Neoproterozoic-Paleozoic Sedimentary Basins Evolution of Xing-Meng Orogenic Belt
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摘要: 在系统分析兴蒙造山系新元古代-古生代24个沉积盆地类型、沉积建造、生物地层与年代地层等特征的基础上，划分了6个沉积大地构造演化阶段并对其进行讨论：(1)新元古代-寒武纪早期陆缘增生阶段：额尔古纳地块向南增生并与兴安地块拼贴，形成环宇-新林蛇绿岩拼合带；(2)寒武纪纽芬兰世-第二世陆缘稳定沉积阶段：各地块边缘发育相对稳定的碎屑岩-碳酸盐岩沉积，佳木斯地块受晚泛非造山作用影响；(3)早-中奥陶世多岛弧盆系形成阶段：多宝山地区弧盆系发育，其他地块边缘均有不同强度陆间洋壳俯冲作用；(4)晚奥陶世-志留纪普里道利世多岛弧盆系发展阶段：各地块隆升遭受剥蚀；(5)早泥盆世-早石炭世多岛弧盆系消减阶段：早石炭世晚期额尔古纳-兴安地块与松嫩地块拼贴，佳木斯西缘由被动陆缘转为活动陆缘；(6)晚石炭世-二叠纪乐平世拼合后洋-陆转化阶段：从早石炭世晚期开始至二叠纪末，佳木斯地块分别与松嫩地块、兴凯地块拼贴，至此东北各地块拼贴完成.Abstract: Based on comprehensive analysis of the type, sedimentary formation, biostratigraphy and chronostratigraphy for 24 main sedimentary basins, we study the evolution of sedimentary basins of Xing-Meng orogenic belt in the Neoproterozoic-Paleozoic, dividing it into six phases as follows. (1) The epicontinental accretion in the Neoproterozoic to Early Cambrian characterized by the assembly of Ergun and Xing'an blocks, as Huanyu-Xinlin ophiolite accreted to margin of southern Ergun blocks; (2) The stable epicontinental sediment in the Terreneuvian-Serises 2, with the feature of a relatively stable clastic-calciclastic sediment around the blocks while Jiamusi massif affected by Late Pan-African metamorphic event; (3) The formation of archipelagic arc-basin systems in the Early and Middle Ordovician, marked by the distribution of arc-basin in the margin of Duobaoshan and the different levels oceanic crust subduction effect among other land masses; (4) The development of archipelagic arc-basin systems in the Late Ordovician to Pridoli, as the erosion of the uplifted land masses; (5) The subduction of archipelagic arc-basin systems in the Early Devonian to Early Carboniferous, characterized by the collage of Ergun-Xing'an and Songnen blocks and the transformation of western margin of Jiamusi massif from passive to active in the late Early Carboniferous; (6) The oceanic-continental transition in the Late Carboniferous-Lopingian, characterized by the assembly of Jiamusi massif, Songnen massif, and Khanka massif. Massifs of Northeast China completely collaged to a whole.
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Key words:
- sedimentology /
- tectonics /
- basin evolution /
- Xing-Meng orogenic belt /
- Neoproterozoic-Paleozoic
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图 1 兴蒙造山系构造-地层区划分
①德布尔干断裂；②鄂伦春-头道桥断裂；③嫩江-开鲁走滑断裂；④伊通-依兰走滑断裂；⑤牡丹江断裂；⑥锡霍特-阿林构造带；⑦敦密走滑断裂；⑧西拉木伦-长春-延吉缝合线；据潘桂棠等(2009)、刘永江等(2010)、佘宏全等(2012)修改
Fig. 1. Tectonic-stratigraphic regionalization of Xing-Meng orogenic belt
图 2 兴蒙造山系新元古代-寒武纪早期沉积盆地分布
1.额尔古纳活动陆缘(NhZAM)；2.环宇-新林蛇绿混杂岩带(Pt3OM)；3.海拉尔-呼玛弧后盆地-岩浆弧()；4.伊春-张广才岭弧后-弧间盆地()；参考谢鸣谦(2000)、郑和荣和胡宗全(2010)
Fig. 2. Sedimentary basins distribution map of Xing-Meng orogenic belt in the Neoproterozoic-Early Cambrian
图 3 兴蒙造山系纽芬兰世-中奥陶世沉积盆地分布
1.额尔古纳活动陆缘(O1-2AM)；2.海拉尔-呼玛弧后盆地(O1-2BA)；3.扎兰屯-多宝山岩浆弧(弧背盆地)()；4.伊春-延寿弧间盆地-岩浆弧()；5.佳木斯被动陆缘()；6.兴凯湖边缘海混积浅海()；据李锦轶等(1999)、谢鸣谦(2000)、郑和荣和胡宗全(2010)
Fig. 3. Sedimentary basins distribution map of Xing-Meng orogenic belt in the Terreneuvian-Middle Ordovician
图 4 兴蒙造山系晚奥陶世-普里道利世沉积盆地分布
1.额尔古纳活动陆缘(S3-4AM)；2.扎兰屯-多宝山岩浆弧(O3S4MA)；参考李锦轶等(1999)、谢鸣谦(2000)、郑和荣和胡宗全(2010)
Fig. 4. Sedimentary basins distribution map of Xing-Meng orogenic belt in the Late Ordovician-Pridoli
图 5 兴蒙造山系早泥盆世-早石炭世沉积盆地分布
1.漠河弧后盆地(DBA)；2.莫尔道嘎弧后陆坡(C1bs)；3.海拉尔-呼玛弧后盆地(D1C1BA)；4.大兴安岭岩浆弧(D1C1MA)；5.贺根山蛇绿混杂岩带(DOM)；6.小兴安岭-张广才岭弧间盆地-岩浆弧(D1-2ib-MA)；7.佳木斯被动陆缘-活动陆缘(D1C1PM-AM)；参考谢鸣谦(2000)、余和中等(2001)、郑和荣和胡宗全(2010)
Fig. 5. Sedimentary basins distribution map of Xing-Meng orogenic belt in the Early Devonian-Early Carboniferous
图 6 兴蒙造山系晚石炭世-乐平世沉积盆地分布
1.海拉尔-呼玛弧后盆地(C2BA)；2.大兴安岭岩浆弧(C2P3MA)；3.小兴安岭岩浆弧(C2P3MA)；4.佳木斯弧后前陆盆地(C2P3BF)；5.兴凯弧后前陆盆地(P1-3BF)；参考李锦轶等(1999)、谢鸣谦(2000)、郑和荣和胡宗全(2010)
Fig. 6. Sedimentary basins distribution map of Xing-Meng orogenic belt in the Late Carboniferous-Lopingian
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