秀清, 李厚民, 李立兴, 刘明军, 陈靖, 白云. 2012. 辽宁弓长岭铁矿床磁铁矿稀土元素特征及其地质意义. 岩矿测试, 31(6): 1058-1066
[108] 杨秀清, 李厚民, 薛春纪, 李立兴, 刘明军, 陈靖. 2013. 辽宁歪头山铁矿床两类矿石地球化学特征及其对成矿作用的制约. 地质学报, 87(10): 1580-1592
[109] 杨秀清, 李厚民, 李立兴, 马玉波, 陈靖, 刘明军, 姚通, 陈伟十, 姚良德. 2014. 辽宁鞍山-本溪地区铁矿床流体包裹体和硫、氢、氧同位素特征研究. 地质学报, 88(10): 1917-1931
[110] 曾玖吾, 陈森煌, 汪曼祉等. 1992. 舞阳地区太华群变质岩系及风化壳富铁矿矿化特征. 见: 王可南, 姚培慧编. 中国铁矿床综论. 北京: 冶金工业出版社, 280-300
[111] 张湖. 1982. 辽宁鞍本地区弓长岭型富铁矿成矿的垂直分带. 地球化学, (3): 260-269
[112] 张连昌, 代堰锫, 王长乐, 刘利, 朱明田. 2014. 鞍山-本溪地区前寒武纪条带状铁建造铁矿时代、物质来源与形成环境. 地球科学与环境学报, 36(4): 1-15
[113] 张龙飞, 许英霞, 高孝敏, 贾东锁, 王宇. 2015. 冀东杏山沉积变质型铁矿床富铁矿成因探讨. 地质与勘探, 51(3): 405-413
[114] 张秋生. 1984. 中国早前寒武纪地质及成矿作用. 吉林: 吉林人民出版社, 1-535
[115] 张秋生. 1988. 辽东半岛早期地质与矿床. 北京: 地质出版社, 1-574
[116] 赵斌, 李统锦. 1980. 鞍山弓长岭富磁铁矿床的形成机制和物理化学条件研究. 地球化学, (4): 333-344
[117] 郑宝鼎. 1992. 辽宁省鞍山-本溪地区太古代花岗质岩绿岩地体中层控磁铁富矿床. 见: 王可南, 姚培慧编. 中国铁矿床综论. 北京: 冶金工业出版社, 160-171
[118] 郑梦天, 张连昌, 王长乐, 朱明田, 李智泉, 王亚婷. 2015. 冀东杏山BIF铁矿形成时代及成因探讨. 岩石学报, 31(6): 1636-1652
[119] 郑柱, 蓝海洋. 2009. 弓长岭富铁矿床地质特征及成因探讨. 现代矿业, (4): 67-70
[120] 周世泰. 1992. 辽宁鞍本地区太古宙鞍山群地质特征. 见: 王可南, 姚培慧编. 中国铁矿床综论. 北京: 冶金工业出版社, 84-93
[121] 周世泰. 1994. 鞍山-本溪地区条带状铁矿地质. 北京: 地质出版社, 1-228
[122] 周永贵, 陈正乐, 陈柏林, 韩凤彬. 2012. 河北迁安杏山富大铁矿体成因初析. 吉林大学学报(地球科学版), 42(增刊3): 81-92
-
计量
- 文章访问数: 8127
- PDF下载数: 5660
- 施引文献: 0
下载: