[1] James H L. Sedimentary facies of iron-formation [J]. Economic Geology, 1954, 49(3): 235-293.
[2] Gross G A. A classification of iron formations based on depositional environments [J]. Canadian Mineralogist, 1980, 18(2): 215-222.
[3] Gross G A. Tectonic systems and the deposition of iron-formation [J]. Precambrian Research, 1983, 20(2/4): 171-187.
[4] 张春晓, 包杰, 胡忠义, 等. 镓元素在羊鼻山矿床中的地质特征 [J]. 黑龙江科技信息, 2010, 26: 28-29. ZHANG Chun-xiao, BAO Jie, HU Zhong-yi, et al. Geologic features of gallium element in Yangbishan deposit [J]. Heilongjiang Science and Technology Information, 2010, 26: 28-29.
[5] 吴佳滨. 黑龙江省佳木斯隆起成矿带沉积变质型铁矿特征及找矿前景 [J]. 科技创业家, 2012, 23: 200. WU Jia-bin. Features and prospects of sedimentary metamorphic-type iron deposit in mineralization belt within Jiamusi Uplifting, Heilongjiang Province [J]. Technological Pioneers, 2012, 23: 200.
[6] 谭成印. 黑龙江省主要金属矿床构造-成矿系统基本特征: 博士学位论文 [D]. 北京: 中国地质大学, 2009. TAN Cheng-yin. General characteristics of the tectonic-metallogenic system of main ore deposit in Heilongjiang Province, Northeast China: doctor's degree thesis [D]. Beijing: China University of Geosciences, 2009.
[7] 王长水, 孙福生, 王秀华. 黑龙江省前寒武纪基底及金矿成矿系列研究 [J]. 黄金, 2007, 28(3): 15-21. WANG Chang-shui, SUN Fu-sheng, WANG Xiu-hua. A research on the Precambrian basement and gold metallogenic series in Heilongjiang Province [J]. Gold, 2007, 28(3): 15-21.
[8] 邵建波, 张希友, 王洪涛, 等. 吉林省塔东大型铁矿地球化学特征及黄铁矿Re-Os同位素定年 [J]. 地质学报, 2014, 88(1): 83-98. SHAO Jian-bo, ZHANG Xi-you, WANG Hong-tao, et al. Geochemistry and pyrite Re-Os dating of the Tadong iron deposit in Jilin Province [J]. Acta Geologica Sinica, 2014, 88(1): 83-98.
[9] 周静, 李本仙, 梁一鸿, 等. 吉林东部塔东铁矿区雁脖岭岩体和朱敦店岩体的形成时代与构造背景分析 [J]. 世界地质, 2016, 35(1): 142-152. ZHOU Jing, LI Ben-xian, LIANG Yi-hong, et al. Formation age and tectonic setting of Yanboling and Zhudundian plutons in Tadong iron deposit,eastern Jilin Province [J]. Global Geology, 2016, 35(1): 142-152.
[10] Ludwig K R. User's Manual for isoplot 3.0: a geochronological toolkit for Microsoft Excel[M]. Berkeley: Berkeley Geochronology Center Special Publication, 2003: 1-71.
[11] Andersen T, Griffin W L, Pearson N J. Crustal evolution in the SW part of the Baltic Shield: the Hf isotope evidence[J].Journal of Petrology, 2002, 43(9): 1725-1747.
[12] 姜继圣. 孔兹岩系及其研究概况 [J]. 长春地质学院学报, 1990, 20(2): 167-175. JIANG Ji-sheng. A review of researches in khondalite series [J]. Journal of Changchun University of Earth Science, 1990, 20(2): 167-175.
[13] 黑龙江省地质矿产局. 黑龙江省区域地质志 [M]. 北京: 地质出版社, 1993:1-734. Heilongjiang Bureau of Geology and Mineral Resources. Regional geology of Heilongjiang Province [M]. Beijing: Geological Publishing House, 1993: 1-734.
[14] 李延河, 侯可军, 万德芳, 等. Algoma型和Superior型硅铁建造地球化学对比研究[J]. 岩石学报, 2012, 28(11): 3513-3519. LI Yan-he, HOU Ke-jun, WAN De-fang, et al. A compare geochemistry study for Algoma- and Superior-type banded iron formations[J]. Acta Petrologica Sinica, 2012, 28(11): 3513-3519.
[15] 姚凤良, 孙丰月. 矿床学教程 [M]. 北京: 地质出版社, 2006:1-254. YAO Feng-liang, SUN Feng-yue. Course of mineral deposit geology [M]. Beijing: Geological Publishing House, 2006:1-254.
