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新疆昌吉南部侏罗系头屯河组物源与沉积环境分析

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罗居德, 刘云华, 夏昭德, 汪帮耀, 范媛媛. 新疆昌吉南部侏罗系头屯河组物源与沉积环境分析[J]. 地质与资源, 2022, 31(4): 473-485. doi: 10.13686/j.cnki.dzyzy.2022.04.003
引用本文: 罗居德, 刘云华, 夏昭德, 汪帮耀, 范媛媛. 新疆昌吉南部侏罗系头屯河组物源与沉积环境分析[J]. 地质与资源, 2022, 31(4): 473-485. doi: 10.13686/j.cnki.dzyzy.2022.04.003
shu
LUO Ju-de, LIU Yun-hua, XIA Zhao-de, WANG Bang-yao, FAN Yuan-yuan. SOURCE AND SEDIMENTARY ENVIRONMENT OF JURASSIC TOUTUNHE FORMATION IN SOUTHERN CHANGJI, XINJIANG[J]. Geology and Resources, 2022, 31(4): 473-485. doi: 10.13686/j.cnki.dzyzy.2022.04.003
Citation: LUO Ju-de, LIU Yun-hua, XIA Zhao-de, WANG Bang-yao, FAN Yuan-yuan. SOURCE AND SEDIMENTARY ENVIRONMENT OF JURASSIC TOUTUNHE FORMATION IN SOUTHERN CHANGJI, XINJIANG[J]. Geology and Resources, 2022, 31(4): 473-485. doi: 10.13686/j.cnki.dzyzy.2022.04.003
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新疆昌吉南部侏罗系头屯河组物源与沉积环境分析

  • 长安大学 地球科学与资源学院，陕西 西安 710054

  • 基金项目:
    中国地质调查局地质调查项目“新疆昌吉地区K45E001012等六幅1 : 5万区域地质调查”（2019-002）
详细信息
    作者简介: 罗居德(1998-), 男, 硕士研究生, 从事构造地质学和沉积学研究, 通信地址陕西省西安市长安大学雁塔校区, E-mail//2915711423@qq.com
    通讯作者: 刘云华(1965-), 男, 博士, 研究员, 从事地质学教学与研究工作, 通信地址陕西省西安市长安大学雁塔校区, E-mail//zyyhliu@chd.edu.cn

  • 中图分类号: P618.13

SOURCE AND SEDIMENTARY ENVIRONMENT OF JURASSIC TOUTUNHE FORMATION IN SOUTHERN CHANGJI, XINJIANG

  • School of Earth Sciences and Resources, Chang'an University, Xi'an 710054, China

More Information

    摘要

  • 在野外勘察和实测剖面的基础上, 运用粒度分析、碳氧同位素分析及多碎屑三角端元分析等方法, 对新疆昌吉南部侏罗系头屯河组进行研究. 认为头屯河组主要发育辫状河三角洲前缘亚相以及滨浅湖亚相. 碳氧同位素样品结果显示13CV-PDB值均在-9‰~-17.3‰之间, 平均-13.275‰, 18OV-PDB值在-14.2‰~-16.2‰之间, 平均-15.425‰, 18OV-SMOW值在-14.2‰~-16.3‰之间, 平均-15.05‰, 表明头屯河组砂岩形成于大气淡水成岩环境. 成岩压实的温度范围为99.26~114.1℃, 埋深在4.34~5.23 km之间, 平均4.87 km. 物源分析反映其主要为隆升基底、岛弧造山带的构造背景, 并在沉积后期显示为混合物源区. 侏罗纪沉积环境由潮湿型气候逐渐向干旱型气候转变, 在头屯河组沉积时期, 沉积环境发生多次弱还原-弱氧化环境与较强氧化环境之间的交替转换.

    The methods of particle analysis, carbon-oxygen isotope and polyclastic triangular end member analysis are used to study the Jurassic Toutunhe Formation in southern Changji of Xinjiang based on field survey and section measuring. It is considered that the braided river delta front subfacies and shore shallow lake subfacies are mainly developed in Toutunhe Formation. The analysis results of carbon and oxygen isotope samples indicate that the sandstones of Toutunhe Formation were formed in meteoric freshwater diagenetic environment, with the compaction temperature of 99.26-114.1℃ and burial depth of 4.34-5.23 km (averagely 4.87 km). The provenance analysis reflects the tectonic setting of uplifted basement and island arc orogenic belt, showing mixed source in the late sedimentary stage. The Jurassic sedimentary environment changed from moist to arid climate, and alternated between weak reduction-weak oxidation and strong oxidation environment repeatedly during the sedimentary period of Toutunhe Formation.

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  • 图 1  研究区实测地质简图及大地构造位置

    Figure 1. 

    下载: 全尺寸图片 幻灯片

    图 2  中侏罗统头屯河组剖面图

    Figure 2. 

    下载: 全尺寸图片 幻灯片

    图 3  头屯河组砂岩样品岩性分类三角图(底图据文献[42])

    Figure 3. 

    下载: 全尺寸图片 幻灯片

    图 4  中侏罗统头屯河组砂岩显微特征(正交偏光)

    Figure 4. 

    下载: 全尺寸图片 幻灯片

    图 5  头屯河组典型沉积构造

    Figure 5. 

    下载: 全尺寸图片 幻灯片

    图 6  昌吉地区头屯河组砂岩粒度曲线图

    Figure 6. 

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    图 7  昌吉地区头屯河组柱状图

    Figure 7. 

    下载: 全尺寸图片 幻灯片

    图 8  13CV-PDB-Z值与成岩环境的关系(底图据文献[46])

    Figure 8. 

    下载: 全尺寸图片 幻灯片

    图 9  新疆昌吉南部头屯河组砂岩碎屑组分与物源类型三角图解(底图据文献[46-48])

    Figure 9. 

    下载: 全尺寸图片 幻灯片

    表 1  头屯河组砂岩粒度参数表

    Table 1.  Grain size parameters for sandstones of Toutunhe Formation

    样品编号 标准偏差（σ1） 分选性 偏度（SK1） 偏态 峰度（KG） 等级 C值 M值
    VI-113-1b 0.47 好 0.12 正 1.33 尖锐 0.1401 0.0745
    VI-109-1b 0.64 较好 0.1 正 1 中等 1.609 0.7415
    VI-96-1b 0.63 较好 0.18 正 1.26 尖锐 0.23 0.0991
    VI-90-1b 0.54 较好 0.2 正 1.1 中等 0.3995 0.177
    VI-78-1b 0.54 较好 -0.11 负 1.02 中等 1.3187 0.4545
    VI-67-1b 0.46 好 0.14 正 1 中等 0.5767 0.3354
    下载: 导出CSV

    表 2  头屯河组砂岩C、O同位素分析

    Table 2.  C and O isotope analysis of sandstones from Toutunhe Formation

    样品编号 岩性 13CV-PDB/‰ 18OV-PDB/‰ 18OV-SMOW/‰ 古盐度Z值 古温度/℃
    Ⅵ-68-1b 粗中粒长石砂岩 -17.3 -16.2 14.2 83.802 114.1
    Ⅵ-75-1b 中粗粒长石砂岩 -15.6 -15.6 14.9 87.582 109.564
    Ⅵ-78-1b 粗粒长石砂岩 -9 -14.2 16.3 101.796 99.26
    Ⅵ-98-1b 含海绿石细粒长石砂岩 / / / / /
    Ⅵ-109-1b 砂质砾岩 -11.2 -15.7 14.8 96.544 110.315
    平均 -13.275 -15.425 15.05 92.431 108.310
    下载: 导出CSV
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