Tracing Archives of Ocean Plate Geology and Tracking Plate Tectonics from the Neoarchean Granite-Greenstone Belt of the Western Shandong Province
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摘要: 鲁西地区是我国新太古代经典的花岗岩-绿岩带出露地区之一，前人已积累了丰硕的构造地层、同位素地质年龄、地球化学及成矿作用等方面的资料，并对这一时期的地球动力学特征进行了讨论.通过研究“洋板块地质”的思路综合前人已获得的区域地质调查研究资料，表明泰山岩群镁铁质火山岩演化是一套由科马提岩-拉斑玄武岩和拉斑玄武岩、钙碱性玄武岩及安山岩等两类岩石组合复合而成的火山岩系，反映了相对早期形成与洋内地幔柱有关的科马提岩向相对晚期与弧有关的钙碱性玄武岩-安山岩的演化过程；新太古代初期形成岛弧型英云闪长岩带到新太古代中期形成分异型奥长花岗岩，则反映了俯冲过程中的花岗岩演化特点；新太古代晚期硅质高镁玄武岩（高镁玄武安山岩）的确定则是活动大陆边缘岩浆弧的产物；泰山岩群中红宝石（刚玉）的发现，进一步指示其形成的背景与新太古代板块构造俯冲作用有关，为鲁西存在新太古代洋板块地质遗迹提供了地质学证据.Abstract: The Luxi district which is located in West Shandong Province is one of the most representative granite-greenstone belts in the Neoarchean of China. Our pioneers have already accumulated rich sources related to tectonic lithostratigraphy, isotopic geochronology, geochemistry, mineralization, and etc. Some geologists also explores progressively the geodynamic features in this era. From the perspective of ocean plate geology, this article examines the previous data of regional geological investigation and research obtained by the predecessors, and shows that the mafic volcanic rocks of the Taishan Complex are composed of two rock associations, komatite-tholeiite and tholeiite-calc alkaline basalt-andesite, respectively. It reflects the evolution process from komatite related to mantle plume in the early stage to calc alkaline basalt-andesite related to arc in the late stage. From island arc type tonalite formed in the early stage of Neoarchean to differentiated trondhjemite formed in the middle stage of Neoarchean, it reflects the characteristics of granite evolution during subduction. The late Neoarchean Siliceous High Mg Basalt is the product of the active continental margin magma arc. The discovery of Ruby in the Taishan Complex further indicates that the setting of its formation is related to the subduction of Neoarchean plates. All these provide geological evidence for the existence of new Archean oceanic plate in Luxi District.
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Key words:
- western Shandong Province /
- Neoarchean /
- ocean plate geology /
- plate tectonics /
- tectonics
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图 1 鲁西地区前寒武纪地(岩)层分布略图
1.显生宙地层; 2.济宁岩群; 3.泰山岩群; 4.沂水岩群; 5.钾长花岗岩; 6.石英二长岩; 7.黑云母二长花岗岩; 8.二长花岗岩; 9.片麻状英云闪长岩; 10.推断断层; 11.断层带; 12.地层构造分区; 据宋志勇等(1994)
Fig. 1. Sketch map of Precambrian rocks in western Shandong Province
图 2 鲁西新太古代侵入岩空间分带示意图
据万渝生等(2015a)；其中：A.傲徕山岩浆弧；B.泰山-蒙阴岩浆弧；C.肥城-枣庄岩浆弧
Fig. 2. Sketch map of Neoarchean intrusive rocks in western Shandong Province
图 3 鲁西新太古代构造环境的简化模型
指示TTG、高硅(HAS)、低硅埃达克岩(LSA；赞岐岩类)和硅质高镁玄武岩的岩浆背景(据Peng et al., 2013)
Fig. 3. Simplified model of the tectonic and magmatic evolution of Late Archean
图 4 山东省新泰龙廷地区地质略图
1.第四系；2.古元古代辉绿岩（脉）；3.新太古代晚期二长花岗岩；4.新太古代中期花岗闪长质片麻岩；5.新太古代中期变质辉长岩；6.壳源岩石包体；7.含有红刚玉的暗色岩石包体；8.实测、推测断层；据张增奇（2012)
Fig. 4. Geological sketch map of Longting area, Xintai, Shandong Province
图 5 刚玉被绿色含铬白云母集合体包裹
Fig. 5. Corundum encapsulated in green chromium-bearing Muscovite aggregates
