Records of the Late Jurassic Magmatic Arc in Heihe Area, Heilongjiang Province: Discussion on the Relationship with Mongolia-Okhotsk Ocean
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摘要: 黑龙江黑河北部的黑花山地区广泛发育中生代的侵入岩，但该侵入岩的形成时代、岩石组合、成因仍然不清.对黑花山地区侵入岩进行了野外、岩相学、岩石学、年代学、岩石地球化学等研究，以探讨该套岩石形成的时代、原因及大地构造背景.对两件二长花岗岩开展的LA-ICP-MS锆石U-Pb测年获得加权平均年龄分别为148.7±0.6 Ma、153.50±0.56 Ma，表明其形成于晚侏罗世.岩石组合主要为含有少量英云闪长岩（T1）、奥长花岗岩（T2）的T1T2G（狭义花岗岩）组合，即弧环境的侵入岩组合.上述岩石组合富硅、碱、高钾、过铝（A/CNK大于1）、低Fe2O3T.其在SiO2-K2O图上为高钾钙碱系列，硅镁图中为低铁钙碱（LF-LA）系列，Peacock指数为钙碱性或碱钙性，痕量元素蛛网图显示富集大离子亲石元素，亏损Nb、Ta、P、Ti、Y、Yb等元素.稀土元素配分模式为右倾型，轻稀土相对富集，（La/Yb）n=13.78~29.85，无负Eu异常或弱正Eu异常或弱的Eu负异常.花岗岩类具有高Sr低Y的特征，Sr/Y比值介于29.53~103.80，具有“C型”埃达克岩的特征.上述岩石组合及其特征均指示了弧火成岩的性质，结合构造环境判别认为该区晚侏罗世花岗岩类形成于蒙古-鄂霍茨克洋的南向俯冲有关的环境，岩浆可能源于兴安弧加厚下地壳的部分熔融作用.Abstract: The Mesozoic intrusive rocks are widely developed in Heihuashan area in the north of Heihe City, Heilongjiang Province, but the formation age, rock assemble age and genesis of the intrusive rocks are still unclear. In this paper, the intrusive rocks in Heihuashan area have been studied in the field, petrography, petrology, geochronology and petrochemistry, in order to discuss the formation age, petrogenesis and geotectonic background of these rocks, For two monzonitic granites, the weighted average ages of zircon U-Pb dating by LA-ICP-MS are 148.7±0.6 Ma and 153.50±0.56 Ma respectively, indicating that they were formed in the Late Jurassic. The intrusive rock assemblage of tonalite(T1), trondhjemite(T2), and granite(G) etc indicates a rock assembleage of T1T2G in arc environment. The above granitoids are rich in silicon, alkali, high potassium, peraluminium (A/CNK is greater than 1), and low in Fe2O3T. The rocks belong to high potassium calcium alkali series in the SiO2-K2O diagram, low Fe- calcium alkali (LF-CA) series in SiO2-MgO diagram and calcium alkali or alkali calcium in SiO2-(Na2O+K2O-CaO)diagram. The distribution pattern of rare earth element is right-leaning, with LREE relatively enriched and HREE depleted, giving (La/Yb)n=13.78-29.85 and no negative Eu anomaly or weak positive Eu anomaly or weak negative Eu anomaly.The granitoids are characterized by high Sr and low Y, with Sr/Y ratio ranging from 29.53 to 103.80, which are characteristic of "C-type" adakites. The above rock assemblages and their characteristics all indicate the properties of arc igneous rocks. Combined with the tectonic environment, it is believed that the Late Jurassic granitoids in this area were formed in the southwardly subduction environment of the Mongolia-Okhotsk Ocean.The magma maybe derived from the partial melting of the thickening lower crust of Xing'an Arc.
