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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