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兴蒙造山系新元古代-古生代沉积盆地演化
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  • 英文篇名:Neoproterozoic-Paleozoic Sedimentary Basins Evolution of Xing-Meng Orogenic Belt
  • 作者:杨文麟 ; 骆满生 ; 王成刚 ; 徐增连
  • 英文作者:Yang Wenlin;Luo Mansheng;Wang Chenggang;Xu Zenglian;Faculty of Earth Sciences,China University of Geosciences;State Key Laboratory of Biogeology and Environmental Geology,China University of Geosciences;Wuhan Institute of Geology and Mineral Resources;
  • 关键词:沉积 ; 构造 ; 盆地演化 ; 兴蒙造山系 ; 新元古代-古生代
  • 英文关键词:sedimentology;;tectonics;;basin evolution;;Xing-Meng orogenic belt;;Neoproterozoic-Paleozoic
  • 中文刊名:地球科学(中国地质大学学报)
  • 英文刊名:Earth Science(Journal of China University of Geosciences)
  • 机构:中国地质大学地球科学学院;中国地质大学生物地质与环境地质国家重点实验室;武汉地质矿产研究所;
  • 出版日期:2014-08-15
  • 出版单位:地球科学(中国地质大学学报)
  • 年:2014
  • 期:08
  • 基金:中国地质调查局项目(Nos.1212011121261,12120113012500)
  • 语种:中文;
  • 页:244-257
  • 页数:14
  • CN:42-1233/P
  • ISSN:1000-2383
  • 分类号:P534;P548
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.
        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 arcbasin 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.
引文
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