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Key words:
- Heihuashan area /
- Heihe, Heilongjiang Province /
- granitoids /
- geochemistry /
- Late Jurassic /
- magmatic arc
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图 1 大地构造位置简图(a)和黑花山地区区域地质简图(b)
1.古元古界兴华渡口岩群黑云斜长片麻岩; 2.新元古界落马湖岩群北宽河组大理岩; 3.新元古界落马湖岩群嘎拉山岩组黑云石英片岩; 4.晚侏罗世二长花岗岩; 5.早侏罗世花岗闪长岩; 6.白垩系龙江组安山岩; 7.早白垩世二长花岗岩; 8.早白垩世花岗闪长岩; 9.龙江期辉长岩脉; 10.早白垩世石英正长斑岩脉; 11.第四系; 12.本文采样点; 13.钼矿; 14.研究区15.收集前人的采样点；根据赵焕利和李仰春（2009)修改
Fig. 1. Geotectonic location sketch map and regional geological map of the study area
图 2 黑花山地区花岗岩类野外与显微照片
a.含钾长石巨斑花岗岩；b.似斑状花岗岩；c.似斑状二长花岗岩单偏光显微镜下；d.似斑状二长花岗岩正交偏光显微镜下；e.二长花岗岩单偏光显微镜下；d.二长花岗岩正交偏光显微镜下；g.二长花岗岩单偏光显微镜下；h.二长花岗岩正交偏光显微镜下；Pl.斜长石；Kf.钾长石；Bt.黑云母；Q.石英
Fig. 2. Field photos and microscopic photos of the granitoids in Heihuashan area
图 3 SJY20160813-1样品锆石阴极发光图像（单位：Ma）
Fig. 3. Cathodoluminescence images of zircon from sample SJY20160813-1
图 4 SJY20160813-6样品锆石阴极发光图像（单位：Ma）
Fig. 4. Cathodoluminescence images of zircon from sample SJY20160813-6
图 5 黑花山地区花岗岩的LA-ICP-MS锆石U-Pb年龄谐和图
Fig. 5. Zircon LA-ICP-MS U-Pb concordia diagrams of the granitoids in Heihuashan area
图 6 TAS图解（a）及TTG类判别图解（b）
a.据Eric（1994），图中虚线为碱性和亚碱性分界线, 据Irvine and Baragar（1971）; b.据O’Connor（1965）
Fig. 6. TAS diagram(a)and TTG type discrimination diagram of granite(b)
图 10 黑花山地区侵入岩痕量元素原始地幔标准化蛛网图（a）和稀土元素球粒陨石标准化配分模式图（b）（标准化值据Sun and McDonough, 1989）
Fig. 10. Primitive mantle normalized trace element spider diagrams(a) and chondrite-normalized REE patterns(b) of granitic rocks in Heihuashan area(modified from Sun and McDonough, 1989)
图 11 黑花山地区侵入岩的Sr/Y-Y图
Fig. 11. Diagram of Sr/Y-Y of intrusive rocks in Heihuashan area
图 12 SiO2-MgO图
HT-HMA.高温-高镁安山岩; MT-HMA.中温-高镁安山岩; LT-HMA.低温-高镁安山岩; 据邓晋福（2010）
Fig. 12. SiO2-MgO diagram
图 13 构造环境判别图
VAG.火山弧花岗岩；WPG.板内花岗岩；syn-COLG.同碰撞花岗岩；ORG.洋中脊玄武岩；据Pearce et al.（1984）
Fig. 13. Discrimination diagrams of tectonic setting
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[1] Andersen, T., 2002. Correction of Common Lead in U-Pb Analyses that do not Report 204Pb. Chemical Geology, 192(1/2):59-79. https://doi.org/10.1016/s0009-2541(02)00195-x http://www.ingentaconnect.com/content/el/00092541/2002/00000192/00000001/art00005 [2] Arculus, R. J., 2003. Use and Abuse of the Terms Calcalkaline and Calcalkalic. Journal of Petrology, 44(5):929-935. https://doi.org/10.1093/petrology/44.5.929 [3] Castillo, P.R., 2012.Adakite Petrogenesis.Lithos, 134/135:304-316. https://doi.org/10.1016/j.lithos.2011.09.013 [4] Chu, S.X., Liu, J.M., Xu, J.H., et al., 2012. Zircon U-Pb Dating, Petrogenesis and Tectonic Significance of the Granodiorite in the Sankuanggou Skarn Fe-Cu Deposit, Heilongjiang Province. Acta Petrologica Sinica, (2):433-450(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201202008 [5] Deng, J.F., Feng, Y.F., 2015. Specification of Tectonic Map of Intrusive Rocks in