[16] 周建波, 张兴洲, Wilde A S, 等. 中国东北~500 Ma泛非期孔兹岩带的确定及其意义 [J]. 岩石学报, 2011, 27(4): 1235-1245. ZHOU Jian-bo, ZHANG Xing-zhou, Wilde A S, et al. Confirming of the Heilongjiang ~500 Ma Pan-African khondalite belt and its tectonic implications [J]. Acta Petrologica Sinica, 2011, 27(4): 1235-1245.
[17] Wilde S A, 吴福元, 张兴洲. 中国东北麻山杂岩晚泛非期变质的锆石SHRIMP年龄证据及全球大陆再造意义 [J]. 地球化学, 2001, 30(1): 35-50. Wilde S A, WU Fu-yuan, ZHANG Xing-zhou. The Mashan complex: SHRIMP U-Pb zircon evidence for a Late Pan-African metamorphic event in NE China and its implication for global continental reconstructions [J]. Geochimica, 2001, 30(1): 35-50.
[18] 董策, 周建波. 中国东北地区西部~500 Ma泛非期孔兹岩系地球化学特征及其地质意义[J]. 岩石学报, 2012, 28(9): 2866-2878. DONG Ce, ZHOU Jian-bo. Geochemistry of~500 Ma Pan-African khondalite series in west of NE China and its tectonic implications [J]. Acta Petrologica Sinica, 2012, 28(9): 2866-2878.
[19] 赵华雷. 吉黑东部钨矿成因及成矿地球动力学背景: 博士学位论文 [D]. 长春: 吉林大学, 2014. ZHAO Hua-lei. Ore genesis and geodynamic setting of tungsten deposit in eastern Jilin and Heiongjiang Province: doctor's degree thesis [D]. Changchun: Jilin University, 2014.
[20] 金珍花, 张守志, 赵喜峰. 佳木斯隆起与周缘盆地间边界断裂特征研究 [J]. 世界地质, 2013, 32(2): 273-278. JIN Zhen-hua, ZHANG Shou-zhi, ZHAO Xi-feng. Jiamusi uplift and the boundary fractures of characteristics of surrounding basins [J]. Global Geology, 2013, 32(2): 273-278.
[21] Li J Y. Permian geodynamic setting of Northeast China and adjacent regions: closure of the Paleo-Asian and subduction of the Paleo-Pacific Plate [J]. Journal of Asian Earth Sciences, 2006, 26: 207-224.
[22] Wu F Y, Yang J H, Lo C H. Jiamusi Massif in China: a Jurassic accretionary terrane in the western Pasific [J]. The Island Arc, 1990, 16:156-172.
[23] Zhou J B, Simon A W, Zhang X Z. The onset of Pacific margin accretion in NE China: evidence from the Heilongjiang high-pressure metamorphic belt [J]. Tectonophysics, 1999, 478: 230-246.
[24] 黄映聪. 佳木斯地块古生代变质作用与构造演化: 博士学位论文 [D]. 长春: 吉林大学, 2009. HUANG Ying-cong. Paleozoic metamorphism and tectonic evolution of Jiamusi block: doctor's degree thesis [D]. Changchun: Jilin University, 2009.
[25] Faure G. Principles of isotope geology [M]. New York: John Wiley & Sons, 1986: 1-589.
[26] 吴元保, 郑永飞. 锆石成因矿物学研究及其对U-Pb年龄解释的制约 [J]. 科学通报, 2004, 49(16): 1589-1604. WU Yuan-bao, ZHENG Yong-fei. Zircon minerageny and its constraints on the explanation of U-Pb age [J]. Chinese Science Bulletin, 2004, 49(16): 1589-1604.
[27] 董策. 佳木斯地块构造演化:来自晚古生代沉积-火山岩的制约: 博士学位论文 [D]. 长春: 吉林大学, 2013. DONG Ce. Tectonic evolution of the Jiamusi Massif: constrains from Late Paleozoic sedimentary-volcanic rocks: doctor's degree thesis [D]. Changchun: Jilin University, 2013.
[28] 李厚民, 王登红, 李立兴, 等. 中国铁矿成矿规律及重点矿集区资源潜力分析 [J]. 中国地质, 2012, 39(3): 559-580. LI Hou-min, WANG Deng-hong, LI Li-xin, et al. Metallogeny of iron deposits and resource potential of major iron minerogenetic units in China [J]. Geology in China, 2012, 39(3): 559-580.
[29] 周建波, 曾维顺, 曹嘉麟, 等. 中国东北地区的构造格局与演化: 从500 Ma到180 Ma [J]. 吉林大学学报:地球科学版, 2012, 42(5): 1298-1329. ZHOU Jian-bo, ZENG Wei-shun, CAO Jia-lin, et al. The tectonic framework and evolution of the NE China: from ~500 Ma to ~180 Ma [J]. Journal of Jilin University: Earth Science Edition, 2012, 42(5): 1298-1329.