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新疆卡克地区上石炭统别根他乌组碳酸盐岩微相及古环境分析

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姜文钦, 赵志刚, 王庆同, 代有旭. 2020. 新疆卡克地区上石炭统别根他乌组碳酸盐岩微相及古环境分析. 西北地质, 53(3): 66-75. doi: 10.19751/j.cnki.61-1149/p.2020.03.005
引用本文: 姜文钦, 赵志刚, 王庆同, 代有旭. 2020. 新疆卡克地区上石炭统别根他乌组碳酸盐岩微相及古环境分析. 西北地质, 53(3): 66-75. doi: 10.19751/j.cnki.61-1149/p.2020.03.005
shu
JIANG Wenqin, ZHAO Zhigang, WANG Qingtong, DAI Youxu. 2020. The Carbonate Microfacies and Paleoenvironment of the Upper Carboniferous Biegentawu Formation in Kake Area, Xinjiang. Northwestern Geology, 53(3): 66-75. doi: 10.19751/j.cnki.61-1149/p.2020.03.005
Citation: JIANG Wenqin, ZHAO Zhigang, WANG Qingtong, DAI Youxu. 2020. The Carbonate Microfacies and Paleoenvironment of the Upper Carboniferous Biegentawu Formation in Kake Area, Xinjiang. Northwestern Geology, 53(3): 66-75. doi: 10.19751/j.cnki.61-1149/p.2020.03.005
shu

新疆卡克地区上石炭统别根他乌组碳酸盐岩微相及古环境分析

  • 1. 中国地质大学(北京), 北京 100083;

  • 2. 中国人民武装警察部队黄金第七支队, 山东 烟台 264004;

  • 3. 中国地质大学(武汉), 湖北 武汉 430074

  • 基金项目:

    中国地质调查局项目“西北沿边及特殊地区地质矿产调查”（DD20160079）和“雷州半岛海岸带综合地质调查”（DD20208011）资助

详细信息
    作者简介: 姜文钦(1990-),男,助理工程师,古生物学与地层学硕士研究生。E-mail:453050894@qq.com
    通讯作者: 赵志刚(1985-),男,工程师,从事区域地质调查工作。E-mail:156513449@qq.com

  • 中图分类号: P588.245

The Carbonate Microfacies and Paleoenvironment of the Upper Carboniferous Biegentawu Formation in Kake Area, Xinjiang

  • 1. China University of Geosciences(Beijing);Beijing 100083, China;

  • 2. No.7 Gold Geological Party of CAPF, Yantai 264004, Shandong, China;

  • 3. China University of Geosciences(Wuhan), Wuhan 430074, Hubei, China

More Information

    摘要
  • 通过对新疆卡克地区上石炭统别根他乌组105个岩石薄片进行显微镜下观察，识别出6种微相：MF1灰泥灰岩微相、MF2含生物碎屑灰泥灰岩、MF3生物碎屑粒泥灰岩、MF4含生物碎屑亮晶似球粒灰岩、MF5生物碎屑亮晶灰岩和MF6生物碎屑砾屑灰岩。根据微相组合类型，推断该地区在罗苏期至达拉期经历了台地-台地边缘浅滩及礁-台地边缘斜坡3种环境，整体为一个完整海侵-海退的过程。
    The observation under microscope of 105 petrographic thin sections from the Upper Carboniferous Biegentawu Formation in Kake area, Xinjiang identified 6 microfacies: MF1 lime marl, MF2 bioclastic lime marl, MF3 bioclastic wackstone, MF4 bioclastic pelletoid limestone, MF5 sparry bioclastic limestone and MF6 bioclastic rudstone. According to the types of microfacies assemblage, we deduce that this area experienced three sedimentary environments of open platform-platform margin-platform margin slope which is a complete transgression-regression progress.
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收稿日期:  2020-01-20
修回日期:  2020-04-17

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