China. Geological Press, Beijing(in Chinese with English abstract). [6] Deng, J.F., Liu, C., Di, Y.J., et al., 2016. Crustal Convergent and Accretional Consumption Zones, and Continent-Continent Collisional Orogenes and Subduction-Accretional Orogenes:Records from the Igneous Petrotectonic Assemblages. Earth Science Frontiers, 23(6):34-41(in Chinese with English abstract). http://www.researchgate.net/publication/316515179_Crustal_convergent_and_accretional_consumption_zones_and_continent-continent_collisional_orogenes_and_subduction-accretional_orogenes_Records_from_the_igneous_petrotectonic_assemblages [7] Deng, J.F., Liu, C., Di, Y.J., et al., 2018. Tonalite Trondhjemite Granodiorite (TTG) Rock Structural Association and Its Subclass Division. Earth Science Frontiers, 25(6):42-50. [8] Deng, J.F., Liu, C., Feng, Y.F., et al., 2010. High Magnesian Andesitic/Dioritic Rocks(HMA)and Magnesian Andesitic/Dioritic Rocks(MA):Two Igneous Rock Types Related to Oceanic Subduction. Chinese Geology, 37(4):1112-1118(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DIZI201004027.htm [9] Dong, Y., Ge, W. C., Yang, H., et al., 2016. Geochronology, Geochemistry, and Hf Isotopes of Jurassic Intermediate-Acidic Intrusions in the Xing'an Block, Northeastern China:Petrogenesis and Implications for Subduction of the Paleo-Pacific Oceanic Plate. Journal of Asian Earth Sciences, 118:11-31. https://doi.org/10.1016/j.jseaes.2016.01.006 [10] Eric, A.K., 1994. Naming Materials in the Magma/Igneous Rock System. Earth-Science Reviews, 37:215-224. doi: 10.1016/0012-8252(94)90029-9 [11] Ge, W.C., Lin, Q., Sun, D.Y., et al., 1999. Geochemical Characteristics of the Mesozoic Basalts in Da Hinggan Ling:Evidence of the Mantle-Crust Interaction. Acta Petrologica Sinica, 15(3):396-407(in Chinese with English abstract). http://www.researchgate.net/publication/279540240_Geochemical_characteristics_of_the_Mesozoic_basalts_in_Da_Hinggan_Ling_Evidence_of_the_mantle-crust_interaction [12] Gou, J., Sun, D.Y., Li, R., et al., 2013. Geochronology, Geochemistry and Petrogenesis of the Early Mesozoic Granites in the Sunwu-Jiayin Area, Heilongjiang Province. Journal of Jilin Unviersity: Earth Science Edition, 43:119-133(in Chinese with English abstract). http://www.researchgate.net/publication/285737712_Geochronology_geochemistry_and_petrogenesis_of_the_early_mesozoic_granites_in_the_Sunwu-Jiayin_area_Heilongjiang_province [13] Hu, Z. C., Liu, Y. S., Gao, S., et al., 2012. Improved in Situ Hf Isotope Ratio Analysis of Zircon Using Newly Designed X Skimmer Cone and Jet Sample Cone in Combination with the Addition of Nitrogen by Laser Ablation Multiple Collector ICP-MS. Journal of Analytical Atomic Spectrometry, 27(9):1391. https://doi.org/10.1039/c2ja30078h [14] Irvine, T. N., Baragar, W. R. A., 1971. A Guide to the Chemical Classification of the Common Volcanic Rocks. Canadian