图 6 (a) 太平洋型俯冲带，形成硬玉岩；(b)大陆碰撞带，形成红宝石
HP.高压; UHP.超高压; 据Stern et al.(2013)
Fig. 6. (a) Pacific type subduction zone, forming jadeite; (b) Continental collision zone, forming ruby
表 1 泰山岩群岩石组合类型及划分(据万渝生等，2012修改)
Table 1. Litho⁃assemblages and classification of Taishan Complex (modified from Wan et al., 2012)
岩石组合序列 建议划分命名 与原划分方案关系(王世进等, 2012) 新划分的方案 主要岩石组合 推测形成的构造环境 第Ⅱ组合 泰山岩群 上亚岩群 原柳行岩组上段 柳行岩组 含砾石层夹层的变碎屑岩 大陆斜坡海下扇中-上部为主 山草峪岩组 山草峪岩组 变碎屑岩为主 大陆斜坡海下扇下部为主 第Ⅰ组合 下亚岩群 (柳行岩组下段)雁岭关岩组 孟家屯岩组 变玄武岩与变碎屑岩、石英岩 与弧有关的岩石组合特点 孟家屯岩组 雁岭关岩组 科马提岩及变玄武岩 洋板块形成的MORB、OPB等 
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表 2 泰山主要侵入岩体锆石U⁃Pb年龄测定结果
Table 2. Zircon U-Pb dating of major intrusive rocks in Mount Taishan
采样地点 测年样品岩石类型 年龄数据与测试方法 年代范围 资料来源 泰山红门 辉绿玢岩（岩墙） 1 621.1±8.8 Ma斜锆石U-Pb 中元古代早期 陆松年等(2008) 1 632.4±4.2 Ma斜锆石U-Pb 相振群等(2012) 泰山普照寺 细粒闪长岩 2 480.1±6.8 Ma (S) 新太古代晚期 陆松年等(2008) 泰山泰澳山庄 细粒闪长岩 2 481±17 Ma (S) 泰山中天门 二长闪长岩 2 479±65 Ma (L) 泰山傲徕山黑龙潭瀑布长寿桥侧 二长花岗岩 2 520.5±8.5 Ma (S) 泰山玉皇顶 片麻状石英闪长岩 2 523±16 Ma (L) 泰山大众桥 片麻状石英闪长岩 2 551±28 Ma (L) 黄前水库 英云闪长岩 2 557±20 Ma (S) 泰山玉皇顶 花岗岩 2 561±23 Ma (S) 栗杭村公路边 白色长英质脉 2 609±19 Ma (S) 新太古代中期 陆松年等(2008) 栗杭村 奥长花岗片麻岩 2 611±19 Ma (S) 上港 奥长花岗片麻岩 2 623±9 Ma (S) 王世进等(2012) 新甫山 片麻状花岗闪长岩 2 625±15 Ma (S) 栗杭村 英云闪长片麻岩 2 627±18 Ma (S) 陆松年等(2008) 泰山望府山十八盘 英云闪长片麻岩 2 637±22 Ma (L) 泰山彩石溪 白色长英质脉 2 663±16 Ma (L) 新太古代早期 陆松年等(2008) 泰山彩石溪 斜长角闪岩 2 678±26 Ma (L) 徂徕山 英云闪长片麻岩 2 711±11 Ma (S) 万渝生等(2015a) 泰山桃花峪 英云闪长片麻岩 2 711±10 Ma (S) 王世进等(2012) 泰安钟秀山庄 英云闪长片麻岩 2 712±17 Ma (S) 栗杭村 闪长质片麻岩 2 741±47 Ma (L) 陆松年等(2008) 2 729±37 Ma (S)
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[1] Brown, G.C., 1982. Calc-Alkaline Intrusive Rocks: Their Diversity, Evolution and Relation to Volcanic Arcs. In: Thorpe, R. S., ed., Andesites. John Wiley & Sons, New York, 437-461. [2] Cao, G.Q., 1995. The Early Precambrain Crustal Evolution in Western Shandong. Shandong Geology, 11(2):1-14(in Chinese with English abstract). [3] Cao, G.Q., 1996. Early Precambrain Geology of Western Shandong. Geological Publishing House, Beijing, 1-210(in Chinese). [4] Cao, G.Q., Wang, Z., Dong, Y.J., et al., 1987. New Recognition on Some Geological Problems Related to the Early-Middle Precambrian in the Western Shandong Mountainous Region. Bulletin of the Chinese Academy of Geological Sciences, 16:189-200(in Chinese with English abstract). [5] Chen, Y.Q., 1994. Concise Regional Geology of China. Geological Publishing House, Beijing, 1-517(in Chinese). [6] Chen, Y.Q., Shen, Q.H., Wang, Z.J., 1982. Preliminary Study of the Metamorphosed Basic Volcano-Sedimentary Yanlingguan Formation of Taishan Group of Xintai, Shandong. Geological Publishing House, Beijing, 1-72 (in Chinese). [7] Chen, Y.Q., Xu, H.F., 1991. Some New Understanding of the Komatites in the Late Archean Yanlingguan Formation of Xintai, Shandong. Geology in China, 4:31-32 (in Chinese with English abstract). [8] Condie, K.C., 1982. Plate Tectonics and Crustal Evolution. Pergamon Oress, New York, 1-310. [9] Deng, J.F., Feng, Y.F., Di, Y.J., et al., 2015. Magmatic Arc and Ocean:Continent Transition:Discussion. Geological