额尔齐斯-西拉木伦对接带古生代沉积盆地演化

徐增连; 骆满生; 杨文麟; 王成刚; 吴年文

doi:10.3799/dqkx.2014.097

额尔齐斯-西拉木伦对接带古生代沉积盆地演化

doi: 10.3799/dqkx.2014.097

徐增连^{1, 2,},
骆满生²,
杨文麟^{1, 2},
王成刚³,
吴年文³

1.
中国地质大学地球科学学院, 湖北武汉 430074
2.
中国地质大学生物与环境地质国家重点实验室, 湖北武汉 430074
3.
武汉地质矿产研究所, 湖北武汉 430205

基金项目:

中国地质调查局项目 1212010733802

中国地质调查局项目 12120113012500

详细信息

作者简介:
徐增连(1985-), 男, 在读博士研究生, 主要从事地层古生物与沉积学研究.E-mail: lz_xu870601@126.com

中图分类号: P534
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出版历程
- 收稿日期: 2014-04-03
- 刊出日期: 2014-08-01

Paleozoic Sedimentary Basins Evolution of Ertix-Xar Moron Suture

1.
Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China
2.
State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, China
3.
Wuhan Institute of Geology and Mineral Resources, Wuhan 430205, China

摘要

摘要: 额尔齐斯-西拉木伦对接带位于西伯利亚板块、华北陆块和准噶尔地块之间, 其构造演化和古亚洲洋洋盆的打开与关闭有密切的关系.笔者在系统分析研究区3个二级和19个三级构造单元古生代岩石地层、生物地层及年代地层的基础上, 对沉积盆地进行原型恢复, 共划分出10个盆地类型.同时, 根据沉积盆地充填序列对研究区的构造-沉积演化做出了初步的论述.(1)早古生代-早石炭世古亚洲洋俯冲阶段; (2)早、晚石炭世之交的碰撞演化阶段; (3)晚石炭世-早二叠世碰撞及碰撞后演化阶段.研究认为古亚洲洋的闭合由西向东呈"剪刀式", 时间分别为早石炭世末(318 Ma)和中二叠世-早三叠世(260~245 Ma).三叠纪古亚洲洋消亡总体转为陆相环境.
- 沉积 /
- 构造 /
- 盆地演化 /
- 古生代 /
- 额尔齐斯-西拉木伦
Abstract: The Ertix-Xar Moron suture is located at the joint part of Siberia, North China and Junggar, and its tectonic evolution has a close relationship with the opening and closing of Paleo-Asian Ocean basin.In this paper, plates the sedimentary basin types are reconstruted and define 10 basin types by an integrated research on the Paleozoic lithostratigraphy, biostratigraphy and chronostratigraphy are defined. The structure-sedimentary evolution of the study area is discussed based on the sedimentary basin-fill sequence and concluded as the following stages: (1) Early Paleozoic-Early Carboniferous subduction stage of the Paleo-Asian Ocean; (2) Early, Late Carboniferous collisional stage; (3) Late Carboniferous-Early Permian collision and post-collisional evolution stage. It is suggested that the Paleo-Asian Ocean closed from west to east like "scissors", and the closing began from the end of the Early Carboniferous (318 Ma) to the Middle Permian-Early Triassic (260-245 Ma).During Triassic, the Paleo-Asian Ocean disappeared and converted to total terrestrial environment.
- sedimentology /
- tectonics /
- basin evolution /
- Paleozoic /
- Ertix-Xar Moron

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1a 额尔齐斯地区古生代生物地层划分对比

1a. Fossil zones and assemblages of Paleozoic strata in Ertix area

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1b 西拉木伦地区古生代生物地层划分对比

1b. Fossil zones and assemblages of Paleozoic strata in Xar Moron area

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图 2 额尔齐斯-西拉木伦大地构造格局与构造单元划分

Ⅱ-1.额尔齐斯结合带：Ⅱ-1-1.额尔齐斯复合增生楔(D-C)，Ⅱ-1-2.陆内断陷盆地(N-Q)，Ⅱ-1-3.乔夏哈拉-布尔根蛇绿混杂岩(D₁-C₁)，Ⅱ-1-4.北准噶尔-萨吾尔洋内弧(D₁-C₁)，Ⅱ-1-5.塔尔巴哈台-洪古勒楞蛇绿混杂岩(D₁-C₁)，Ⅱ-1-6.阿尔曼太-扎河偃蛇绿混杂岩(D₁-C₁)；Ⅱ-2.索伦山-西拉木伦结合带：Ⅱ-2-1.白音宝力道(查干乌拉)俯冲增生杂岩(O-D)，高压蓝片岩变质杂岩，Ⅱ-2-2.索伦山蛇绿混杂带(D-P₁)，Ⅱ-2-3.林西残余盆地(P₂-T₁)，Ⅱ-2-4.温都尔庙俯冲增生杂岩(O)，高压蓝片岩带，Ⅱ-2-5.柯单山-小苇塘蛇绿混杂岩带(C-P)，Ⅱ-2-6.机房沟-汪青-珲春蛇绿混杂岩带(C-P)；Ⅱ-3.包尔汗图-白乃庙弧盆系：Ⅱ-3-1.宝音图基底残块(Pt₁)，岩浆弧(Pz₂)，Ⅱ-3-2.镶黄旗-多伦陆缘岩浆弧(Pz₂)，断陷-火山沉积盆地(K₁)，Ⅱ-3-3.包尔汗图岛弧(Pz₁)，Ⅱ-3-4.白乃庙岛弧(Pz₁)，Ⅱ-3-5.通辽岩浆弧(SD₁，Pz)，Ⅱ-3-6.盘石-百里坪岩浆弧(Pz)，Ⅱ-3-7.下二台-呼兰岩浆弧(Pz)；a.吴波等(2006)；b.张越等(2012)；c.王玉往等(2011)；d.朱永峰和徐新(2006)；e.张元元等(2010)；f.金成伟等(2001)；g.何国琦等(2001)；h.简平等(2003)；i.黄萱等(1997)；j.刘伟和张湘炳(1993)；k.肖文交等(2006)；据潘桂棠等，中国大地构造图说明书(1∶250万)，2013修改

Fig. 2. Sketch map of Ertix-Xar Moron tectonic framework and tectonic units

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图 3 研究区古生代岩石地层单位序列

Fig. 3. Lithostragraphic sequence of Paleozoic strata in study area

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图 4 研究区古生代沉积盆地划分

Fig. 4. Paleozoic sedimentary basin classification of study area

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图 5 额尔齐斯-西拉木伦古生代构造-沉积演化示意

Fig. 5. Sketch map of the Paleozoic tectonic-sedimentary evolution of Ertix-Xar Moron area

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