Journal of Earth Sciences, 8(5):523-548. https://doi.org/10.1139/e71-055 [15] Jackson, S. E., Pearson, N. J., Griffin, W. L., et al., 2004. The Application of Laser Ablation-Inductively Coupled Plasma-Mass Spectrometry to in Situ U-Pb Zircon Geochronology. Chemical Geology, 211(1/2):47-69. https://doi.org/10.1016/j.chemgeo.2004.06.017 http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=17d96cdc3a96b2aa4c52b4ebb0b5da26 [16] Li, J.Y., 2009. Cycles and Stages of Geological History of China Mainland. Chinese Geology, 3:504-527(in Chinese with English abstract) http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgdizhi200903003 [17] Lin, Q., Ge, W.C., Wu, F.Y., et al., 2004. Geochemistry of Mesozoic Granitoids in Daxinganling. Acta Petrologica Sinica, 20(3):403-412(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=gjsdz202003001 [18] Liu, C., Deng, J.F., Xu, L.Q., et al., 2011. A Preliminary Frame of Magma-Tectonic-Mo Metallogenic Events of Mesozoic Era in Da Hinggan Mountains and Xiao Hinggan Mountains Areas. Earth Science Frontiers, 3:166-178(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy201103014 [19] Liu, Y. S., Hu, Z. C., Gao, S., et al., 2008. In Situ Analysis of Major and Trace Elements of Anhydrous Minerals by LA-ICP-MS without Applying an Internal Standard. Chemical Geology, 257(1/2):34-43. https://doi.org/10.1016/j.chemgeo.2008.08.004 http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=babd721ac13e2675d9485b52683be64c [20] Liu, Y. S., Hu, Z. C., Zong, K. Q., et al., 2010b. Reappraisement and Refinement of Zircon U-Pb Isotope and Trace Element Analyses by LA-ICP-MS. Chinese Science Bulletin, 55(15):1535-1546. https://doi.org/10.1007/s11434-010-3052-4 [21] Liu, Y., Gao, S., Hu, Z., et al., 2010a. Continental and Oceanic Crust Recycling-Induced Melt-Peridotite Interactions in the Trans-North China Orogen:U-Pb Dating, Hf Isotopes and Trace Elements in Zircons from Mantle Xenoliths. Journal of Petrology, 51(1/2):537-571. https://doi.org/10.1093/petrology/egp082 https://academic.oup.com/petrology/article-abstract/51/1-2/537/1463381 [22] Ludwig, K.R., 2001. Users Manual for Isoplot/Ex Rev.2.49. Berkeley Geochronology Centre Special Publication, Berkeley, 1: 56. [23] Maniar, P. D., Piccoli, P. M., 1989. Tectonic Discrimination of Granitoids. Geological Society of America Bulletin, 101(5):635-643. https://doi.org/10.1130/0016-7606(1989)101 < 0635:tdog > 2.3.co; 2 doi: 10.1130/0016-7606(1989)101<0635:TDOG>2.3.CO;2 [24] O'Connor, J.T., 1965.A Classification for Quartz-Rich Igneous Rocks Based on Feldspar Ratios. U.S. Geol. Surv. Prof. Paper, 525:79-84. http://ci.nii.ac.jp/naid/10011069261 [25] Parfenov, L. M., Popeko, L. I., Tomurtogoo, O., 1999. Problems of the tectonics of the Mongolia-Okhotsk Orogenic Belt. Tikhookean Geol., 18:24-43 http://ci.nii.ac.jp/naid/10007185568 [26] Pearce, J. A., Harris, N. B. W., Tindle, A. G., 1984. Trace Element Discrimination Diagrams for the Tectonic Interpretation of Granitic Rocks. Journal of Petrology, 25(4):956-983. https://doi.org/10.1093/petrology/25.4.956 [27] Peccerillo, A., Taylor, S. R., 1976. Geochemistry of Eocene Calc-Alkaline Volcanic Rocks from the Kastamonu Area, Northern Turkey. Contributions to Mineralogy and Petrology, 58(1):63-81.https://doi.org/10.1007/bf00384745 doi: 10.1007/BF00384745 [28] Peng, Y.J., Qi, C.D., Zhou, X.D., et al., 2012. Transition form Paleo-Asian Ocean Domain to Circun-Pacific Ocean Domain for the Ji-Hei Composite Orogenic Belt:Time Mark and Relationship to Global Tectonics. Geology and Resources, 21(3):261-265(in Chinese with English abstract). http://www.researchgate.net/publication/288818155_Transition_from_Paleo-Asian_ocean_domain_to_circum-pacific_ocean_domain_for_the_Jihei_composite_orogenic_belt_Time_mark_and_relationship_to_global_tectonics [29] Shao, J.A., Zhang, L.Q., Xiao, Q.H., et al., 2005. Uplift of Daxinganling in Mesozoic:A Possible Mechanism of Intracontinental Orogeny. Acta Petrologica Sinica, 21:789-794(in Chinese with English abstract). http://www.oalib.com/paper/1473756 [30] Shao, S., Deng, J.F., Liu, C., et al., 2018. Geochemical Characteristics and Tectonic Setting of Early Cretaceous Volcanic Rocks in the Heihe Area, Heilongjiang Province, China. Earth Science Frontiers, 25(3):215-229(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy201803018 [31] She, H.Q., Li, J.W., Xiang, A.P., et al., 2012. U-Pb Ages of the Zircons from Primary Rocks in Middle-Northern Daxinganling and Its Implications to Geotectonic Evolution. Acta Petrologica Sinica, 28:571-594(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201202018 [32] Sheng, H.Y., 2018. New Breakthrough in Geological Exploration of Heihe City. Heilongjiang Land and Resources, (3):12(in Chinese with English abstract). [33] Sláma, J., Košler, J., Condon, D. J., et al., 2008. Plešovice Zircon:A New Natural Reference Material for U-Pb and Hf Isotopic Microanalysis. Chemical Geology, 249(1/2):1-35. https://doi.org/10.1016/j.chemgeo.2007.11.005 http://www.researchgate.net/publication/290802854_Zircon_M257_-_A_homogeneous_natural_reference_material_for_U-Pb_and_Hf_isotopic_microanalysisJ [34] Sui, Z.M., Ge, W.C., Wu, F.Y., et al., 2006. Zircon U-Pb Age and Genesis of Halabaqi Granite in the Northeast of Daxinganling. Global Geology, 3:229-236(in Chinese with English abstract). [35] Sui, Z.M., Ge, W.C., Wu, F.Y., et al., 2007. Zircon U-Pb Ages, Geochemistry and Its Petrogenesis of Jurassic Granites in Northeastern Part of the Da Hinggan Mts. Acta Petrologica Sinica, 23:461-480(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200702023 [36] Sui, Z.M., Ge, W.C., Xu, X.C., et al., 2009. Characteristics and Geological Significance of Late Paleozoic Post Orogenic Granites in the 