Review, 61(3):473-484(in Chinese with English abstract). http://cn.bing.com/academic/profile?id=adaba86d78fe17d6e628a02f2f3256fc&encoded=0&v=paper_preview&mkt=zh-cn [10] Deng, J.F., Liu, C., Di, Y.J., et al., 2018. Discussion on the Tonalite-Trondhjemite-Granodiorite (TTG) Petrotectonic Assemblage and Its Subtypes. Earth Science Frontiers, 25(6):42-50 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy201806005 [11] 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. Geology in China, 37(4), 1112-1118 (in Chinese with English abstract). http://cn.bing.com/academic/profile?id=9cd4bb0eb757170f16b82ba4483fdb7f&encoded=0&v=paper_preview&mkt=zh-cn [12] Deng, J.F., Luo, Z.H., Su, S.G., et al., 2004. Petrogenesis, Tectonic Environment and Mineralization. Geological Publishing House, Beijing, 1-318(in Chinese). [13] Deng, J.F., Xiao, Q.H., Su, S.G., et al., 2007. Igneous Petrotectonic Assemblages and Tectonic Settings:A Discussion. Geological Journal of China Universities, 13(3):392-402 (in Chinese with English abstract). http://cn.bing.com/academic/profile?id=a14262ce8afe00aa0316e1a98cceda67&encoded=0&v=paper_preview&mkt=zh-cn [14] Feng, Y.F., Deng, J.F., Wang, S.J., et al., 2010. The Recognition of the Magnesian Andesitic Series(MA)in the Precambrian Granitic Rocks in Western Shandong Province and the Continental Crustal Growth. Geology in China, 37(4):1119-1129(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgdizhi201004026 [15] Furnes, H., Dilek, Y., De Wit, M., 2015. Precambrian Greenstone Sequences Represent Different Ophiolite Types. Gondwana Research, 27:649-685. https://doi.org/10.1007/978-94-007-7615-9_1 [16] Jahn, B.M., Auvray, B., Shen, Q.H., et al., 1988. Archaean Crustal Evolution in China:The Taishan Complex, and Evidence for Juvenile Crustal Addition from Long-Term Depleted Mantle. Precambrian Research, (38):381-403. https://doi.org/10.1016/0301-9268(88)90035-6 [17] Kusky, T.M., Polat, A., Windley, B.F., et al., 2016. Insights into the Tectonic Evolution of the North China Craton through Comparative Tectonic Analysis:A Record of Outward Growth of Precambrian Continents. Earth-Science Reviews, 162:387-432. https://doi.org/10.1016/j.earscirev.2016.09.002 [18] Kusky, T.M., 2011. Geophysical and Geological Tests of Tectonicmodels of the North China Craton. Gondwana Res. 20: 26-35. https: //doi.org/10.1016/j.gr.2011.01.004 [19] Li, S.S., Santosh, M., Cen, K., et al., 2016. Neoarchean Convergent Margin Tectonics Associated with Microblock Amalgamation in the North China Craton:Evidence from the Yishui Complex. Gondwana Research, 38:113-131. https://doi.org/10.1016/j.gr.2015.11.004 [20] Li, T.D., Xiao, Q.H., Pan, G.T., et al., 2019. A Consideration about the Development of Ocean Plate Geology. Earth Science, 44(5):1441-1451(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqkx201905003 [21] Lu, S.N., Chen, Z.H., Xiang, Z.Q., 2008. Geochronologic Framework of Ancient Igneous Rocks in Taishan Worldpark. Geological Publishing House, Beijing, 1-90(in Chinese). [22] Lu, S.N., Hao, G.J., Wang, H.C., et