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西准噶尔克拉赛勒克山和布克河组晚泥盆世化石的发现及其地层归属

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纵瑞文, 龚一鸣. 2019. 西准噶尔克拉赛勒克山和布克河组晚泥盆世化石的发现及其地层归属[J]. 中国地质, 46(6): 1259-1269. doi: 10.12029/gc20190602
引用本文: 纵瑞文, 龚一鸣. 2019. 西准噶尔克拉赛勒克山和布克河组晚泥盆世化石的发现及其地层归属[J]. 中国地质, 46(6): 1259-1269. doi: 10.12029/gc20190602
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ZONG Ruiwen, GONG Yiming. 2019. The discovery of the Late Devonian fossils from the Hebukehe Formation and its stratal position in Kelasaileke Mountain, western Junggar, Xinjiang[J]. Geology in China, 46(6): 1259-1269. doi: 10.12029/gc20190602
Citation: ZONG Ruiwen, GONG Yiming. 2019. The discovery of the Late Devonian fossils from the Hebukehe Formation and its stratal position in Kelasaileke Mountain, western Junggar, Xinjiang[J]. Geology in China, 46(6): 1259-1269. doi: 10.12029/gc20190602
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西准噶尔克拉赛勒克山和布克河组晚泥盆世化石的发现及其地层归属

  • 1.

    中国地质大学 (武汉) 生物地质与环境地质国家重点实验室, 湖北 武汉 430074

  • 2.

    中国科学院资源地层学与古地理学重点实验室, 中国科学院南京地质古生物研究所, 江苏 南京 210008

  • 基金项目:
    国家自然科学基金（41702006，41290260，41872034）、中国科学院资源地层学与古地理学重点实验室（中国科学院南京地质古生物研究所）开放课题（2017KF05）和中国地质调查局项目（1212011120502，1212011220245）联合资助
详细信息
    作者简介: 纵瑞文, 男, 1988年生, 博士, 副研究员, 从事造山带地层学与古生物学研究; E-mail:zong_1658@126.com
    通讯作者: 龚一鸣, 男, 1958年生, 教授, 博士生导师, 长期从事地层学、古生物学和沉积地质学的科学研究与教学; E-mail:ymgong@cug.edu.cn

  • 中图分类号: P535

The discovery of the Late Devonian fossils from the Hebukehe Formation and its stratal position in Kelasaileke Mountain, western Junggar, Xinjiang

  • 1.

    State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, Hubei, China

  • 2.

    Key Laboratory of Economic Stratigraphy and Palaeogeography, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, Jiangsu, China

  • Fund Project: Supported by National Science Foundation of China (No. 41702006, 41290260, 41872034), Key Laboratory of Economic Stratigraphy and Palaeogeography, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences (No. 2017KF05) and China Geological Survey (No. 1212011120502, 1212011220245)
More Information
    Author Bio: ZONG Ruiwen, male, born in 1988, doctor, associate researcher, engages in the study of stratigraphy and paleontology of orogenic belt; E-mail: zong_1658@126.com .
    Corresponding author: GONG Yiming, male, born in 1958, professor, supervisor of doctor candidates, engages in the study and teaching of stratigraphy, paleontology and sedimentary geology; E-mail: ymgong@cug.edu.cn

    摘要

  • 西准噶尔地区广泛分布的和布克河组已被证明是洪古勒楞组的晚出异名，本文在西准噶尔克拉赛勒克山原划为下石炭统“和布克河组”的碎屑岩地层中发现了丰富的动、植物化石，包括：三叶虫Phacops sp.，菊石Manticoceras sp.，腕足类Tylothyris sp.，Aulacella sp.，“Mucrospirifer” sp.，Cyrtospirifer sp.，植物Leptophloeum rhombicum，Syringodendron sp.，Knorria sp.，其时代显示为晚泥盆世。根据岩性组合特征将其厘定为上泥盆统铁列克提组，而非“和布克河组”的替代名称洪古勒楞组。通过区域地质调查工作，证明了西准噶尔玛依力山地层小区内没有洪古勒楞组的分布，其晚泥盆世地层仅由铁列克提组组成，洪古勒楞组只分布在沙尔布尔提山地层小区，两个地层小区的界线为孟布拉克北侧至谢米斯台山南坡的深大断裂。晚泥盆世两个地层小区沉积分异明显，直到早石炭世早期才进入统一的盆地演化阶段，地层小区的分区性也随之消失。

    The Hebukehe Formation is widely distributed in western Junggar. It is the synonym of the Hongguleleng Formation. This paper presents abundant fossils from the clastic strata which were previously assigned to the Lower Carboniferous Hebukehe Formation in Kelasaileke Mountain, western Junggar. These fossils include trilobites Phacops sp., ammonoids Manticoceras sp., brachiopods Tylothyris sp., Aulacella sp., "Mucrospirifer" sp. and Cyrtospirifer sp., plants Leptophloeum rhombicum, Syringodendron sp. and Knorria sp.. The age of these fossils is attributed to the Late Devonian. According to the lithologic association, the fossiliferous strata are redefined as the Upper Devonian Tielieketi Formation, rather than the Hongguleleng Formation. Regional geological survey reveals that the Upper Devonian of Mayili Mountain stratomicroregion is only composed of the Tielieketi Formation, without the Hongguleleng Formation. The latter is only distributed in the Shaerbuerti Mountain stratomicroregion. The boundary of the two stratomicroregions is the deep fault located in northern Mengbulake to south slope of Xiemisitai Mountain. These two stratomicroregions experienced obvious sedimentary differentiation during the Late Devonian, and gradually evolved into the evolutional stage of uniform basin environment until the early Early Carboniferous, announcing a gradual disappearance of stratigraphic regionalization of the stratomicroregions.

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  • 图 1  西准噶尔克拉赛勒克山位置与地质简图（图a据龚一鸣等, 2015, 图b据1:20万《乌尔禾幅》❶和1:25万《铁厂沟镇幅》❷改编）

    Figure 1. 

    下载: 全尺寸图片 幻灯片

    图 2  西准噶尔克拉赛勒克山晚泥盆世动物和植物化石

    Figure 2. 

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    图 3  西准噶尔晚古生代地层区划与地层对比（据龚一鸣等，2015；纵瑞文等，2015改编）

    Figure 3. 

    下载: 全尺寸图片 幻灯片
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收稿日期:  2018-11-08
修回日期:  2019-05-23
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