12th Station of Daxinganling. Acta Petrologica Sinica, 25:2679-2686(in Chinese with English abstract). [37] Sui, Z.M., Xu, X.C., 2010. Sr-Nd Isotopic Characteristics of Jurassic Granites in Northeastern Daxing'anling and Its Geological Significance. Geology China, 37(1):48-55(in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTOTAL-DIZI201001008.htm [38] Sun, S. S., McDonough, W. F., 1989. Chemical and Isotopic Systematics of Oceanic Basalts:Implications for Mantle Composition and Processes. Geological Society, London, Special Publications, 42(1):313-345. https://doi.org/10.1144/gsl.sp.1989.042.01.19 doi: 10.1144/GSL.SP.1989.042.01.19 [39] Tang, J., Xu, W. L., Wang, F., et al., 2014. Geochronology and Geochemistry of Early-Middle Triassic Magmatism in the Erguna Massif, NE China:Constraints on the Tectonic Evolution of the Mongol-Okhotsk Ocean. Lithos, 184-187:1-16. https://doi.org/10.1016/j.lithos.2013.10.024 [40] Tang, J., Xu, W. L., Wang, F., et al., 2015a. Geochronology, Geochemistry, and Deformation History of Late Jurassic-Early Cretaceous Intrusive Rocks in the Erguna Massif, NE China:Constraints on the Late Mesozoic Tectonic Evolution of the Mongol-Okhotsk Orogenic Belt. Tectonophysics, 658:91-110. https://doi.org/10.1016/j.tecto.2015.07.012 [41] Tang, J., Xu, W. L., Wang, F., et al., 2015b. Early Mesozoic Southward Subduction History of the Mongol-Okhotsk Oceanic Plate:Evidence from Geochronology and Geochemistry of Early Mesozoic Intrusive Rocks in the Erguna Massif, NE China. Gondwana Research, 31:218-240. https://doi.org/10.1016/j.gr.2014.12.010 http://smartsearch.nstl.gov.cn/paper_detail.html?id=6b9afb8de74d9ea97a7699d4214262ac [42] Wang, T., Guo, L., Zhang, L., et al., 2015. Timing and Evolution of Jurassic-Cretaceous Granitoid Magmatisms in the Mongol-Okhotsk Belt and Adjacent Areas, NE Asia:Implications for Transition from Contractional Crustal Thickening to Extensional Thinning and Geodynamic Settings. Journal of Asian Earth Sciences, 97:365-392. https://doi.org/10.1016/j.jseaes.2014.10.005 [43] Wang, T., Zhang, L., Guo, L., et al., 2014. Preliminary Compilation of Mesozoic Granite Map in Asia and Some Research Progress. Journal of Earth, 35:655-672(in Chinese with English abstract). [44] Wiedenbeck, M., Hanchar, J. M., Peck, W. H., et al., 2004. Further Characterisation of the 91500 Zircon Crystal. Geostandards and Geoanalytical Research, 28(1):9-39. https://doi.org/10.1111/j.1751-908x.2004.tb01041.x doi: 10.1111/j.1751-908X.2004.tb01041.x [45] Wu, F. Y., Sun, D. Y., Ge, W. C., et al., 2011. Geochronology of the Phanerozoic Granitoids in Northeastern China. Journal of Asian Earth Sciences, 41(1):1-30. https://doi.org/10.1016/j.jseaes.2010.11.014 http://www.sciencedirect.com/science/article/pii/S1367912010003391 [46] Wu, F.Y., Sun, D.Y., Lin, Q., 1999. Petrogenesis of the Phanerozoic Granites and Crustal