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鄂尔多斯盆地南部奥陶系马六段白云岩特征及形成机制研究

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刘丽红, 王春连, 李丽霞, 杜治利, 唐跃, 韩淼. 2020. 鄂尔多斯盆地南部奥陶系马六段白云岩特征及形成机制研究[J]. 中国地质, 47(3): 810-820. doi: 10.12029/gc20200318
引用本文: 刘丽红, 王春连, 李丽霞, 杜治利, 唐跃, 韩淼. 2020. 鄂尔多斯盆地南部奥陶系马六段白云岩特征及形成机制研究[J]. 中国地质, 47(3): 810-820. doi: 10.12029/gc20200318
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LIU Lihong, WANG Chunlian, LI Lixia, DU Zhili, TANG Yue, HAN Miao. 2020. The characteristics and formation mechanism of Ordovician dolomite in Member 6 of Majiagou Formation in South Ordos Basin[J]. Geology in China, 47(3): 810-820. doi: 10.12029/gc20200318
Citation: LIU Lihong, WANG Chunlian, LI Lixia, DU Zhili, TANG Yue, HAN Miao. 2020. The characteristics and formation mechanism of Ordovician dolomite in Member 6 of Majiagou Formation in South Ordos Basin[J]. Geology in China, 47(3): 810-820. doi: 10.12029/gc20200318
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鄂尔多斯盆地南部奥陶系马六段白云岩特征及形成机制研究

  • 1.

    中国地质调查局油气资源调查中心, 北京 100083

  • 2.

    北京大学石油与天然气研究中心, 地球与空间科学学院, 北京 100871

  • 3.

    中国地质科学院矿产资源研究所, 国土资源部成矿作用与资源评价重点实验室, 北京 100037

  • 4.

    中海油研究总院, 北京 100028

  • 基金项目:
    国家自然科学基金项目（41802173）和中国地质调查局地质调查项目（DD20160175，DD20190106，DD20190708，DD20190090）联合资助
详细信息
    作者简介: 刘丽红, 女, 1982年生, 工程师, 博士生, 主要从事沉积学研究; E-mail:liulihong713@163.com
    通讯作者: 王春连, 男, 1983年生, 博士, 副研究员, 主要从事盆地沉积矿产研究; E-mail:wangchunlian312@163.com

  • 中图分类号: P588.24+5

The characteristics and formation mechanism of Ordovician dolomite in Member 6 of Majiagou Formation in South Ordos Basin

  • 1.

    Oil & Gas Survey, China Geological Survey, Beijing 100083, China

  • 2.

    Oil and Gas Research Center, School of Earth and Space Sciences, Peking University, Beijing 100871, China

  • 3.

    MNR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China

  • 4.

    CNOOC Research Institute, Beijing 100028, China

  • Fund Project: Supported by National Natural Science Foundation of China (No. 41802173) and China Geological Survey Program (No.DD20160175; No.DD20190106;No. DD20190708; No.DD20190090)
More Information
    Author Bio: LIU Lihong, female, born in 1982, doctor, engineer, engages in research on sedimentology; E-mail: liulihong713@163.com .
    Corresponding author: WANG Chunlian, male, born in 1983, doctor, associate researcher, engages in research on basin sedimentary mineral; E-mail: wangchunlian312@163.com

    摘要

  • 鄂尔多斯盆地马六段在盆地大部分地区被剥蚀，仅在盆地周缘地区分布，因此，有关该盆地马六段白云岩成因研究较少。本文通过对马六段白云岩岩石学特征、阴极发光特征、微量元素特征以及碳氧同位素地球化学特征进行分析，对鄂尔多斯盆地南部马六段白云岩特征及形成机制进行了研究。研究结果表明，盆地南部马六段白云岩主要由细—中晶白云岩组成，白云石具“雾心亮边”结构，阴极发光呈暗红色光。微量元素总体上具有较低的Fe、Mn值，平均值分别为447×10-6和62×10-6，较高的K、Na值，平均值分别为517×10-6和252×10-6，以及中等含量的Sr元素值，平均值为155×10-6。δ13C值平均为-0.617‰，δ18O值平均为-7.6‰，以上特征均反映出海源流体特征。白云石的“雾心”和“亮边”结构中微量元素含量相差不大，认为是在相同成岩环境的不同成岩阶段形成，其中“雾心”形成于浅埋藏环境的渗透回流白云石化作用，而“亮边”是在深埋藏环境下对早期白云石的调整和加强。

    Member 6 of Majiagou Formation in south Ordos basin has been eroded in most part of the south Ordos basin,and is hence only distributed in the periphery of the basin. Therefore,less studies have been done on the origin of dolomite in member 6 of Majiagou Formation of the basin. Based on petrologic analysis,cathodoluminescence images,trace elements and carbon and oxygen isotope characteristics,the authors studied the characteristics and formation mechanism of dolomite in member 6 of Majiagou Formation in south Ordos basin. The results reveal that the dolomite of member 6 in south Ordos basin is mainly composed of finemedium crystal dolomite with cloudy cores and clear rims as well as dark red luminescence. The dolomite has relatively low Fe and Mn content (average of 447×10-6 and 62×10-6),relatively high K and Na content (average of 517×10-6 and 252×10-6) and moderate content of Sr (average of 155×10-6). Average value of δ13C and δ18O is -0.617‰ and -7.6‰ respectively,moderate indicating its marine origin. The trace element content of cloudy cores is close to that of clear rims,which indicates that they were formed in similar diagenesis environments. The cloudy cores were formed in a shallow buried environment by seepage reflux dolomitization model,while the clear rims were recrystallized and adjusted in a deep buried environment.

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  • 图 1  鄂尔多斯盆地南部马六段沉积相分布图

    Figure 1. 

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    图 2  鄂尔多斯盆地南部马六段白云岩储层岩石学特征

    Figure 2. 

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    图 3  中—细晶白云岩电子探针分析点位，3301.62 m，马六段，旬探1（a—单偏光；b—局部放大）

    Figure 3. 

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    图 4  鄂尔多斯盆地南部马六段白云岩微量元素含量分布图(图中代号见表 2)

    Figure 4. 

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    图 5  鄂尔多斯盆地南部马六段白云岩Na-Sr含量图

    Figure 5. 

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    图 6  鄂尔多斯盆地南部马六段白云岩C-O同位素图

    Figure 6. 

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    图 7  鄂尔多斯盆地东南部奥陶系白云岩环边流体包裹体均一化温度和氧同位素组成投点图

    Figure 7. 

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    图 8  鄂尔多斯盆地南部马六段白云岩化模式图

    Figure 8. 

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    图 9  鄂尔多斯盆地南部马六段白云岩厚度等值线图

    Figure 9. 

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    表 1  鄂尔多斯盆地南部旬探1井白云石电子探针分析数据（%）

    Table 1.  Electron microprobe analyses (%) of dolomite in Xuntan1 well in the south Ordos basin

    下载: 导出CSV

    表 2  鄂尔多斯盆地南部白云石微量元素含量/10-6

    Table 2.  Trace element data (10-6) of dolomite in the south Ordos basin

    下载: 导出CSV

    表 3  鄂尔多斯盆地南部白云岩C、O同位素含量

    Table 3.  Carbon and oxygen isotope content of dolomite in the south Ordos basin

    下载: 导出CSV
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收稿日期:  2017-11-09
修回日期:  2018-05-18
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