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    新疆叶城南部“赛力亚克达坂群”及其时代的商榷

    王约 王训练 王野

    王约, 王训练, 王野, 2016. 新疆叶城南部“赛力亚克达坂群”及其时代的商榷. 地球科学, 41(7): 1099-1109. doi: 10.3799/dqkx.2016.091
    引用本文: 王约, 王训练, 王野, 2016. 新疆叶城南部“赛力亚克达坂群”及其时代的商榷. 地球科学, 41(7): 1099-1109. doi: 10.3799/dqkx.2016.091
    Wang Yue, Wang Xunlian, Wang Ye, 2016. Discussion on Age of 'Sailiyakedaban Group' in Southern Yecheng, South Xinjiang, NW China. Earth Science, 41(7): 1099-1109. doi: 10.3799/dqkx.2016.091
    Citation: Wang Yue, Wang Xunlian, Wang Ye, 2016. Discussion on Age of "Sailiyakedaban Group" in Southern Yecheng, South Xinjiang, NW China. Earth Science, 41(7): 1099-1109. doi: 10.3799/dqkx.2016.091

    新疆叶城南部“赛力亚克达坂群”及其时代的商榷

    doi: 10.3799/dqkx.2016.091
    基金项目: 

    中国地质调查局项目 1212011121258

    国家自然科学基金项目 41162003

    详细信息
      作者简介:

      王约(1964-),男,博士,教授,主要从事地层及古生物学的教学和研究.E-mail:gzyuewang@126.com

    • 中图分类号: P534.52

    Discussion on Age of "Sailiyakedaban Group" in Southern Yecheng, South Xinjiang, NW China

    • 摘要: 新疆叶城南部西昆仑山区的赛力亚克达坂一带,发育于麻扎-康西瓦构造带内的一套含煤碎屑岩系被命名为“赛力亚克达坂群”,并被认为是早-中三叠世沉积的地层.作为西昆仑和喀喇昆仑两板块分界,也是欧亚板块与“古特提斯域”分界的麻扎-康西瓦构造带,该陆相含煤碎屑岩系的时代对于西昆仑地区的大地构造和古地理演化的研究有着十分重要的意义.该套地层从岩性上大体可分为3个部分:下部以砾岩为主,中部以含煤及煤线为特征,上部以含砾砂岩为主.其中部产有以苏铁类(25%)、真蕨类(20%)、银杏类(20%)和松柏类(15%)占优势的植物群,共17属20种的植物化石.该植物群与西昆仑山及塔里木盆地边缘的叶尔羌群植物群相似,为兼有北方Coniopteris-Phoenicopsis和南方Ptilophyllum-Conioptersis植物群特征的早-中侏罗世植物群.另外,在岩性和地层序列上,麻扎-康西瓦构造带内的含煤碎屑岩系可与叶尔羌群进行对比,也适合叶尔羌群的定义.因而,建议废弃“赛力亚克达坂群”这一岩石地层单位,而沿用叶尔羌群,其时代为早-中侏罗世.

       

    • 图  1  新疆叶城南部赛力亚克达坂地区的地质简图

      Fig.  1.  Geological sketch of Sailiyakedaban area, southern Yechen, South Xinjiang, China

      图  2  新疆叶城南部麻扎-康西瓦构造带内的含煤碎屑岩系中的植物化石

      a.似木贼(未定种)Equisetites sp.;b.新芦木(未定种)Neocalamites sp.;c,d.亚洲枝脉蕨Cladophlebis asiatica Chow et Yeh;d.示叶脉;e, f.具齿枝脉蕨Cladophlebis denticulata (Brongniart) Fontaine;f.示叶脉;g.格子蕨(未定种)Clathropteris sp.;h.异脉蕨(未定种)Phlebopteris sp.;i.拟短形蕉羽叶(比较种)Nilssonia cf. parabrevis Huang;j.楔羽叶(未定种)Sphenozamites sp.;k, l.东方蕉羽叶Nilssonia orientalis Heer

      Fig.  2.  The plant fossils collected from the coal-bearing clastics in the Mazha-Kangxiwa tectonic belt in southern Yecheng, South Xinjiang

      图  3  新疆叶城南部麻扎-康西瓦构造带内叶尔羌群中的植物化石

      a.紧挤侧羽叶Pterophyllum contiguum Sze;b, c.梯兹侧羽叶Pterophyllum tietzei Schenk;d.拜拉(未定种)Baiera sp.;e.坚直茨康叶Czekanowskia rigida Heer;f.西伯利亚似银杏Ginkgoites cf. sibiricus (Heer) Seward;g.似银杏(未定种)Ginkgoites sp.;h.美丽苏铁杉(比较种)Podozamites cf. bullus Wu et Zhou;i.美丽苏铁杉(比较种)Podozamites cf. bullus Wu et Zhou和带状叶(未定种)Desmiophyllum sp.;j.带状叶(未定种)Desmiophyllum sp.;k.东北纵型枝Elatocladus manchuricus (Yokoyama) Yabe;l, m.椭圆似纵枝Elatides ovalis Heer;n.匙形鱼网叶Sagenopteris sp.

      Fig.  3.  The plant fossils collected from the Yarkant Group in the Mazha-Kangxiwa tectonic belt in southern Yecheng, South Xinjiang

      图  4  新疆昆仑山-塔里木盆地边缘下-中侏罗统叶尔羌群的地层对比及古地理示意

      a.叶尔羌群的地层对比;b.早-中侏罗世的古地理示意;c.剖面位置

      Fig.  4.  Stratigraphic correlation and paleogeographical sketch of the Yarkant Group of the Early-Middle Jurassic from the Kunlun Mountains to the margin of Tarim basin in South Xinjiang, NW China

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