Growth in Northeast China. Acta Petrologica Sinica, 15:181-189(in Chinese with English abstract). http://www.oalib.com/paper/1471776 [47] Xu, W.L., Wang, F., Pei, F.P., et al., 2013. Mesozoic Tectonic Regimes and Regional Ore-Forming Background in NE China:Constraints from Spatial and Temporal Variations of Mesozoic Volcanic Rock Associations. Acta Petrologica Sinica, 29(2):339-353(in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical_ysxb98201302001.aspx [48] Zhang, L.L., Liu, C., Zhou, S., et al., 2014. Characteristics of Ore-Bearing Granites and Ore-Forming Age of the Huojihe Molybdenum Deposit in Lesser Xing'an Range. Acta Petrologica Sinica, 11:3419-3431(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201411024 [49] Zhang, Q., Xu, J.F., Wang, Y., et al., 2004. Diversity of Adakite. Geological Bulletin, 23(9-10):959-965(in Chinese with English abstract). http://www.zhangqiaokeyan.com/academic-journal-cn_geological-bulletin-china_thesis/0201252292610.html [50] Zhang, S., Liu, J.J., Yuan, F., et al., 2019. Zricon U-Pb Geochronology and Geochemistry of Granites and Pegmatites, and Metallogenesis of Related Uranium from the Chenjiazhuang Deposit, Shaanxi Province. Earth Science Frontiers, 26(4):270-289(in Chinese with English abstract). [51] Zhao, H.L., Li, Y.C., 2009. Regional Geological Survey Report of the People's Republic of Chin:1:250 000 Map Heihe. Geological Survey and Research Institute of Heilongjiang Province, Haerbin, 1-369(in Chinese with English abstract). [52] Zhao, Y.D., Che, J.Y., Xu, F.M., et al., 2018. Late Jurassic Adakitic Granites in Northeastern Xing'an Block:Geochronology and Geochemical Characteristics and Tectonic Significance. Earth Science Frontiers, 25(6):240-253(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DXQY201806022.htm [53] Zhao, Y.D., Xu, F.M., Zhao, J., et al., 2017. New Discovery of Late Mesozoic Porphyry Molybdenum (Copper) Deposits in the Northwest of Heihe. Address Theory, 63(S1):207-208(in Chinese with English abstract). http://journals.cambridge.org/article_S0016756817000267 [54] Zonenshain, L.P., Kuzmin, M.I., Natapov, L.M., 1990. Geology of the USSR:A Plate Tectonic Synthesis. Geodynamic Monograph, 21:242. doi: 10.1029/GD021 [55] 褚少雄, 刘建明, 徐九华, 等, 2012.黑龙江三矿沟铁铜矿床花岗闪长岩锆石U-Pb定年、岩石成因及构造意.岩石学报, (2):433-450. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201202008 [56] 邓晋福, 冯艳芳, 2015.中国侵入岩大地构造图说明书.北京:地质出版社. [57] 邓晋福, 刘翠, 冯艳芳, 等, 2010.高镁安山岩/闪长岩类(HMA)和镁安山岩/闪长岩类(MA):与洋俯冲作用相关的两类典型的火成岩类.中国地质, 37(4):1112-1118. doi: 10.3969/j.issn.1000-3657.2010.04.025 [58] 邓晋福, 刘翠, 狄永军, 等, 2016.地壳对接消减带和叠接消减带与陆-陆碰撞造山和俯冲增生造山:来自侵入岩构造组合的记录.地学前缘, 23(6):34-41. http://d.wanfangdata.com.cn/Periodical/dxqy201606004 [59] 邓晋福, 刘翠, 狄永军, 等, 2018.英云闪长岩-奥长花岗岩-花岗闪长岩(TTG)岩石构造组合及其亚类划分.地学前缘, 25(6):42-50. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy201806005 [60] 葛文春, 林强, 1999.大兴安岭中生代玄武岩的地球化学特征:壳幔相互作用的证据.