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大兴安岭南部二叠系—三叠系界线及沉积环境演化

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陈树旺, 郑月娟, 张健, 张海华, 张德军, 苏飞, 黄欣, 公繁浩, 甄甄. 2020. 大兴安岭南部二叠系—三叠系界线及沉积环境演化[J]. 中国地质, 47(3): 821-838. doi: 10.12029/gc20200319
引用本文: 陈树旺, 郑月娟, 张健, 张海华, 张德军, 苏飞, 黄欣, 公繁浩, 甄甄. 2020. 大兴安岭南部二叠系—三叠系界线及沉积环境演化[J]. 中国地质, 47(3): 821-838. doi: 10.12029/gc20200319
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CHEN Shuwang, ZHENG Yuejuan, ZHANG Jian, ZHANG Haihua, ZHANG Dejun, SU Fei, HUANG Xin, GONG Fanhao, ZHEN Zhen. 2020. The sedimentary environment and boundary of Permian-Triassic strata in the southern Da Hinggan Mountains, Inner Mongolia[J]. Geology in China, 47(3): 821-838. doi: 10.12029/gc20200319
Citation: CHEN Shuwang, ZHENG Yuejuan, ZHANG Jian, ZHANG Haihua, ZHANG Dejun, SU Fei, HUANG Xin, GONG Fanhao, ZHEN Zhen. 2020. The sedimentary environment and boundary of Permian-Triassic strata in the southern Da Hinggan Mountains, Inner Mongolia[J]. Geology in China, 47(3): 821-838. doi: 10.12029/gc20200319
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大兴安岭南部二叠系—三叠系界线及沉积环境演化

  • 中国地质调查局沈阳地质调查中心, 辽宁 沈阳 110034

  • 基金项目:
    中国地质调查局项目（DD20160163，DD20190097）和国家自然科学基金（31670215）联合资助
详细信息
    作者简介: 陈树旺, 男, 1964年生, 博士, 研究员, 从事油气基础地质调查研究; E-mail:sycswgeology@163.com
    通讯作者: 张健, 1980年生, 男, 硕士, 高级工程师, 从事沉积学和油气基础地质调查工作; E-mail:48487885@qq.com

  • 中图分类号: P534.46;P534.51

The sedimentary environment and boundary of Permian-Triassic strata in the southern Da Hinggan Mountains, Inner Mongolia

  • Shenyang Center of Geological Survey, China Geological Survey, Shenyang 110034, Liaoning, China

  • Fund Project: Supported by China Geological Survey Projects (No. DD20160163, DD20190097), National Natural Science Foundation of China (No. 31670215)
More Information
    Author Bio: CHEN Shuwang, male, born in 1964, professor, mainly engages in fundamental geological survey and research on oil and gas resources; E-mail:sycswgeology@163.com .
    Corresponding author: ZHANG Jian, 48487885@qq.com

    摘要

  • 北方陆相二叠系—三叠系界线研究是界线地层研究的重要问题之一，对采自内蒙古巴林右旗幸福之路组二段建组剖面的安山质岩屑晶屑凝灰岩开展锆石LA-ICP-MS U-Pb测年，结果为（255.5±1.1）Ma，火山岩上部多个层位粉砂质泥岩中发现孢粉化石，计17属20种，时代为晚二叠世—早三叠世，推断幸福之路组的时代为晚二叠世—早三叠世，大兴安岭地区二叠系—三叠系界线在幸福之路组内部，二者为整合接触。幸福之路组以红层做为划分标志，岩性为正常沉积碎屑岩夹火山岩，见大量泥灰岩夹层、钙质结核及干裂现象，反映了炎热、干燥及强氧化条件的气候环境，大兴安岭地区晚二叠世晚期（幸福之路组二段下部）就已出现反映干旱气候的红层沉积，与相邻的华北及新疆准噶尔盆地相似。

    The continental Permian-Triassic boundary is one of the most important problems in the study of the global PermianTriassic boundary. Based on collecting and analyzing tuff samples,the authors conducted LA-ICP-MS U-Pb dating of zircon and obtained an age of (255.5±1.1)Ma in the stratotype section of the middle part of Xingfuzhilu Formation. A total of 20 species of 17 genera sporopollen fossils were discovered on the top of the tuff in the stratotype section. The age of Xingfuzhilu Formation is late Late Permian-early Early Triassic according to the sporopollen fossils. It is considered that the middle part of Xingfuzhilu Formation should be late Late Permian whereas the upper part belongs to early Early Triassic. The boundary of Permian and Triassic strata in Da Hinggan Mountains is actually located inside Xingfuzhilu Formation. Moreover,the Late Permian-Early Triassic strata are of continuous deposition in Da Hinggan Mountains. With red-red features as a dividing point,Xingfuzhilu Formation totally reflects the thermal,arid and strong oxidation climate. It can be dated back to late Late Permian-early Early Triassic. The red beds came into existence from the late Late Permian in Da Hinggan Mountains. In addition,the climate changed from warm and rainless to arid and thermal,which is in accord with features of neighbouring North China and Junggar basin in Xinjiang. These data prove that the thermal,arid and strong oxidation climate did exert an profound influence on Da Hinggan Mountains.