al., 2017. Geotectonics of Metamorphic Rocks in China. Geological Publishing House, Beijing, 1-338(in Chinese with English abstract). [23] Lu, S.N., Hao, G.J., Wang, H.C., et al., 2015. A Booklet on Geotectonic Map of Metamorphic Rocks (1: 2 500 000) in China. Geological Publishing House, Beijing, 1-92(in Chinese). [24] Lu, S.N., Wang, H.C., Hao, G.J., et al., 2016. The Debate Concerning the Beginning of the Plate Tectonics.Geology in China, 43(3):709-720 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DIZI201603002.htm [25] Lu, S.N., Xiang, Z.Q., Wang, H.C., et al., 2019. Neoarchean Geological Evolution of Taishan Area (Upper Part). People Publishing House, Beijing, 1-267(in Chinese). [26] Lu, S.N., Zhao, G.C., Wang, H.C., et al., 2008. Precambrian Metamorphic Basement and Sedimentary Cover of the North China Craton:A Review. Precambrian Res., 160, 77-93. https://doi.org/10.1016/j.precamres.2007.04.017 [27] Maniard, P.D., Piccoli, P.M., 1989. Tectonic Discrimination of Granoids. Geological Society of America Bullietin, 101:635-643. https://doi.org/10.1016/j.precamres.2007.04.017 [28] Pan, G.T., Xiao, Q.H., Zhang, K.X., et al., 2019. Recognition of the Oceanic Subduction-Accretion Zones from the Orogenic Belt in Continents and Its Important Scientific Significance. Earth Science, 44(5):1544-1561(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqkx201905012 [29] Peng, T.P., Wilde, S.A., Fan, W.M., et al., 2013. Neoarchean Siliceous High-Mg Basalt (SHMB) from the Taishan Granite-Greenstone Terrane, Eastern North China Craton:Petrogenesis and Tectonic Implications. Precambrian Research, 228:233-249. https://doi.org/10.1016/j.precamres.2013.01.017 [30] Peng, T.P., Fan, W.M., Peng, B.X., 2012. Geochronology and Geochemistry of Late Archean Adakitic Plutons from the Taishan Granite-Greenstone Terrain: Implications for Tectonic Evolution of the Eastern North China Craton. Precambrian Research, (208-211): 53-71. https://doi.org/10.1016/j.precamres.2012.03.008 [31] Pitcher, W.S., 1983. Grenite Type and Tectonic Environment. In: Hsu, K. J., ed., Mountain Building Processes. Academic Press, Amsterdam, 19-40. [32] Santosh, M., Teng, X.M., He, X.F., et al., 2016. Discovery of Neoarchean Suprasubduction Zone Ophiolite Suite from Yishui Complex in the North China Craton. Gondwana Research, 38:1-27. https://doi.org/10.1016/j.gr.2015.10.017 [33] Song, Z, Y., Zhang, Z, Q., Zhao, G, L., 1994. Suggestions on the Stratigraphic Division and Correlation of the Precambrian Rocks in the Western Shandong Region. Shandong Geology, 10(Suppl.):2-13(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-SDDI4S1.002.htm [34] Stern, R.J., Tsujimori, T., Harlow, G.E., et al., 2013. Plate Tectonic Gemstones. Geology, 41:723-726. https://doi.org/10.1130/G34204.1 [35] Wan, Y.S., Dong, C.Y., Xie, H.Q., et al., 2015a. Composition and Evolution of the Ancient Basement of the North China Craton. Geological Survey of China, 2(3):1-4(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgdzdc201503001 [36] Wan, Y.S., Dong, C.Y., Xie, H.Q., et al., 2015b. Some