岩石学报, (3):396-407. http://www.cnki.com.cn/Article/CJFDTotal-YSXB199903007.htm [61] 苟军, 孙德有, 李蓉, 等, 2013.孙吴-嘉荫地区早中生代花岗岩的年代学、地球化学与成因.吉林大学学报(地球科学版), 43:119-133. http://www.cqvip.com/QK/91256B/201301/45062591.html [62] 李锦轶, 2009.中国大陆地质历史的旋回与阶段.中国地质, 3:504-527. doi: 10.3969/j.issn.1000-3657.2009.03.003 [63] 林强, 葛文春, 吴福元, 等, 2004.大兴安岭中生代花岗岩类的地球化学.岩石学报, 20(3):403-412. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200403004 [64] 刘翠, 邓晋福, 徐立权, 等, 2011.大兴安岭-小兴安岭地区中生代岩浆-构造-钼成矿地质事件序列的初步框架.地学前缘, 3:166-178. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy201103014 [65] 彭玉鲸, 齐成栋, 周晓东, 等, 2012.吉黑复合造山带古亚洲洋向滨太平洋构造域转换:时间标志与全球构造的联系.地质与资源, 21(3):261-265. doi: 10.3969/j.issn.1671-1947.2012.03.001 [66] 邵济安, 张履桥, 肖庆辉, 等, 2005.中生代大兴安岭的隆起——一种可能的陆内造山机制.岩石学报, 21:789-794. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200503018 [67] 邵帅, 邓晋福, 刘翠, 等, 2018.黑龙江黑河地区早白垩世火山岩岩石地球化学特征及其构造环境意义.地学前缘.25(3):215-229。 http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy201803018 [68] 佘宏全, 李进文, 向安平, 等, 2012.大兴安岭中北段原岩锆石U-Pb测年及其与区域构造演化关系.岩石学报, 28:571-594. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201202018 [69] 盛海燕, 2018.黑河市地质勘查取得新突破.黑龙江国土资源, (3):12。 [70] 隋振民, 葛文春, 吴福元, 等, 2006.大兴安岭东北部哈拉巴奇花岗岩体锆石U-Pb年龄及其成因.世界地质, 3:229-236. doi: 10.3969/j.issn.1004-5589.2006.03.003 [71] 隋振民, 葛文春, 吴福元, 等, 2007.大兴安岭东北部侏罗纪花岗质岩石的锆石U-Pb年龄、地球化学特征及成因.岩石学报, 23:461-480. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200702023 [72] 隋振民, 葛文春, 徐学纯, 等, 2009.大兴安岭十二站晚古生代后造山花岗岩的特征及其地质意义.岩石学报, 25:2679-2686. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200910031 [73] 隋振民, 徐学纯, 2010.大兴安岭东北部侏罗纪花岗岩类Sr-Nd同位素特征及其地质意义.中国地质, 37(1):48-55. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgdizhi201001005 [74] 王涛, 张磊, 郭磊, 等, 2014.亚洲中生代花岗岩图初步编制及若干研究进展.地球学报, 35:655-672. doi: 10.3975/cagsb.2014.06.01 [75] 吴福元, 孙德有, 林强, 1999.东北地区显生宙花岗岩的成因与地壳增生.岩石学报, 15:181-189. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98199902003 [76] 许文良, 王枫, 裴福萍, 等, 2013.中国东北中生代构造体制与区域成矿背景:来自中生代火山岩组合时空变化的制约.岩石学报, 29(2):339-353. http://d.old.wanfangdata.com.cn/Periodical_ysxb98201302001.aspx [77] 张琳琳, 刘翠, 周肃, 等, 2014.小兴安岭霍吉河钼矿区含矿花岗岩类特征及成矿年龄.岩石学报, 11:3419-3431. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201411024 [78] 张旗, 许继峰, 王焰, 等, 2004.埃达克岩的多样性.地质通报, 23(9-10):959-965. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgqydz200409020 [79] 张帅, 刘家军, 袁峰, 等, 2019.陕西商丹陈家庄铀矿区花岗岩体和伟晶岩脉的U-Pb年龄、地球化学特征与铀成矿作用.地学前缘, 26(5):270-289. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy201905018 [80] 赵焕利, 李仰春, 2009.中华人民共和国区域地质调查报告1: 25万黑河市幅., 哈尔滨: 黑龙江省地质调查研究总院, 1-369. [81] 赵院冬, 车继英, 许逢明, 等, 2018.兴安地块东北部晚侏罗世C型埃达克质花岗岩年代学、地球化学特征及构造环境意义.地学前缘, 25(6):240-253. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy201806019 [82] 赵院冬, 许逢明, 赵君, 等, 2017.黑河西北新发现晚中生代斑岩型钼(铜)矿特征.地质论评, 63(S1):207-208. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=9146566 -
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