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  • 图 1  内蒙古巴林右旗幸福之路地区地质简图

    Figure 1. 

    下载: 全尺寸图片 幻灯片

    图 2  内蒙古自治区巴林右旗幸福之路乡查干布拉格村西山上二叠统—下三叠统幸福之路组剖面

    Figure 2. 

    下载: 全尺寸图片 幻灯片

    图 3  内蒙古自治区巴林右旗幸福之路乡查干布拉格村西山上二叠统—下三叠统幸福之路组综合柱状图

    Figure 3. 

    下载: 全尺寸图片 幻灯片

    图 4  幸福之路组中段凝灰岩镜下特征

    Figure 4. 

    下载: 全尺寸图片 幻灯片

    图 5  幸福之路组中段凝灰岩的锆石阴极发光图像和206Pb/238U年龄

    Figure 5. 

    下载: 全尺寸图片 幻灯片

    图 6  幸福之路组中段岩屑晶屑凝灰岩样品（13BC01TWS）的锆石U-Pb谐和图

    Figure 6. 

    下载: 全尺寸图片 幻灯片

    图 7  幸福之路组野外照片

    Figure 7. 

    下载: 全尺寸图片 幻灯片
    晚二叠世—早三叠世幸福之路组 总厚度1389.02 mm
    61.灰紫色泥质粉砂岩 26.83 m
    60.紫灰色粉砂岩 1.38 m
    59.灰紫色泥质粉砂岩 6.23 m
    58.灰紫色粗粉砂岩 2.08 m
    57.灰紫色泥质粉砂岩 4.79 m
    56.紫灰色细砂岩 6.39 m
    55.灰紫色泥质粉砂岩、粉砂岩，含裸子植物花粉：Klausipollenites sp., Psophosphaera sp. 12.54 m
    54.灰绿色粉砂岩夹紫灰色泥质粉砂岩 21.65 m
    53.灰绿色粉砂岩 38.84 m
    52.黄绿色粉砂质泥岩 21.85 m
    51.黄绿色粉砂岩 27.53 m
    50.灰绿色粉砂质泥岩，含裸子植物花粉：Piceaepollenites sp., Quadraeculina sp. 65.88 m
    49.黄绿色细砂岩 23.00 m
    48.灰绿色粉砂岩 18.47 m
    47.灰绿色泥质粉砂岩 58.77 m
    46.黄绿色细砂岩 24.12 m
    45.灰绿色粗粉砂岩 4.51 m
    44.灰绿色粉砂岩夹粉砂质泥岩 49.66 m
    43.灰绿色粉细砂岩 57.81 m
    42.灰绿色粉砂岩 11.09 m
    41.深灰色细砂岩夹灰岩透镜体 13.31 m
    40.灰绿色粉砂质泥岩、灰绿色粉砂岩、粉砂质泥岩，含裸子植物花粉：Alisporites sp.，Alisporites indarraensis Segroves Pristinuspollenites sp., Piceites sp., Piceaepollenites sp., Protopinus sp., Lueckisporites virkkiae R. Potonie et Klaus, Pseudopicea sp., Pinuspollenites sp. 107.61 m
    39.灰紫色粉砂岩夹灰绿色细砂岩及灰岩透镜体，Piceaepollenites sp., Pristinuspollenites sp., Piceites sp., Paleoconiferae sp., Protoconiferus sp., Lueckisporites virkkiae 56.20 m
    38.灰绿色泥质粉砂岩，含孢粉：Cyclogranisporites sp., Protopinus sp., Quadraeculina sp., Alisporites parvus，Sulcatisporites rhombicus, Pristinuspollenites sp., Platysaccus sp. 16.14 m
    37.紫红色、灰绿色粉细砂岩，含裸子植物花粉：Piceaepollenites sp., Alisporites indarraensis Segroves, Pristinuspollenites sp., Quadraeculina sp., Piceites sp. 62.59 m
    36.紫红色泥质粉砂岩夹灰绿色粉砂岩，含裸子植物花粉：Pristinuspollenites sp., Piceites sp. 10.28 m
    35.紫红色、灰绿色粉细砂岩 37.25 m
    34.灰紫色中层中细砂岩，夹紫色粉砂质泥砾 34.73 m