Progress in the Study of Archean Basement of the North China Craton. Acta Geosientica Sinica, 36 (6):685-700 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqxb201506001 [37] Wan, Y.S., Liu, D.Y., Wang, S.J., et al., 2012. Redefinition of Early Precambrian Supracrustal Rocks and Formation Age of BIF in Western Shandong, North China Craton. Acta Petrologica Sinica, 28(11):3457-3475(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201211003 [38] Wang, W., Zhai, M.G., Wang, S.J., et al., 2016. Neoarchean Crustal Evolution in Western Shandong Province of the North China Craton: The Role of 2.7~2.6 Ga Magmatism. Precambrian Research, 285: 170-185. https://doi.org/10.1016/j.precamres.2016.09.010 [39] Wang, S.J., 1991. Stage and Phase Division and Basic Features of Precambrian Intrusive Rocks in the Western Shandong Area. Regional Geology of China, 4:59-81 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZQYD199104002.htm [40] Wang, S.J., Wan, Y.S., Song, Z.Y., et al., 2012. Stratigraphic Division and Formation Era of Taishan Group in Luxi Area:Evidence of Zircon SHRIMP U-Pb Dating. Shandong Land and Resources, 28(12):15-23(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SDDI201212005.htm [41] Wang, S.J., Wan, Y.S., Zhang, C.J., et al., 2008. Major Advanced Development Gained in Studying Early Cambrain Geology in Luxi Area. Shandong Land and Resources, 24(1):10-19(in Chinese with English abstract). [42] Wang, W., Liu, S.W., Bai, X., et al., 2015. Precambrian Geodynamics (Ⅷ):Late Archean Crustal Growth Models Recorded in the North China Craton. Earth Science Frontiers, 22(6):109-124(in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTOTAL-DXQY201506010.htm [43] Wang, W., Zhai, M.G., Santosh, M., 2016. The Genesis of Archean Supracrustal Rocks in the Western Shandong Province of North China Craton:Constraints on Regional Crustal Evolution. Science China Earth Sciences, 59(8):1583-1596(in Chinese). doi: 10.1007/s11430-016-5300-1 [44] Wang, Y.J., Zhang, Y.Z., Zhao, G.C., et al., 2009. Zircon U-Pb Geochronological and Geochemical Constraints on the Petrogenesis of the Taishan Sanukitoids (Shandong), Implications for Neoarchean Subduction in the Eastern Block, North China Craton.Precambrian Research, 174:273-286. https://doi.org/10.1016/j.precamres.2009.08.005 [45] Xiang, Z.Q., Li, H.K., Lu, S.N., et al., 2012. Emplacement Age of the Gabbro-Diabase Dike in the Hongmen Scenic Region of Mount Tai, Shandong Province, North China:Baddeleyite U-Pb Precise Dating. Acta Petrologica Sinica, 28(9):2831-2842(in Chinese with English abstract). [46] Zhang, Z.Q., Yang, E.X., Liu, P.R., 2012. Geological Characterisitcs of Longting Rubby Deposit in Xintai City of Shandong Province. Shandong Journal of Land and Resources, 28(1):1-4 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=sddz201201001 [47] Zhao, G.C., Cawood, P.A., 2013. Precambrian Geology of China. Precambrian Res., 222-223: 13-54. https://doi.org/10.1016/j.precamres.2012.09.017 [48] 曹国权, 王致, 董一杰, 等, 1987.鲁西山区与早、中前寒武系有关的几个地质问题的新认识.中国地质科学院院报, 16:189-200. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=HY000002696730 [49] 曹国权, 1995.鲁西山区早前寒武纪地壳演化再探讨.山东地质, 11(2):1-14. [50] 曹国权, 1996.鲁西早前寒武纪地质.北京:地质出版社. 1-210. [51] 程裕淇, 沈其韩, 王泽九, 1982.山东太古代雁翎关变质火山-沉积岩.北京:地质出版社, 1-72. [52] 程裕淇, 1994.中国区域地质概论.北京:地质出版社, 1-517. [53] 程裕琪, 徐惠芬, 1991.对山东新泰晚太古代雁翎关组中科马提岩类的一些新认识.中国地质, (4):31-32. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK000000212712 [54] 邓晋福, 肖庆辉, 苏尚国, 等, 2007.火成岩组合与构造环境:讨论.高校地质学报, 13(3):392-402. doi: 10.3969/j.issn.1006-7493.2007.03.009 [55] 邓晋福, 冯艳芳, 狄永军, 等, 2015.岩浆弧火成岩构造组合与洋陆转换.地质论评, 61(3):473-484. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzlp201503001 [56] 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 [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, 罗照华, 苏尚国, 等, 2004.岩石成因、构造环境与成矿作用.北京:地质出版社, 1-381. [59] 冯艳芳, 邓晋福, 王世进, 等, 2010.鲁西地区早前寒武纪花岗岩类中镁安山质岩石系列(MA)的识别及大陆地壳生长.中国地质, 37(4):1119-1129. doi: 10.3969/j.issn.1000-3657.2010.04.026 [60] 江博明, 沈其韩, 刘敦一, 等, 1988.中国太古代地壳演化-泰山杂岩及长期亏损地慢新地壳增生的证据.中国地质科学院地质研究所所刊, 18:3-57. http://www.cnki.com.cn/Article/CJFDTotal-DZYW198802003.htm [61] 李廷栋, 肖庆辉, 潘桂堂, 等, 2019.关于发展洋板块地质学的思考.地球科学, 44(5):1441-1451. doi: 10.3799/dqkx.2019.970 [62] 陆松年, 王惠初, 郝国杰, 等, 2016.关于板块运动启动时间的争论.中国地质, 43(3):709-720. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgdizhi201603002 [63] 陆松年, 陈志宏, 相振群, 2008.泰山世界地质公园古老侵入岩系年代格架.北京:地质出版社, 1-90. [64] 陆松年, 郝国杰, 王惠初, 等, 2017.中国变质岩大地构造.北京:地质出版社, 1-338. [65] 陆松年, 相振群, 王惠初, 等, 2019.泰山新太古代地质演化史(上).北京:人民出版社, 1-267. [66] 陆松年, 郝国杰, 王惠初, 等, 2015.中国变质岩大地构造图(1:2 500 000)说明书.北京:地质出版社, 1-92. [67] 潘桂棠, 肖庆辉, 张克信, 等, 2019.大陆中洋壳俯冲增生杂岩带特征与识别的重大科学意义.地球科学, 44(5):1544-1561. doi: 10.3799/dqkx.2019.063 [68] 宋志勇, 张增奇, 赵光鲁, 等, 1994.鲁西前寒武纪岩石地层清理意见.山东地质, 10(增刊):2-13. http://www.cnki.com.cn/Article/CJFDTotal-SDDI4S1.001.htm [69] 万渝生, 董春艳, 颉颃强, 等, 2015a.华北克拉通古老大陆地壳组成及演化.中国地质调查, 2(3):1-4. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgdzdc201503001 [70] 万渝生, 董春艳, 颉颃强, 等, 2015b.华北克拉通太古宙研究若干进展.地球学报, 36(6):685-700. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqxb201506001 [71] 万渝生, 刘敦一, 王世进, 等, 2012.华北克拉通鲁西地区早前寒武纪表壳岩系重新划分和BIF形成时代.岩石学报, 28(11):3457-3475. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201211003 [72] 王世进, 万渝生, 宋志勇, 等, 2012.鲁西泰山岩群地层划分及形成时代-锆石SHRIMP U-Pb测年的证据.山东国土资源, 28(12):15-23. doi: 10.3969/j.issn.1672-6979.2012.12.004 [73] 王世进, 万渝生, 张成基, 等, 2008.鲁西地区早前寒武纪地质研究新进展.山东国土资源, 24(1):10-19. doi: 10.3969/j.issn.1672-6979.2008.01.005 [74] 王世进, 1991.鲁西地区早前寒武纪侵入岩期次划分及基本特征.中国区域地质, (4):59-81. http://www.cnki.com.cn/Article/CJFDTotal-ZQYD199104002.htm [75] 王伟, 刘树文, 白翔, 等, 2015.前寒武纪地球动力学(Ⅷ):华北克拉通太古宙末期地壳生长方式.地学前缘, 22(6):109-124. http://www.cqvip.com/QK/98600X/201506/666722791.html [76] 王伟, 翟明国, Santosh, M., 2016.鲁西太古宙表壳岩的成因及其对地壳演化的制约.中国科学:地球科学, 46(7):949-962. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgkx-cd201607007 [77] 相振群, 李怀坤, 陆松年, 等, 2012.泰山地区古元古代末期基性岩墙形成时代厘定:斜锆石U-Pb精确定年.岩石学报, 28(9):2831-2842. http://d.wanfangdata.com.cn/periodical/ysxb98201209013 [78] 张增奇, 杨恩秀, 刘鹏瑞, 等, 2012.鲁西地区"泰山红宝石"的发现及其地质特征.山东国土资源, 28(1):1-4. doi: 10.3969/j.issn.1672-6979.2012.01.001 -
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