    33.紫色粉砂质泥岩，局部夹灰绿色粉砂岩, 含孢粉：Cyclogranisporites sp., Klausipollenites sp. Protoconiferus sp.，Pristinuspollenites sp., Quadraeculina sp. 28.32 m
    32.紫灰色中薄层细砂岩 1.03 m
    31.紫红色粉砂岩，含孢粉：Baculatisporites sp., Cyclogranisporites sp., Piceaepollenites sp., Alisporites sp., Alisporites cacheutensis (Join) Song, Pristinuspollenites sp., Piceites sp., Protopinus sp., Protoconiferus sp., Quadraeculina sp. 7.68 m
    30.灰绿色粉砂岩, 含孢粉：Cyclogranisporites sp., Alisporites sp., Lueckisporites virkkiae R. Potonie et Klaus, Pristinuspollenites sp., Protoconiferus sp., Quadraeculina sp., Psophosphaera sp., Protopinus sp. 56.63 m
    29.紫红色粉砂岩 19.31 m
    28.紫红色粉砂岩与灰色中粗砂岩互层，含裸子植物花粉：Alisporites parvus De Jersey, Pristinuspollenites sp., Protopinus sp., Piceites sp., Quadraeculina sp. 5.65 m
    27.紫红色中层粉细砂岩夹灰色细砂岩，含孢粉：Baculatisporites sp., Cicatricosisporites sp.，Alisporites sp., Pristinuspollenites sp., Piceites sp., Protopinus sp., Pseudopicea sp., Platysaccus sp. 11.02 m
    26.紫红色中层粉细砂岩与深灰色中层中砂岩互层 2.66 m
    25.紫红色中薄层粉细砂岩夹灰色中层中砂岩 4.98 m
    24.紫灰色中薄层细砂岩夹中层灰色粗砂岩 2.99 m
    23.紫灰色中厚层粗砂岩夹紫红色粉砂岩 2.75 m
    22.紫灰色厚层中砂岩夹紫红色粉砂岩 10.16 m
    21.灰色厚层粗砂岩夹紫红色粉砂岩 3.53 m
    20.紫红色粉砂岩夹灰色粗砂岩 4.07 m
    19.灰色粗砂岩与紫红色粉砂岩互层 12.96 m
    18.灰色灰色安山质岩屑晶屑凝灰岩 7.40 m
    17.灰色含砾粗砂岩与紫红色粉砂岩、泥质粉砂岩互层 9.23 m
    16.灰色粗砂岩 7.18 m
    15.紫红色粉砂岩夹灰色粗砂岩 8.69 m
    14.灰色厚层粗砂岩夹紫红色粉砂岩 44.17 m
    13.紫红色粉砂岩夹灰色砂砾岩 21.56 m
    12.灰绿色粉砂岩 11.18 m
    11.灰色含砾粗砂岩 4.97 m
    10.紫红色粉砂岩夹灰色砂砾岩 40.12 m
    9.灰色砂砾岩夹紫红色粉砂岩 4.29 m
    8.紫灰色粉砂岩夹灰色砂砾岩 10.19 m
    7.深灰色砾岩 3.22 m
    6.紫灰色粉砂岩，夹灰色砂砾岩 14.69 m
    5.紫灰色角砾安山岩 8.73 m
    4.灰绿色细砂岩 27.84 m
    3.灰绿色粉砂岩 27.77 m
    2.灰绿色中薄层粉细砂岩，局部夹含砾粗砂岩，含裸子植物花粉：Piceaepollenites sp., Protoconiferus sp. 43.34 m
    1.紫灰色中薄层细砂岩，局部夹含砾粗砂岩 99.18 m
    ================断层================
    紫灰色复成分砾岩夹中薄层紫红色砂岩
    ....................
    下载: 导出CSV

    表 1  幸福之路组晶质凝灰岩LA-ICP-MS锆石U-Th-Pb分析结果

    Table 1.  The zircon LA-ICP-MS U-Pb data from crystal stuff in the middle part of Xingfuzhilu Formation

    下载: 导出CSV
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收稿日期:  2018-08-31
修回日期:  2019-05-24
刊出日期:  2020-06-25

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