| 内蒙古阿拉善左旗乌兰尚德地区志留系圆包山组笔石化石的发现及其地质意义 |
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| 引用本文： | 王挨顺,马云飞,张宝艳,武力军,张云学,邢志强,刘明君,杨富广,梁志宝,贾永琦,赵佳佳,张强,孙泽晨.内蒙古阿拉善左旗乌兰尚德地区志留系圆包山组笔石化石的发现及其地质意义[J].地质通报,2019,38(6):950-958. |
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| 作者姓名： | 王挨顺 马云飞 张宝艳 武力军 张云学 邢志强 刘明君 杨富广 梁志宝 贾永琦 赵佳佳 张强 孙泽晨 |
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| 作者单位： | 内蒙古自治区地质调查院, 内蒙古 呼和浩特 010010,中国建筑材料工业地质勘查中心内蒙古总队, 内蒙古 呼和浩特 010010,中国建筑材料工业地质勘查中心内蒙古总队, 内蒙古 呼和浩特 010010,中国建筑材料工业地质勘查中心内蒙古总队, 内蒙古 呼和浩特 010010,中国建筑材料工业地质勘查中心内蒙古总队, 内蒙古 呼和浩特 010010,中国建筑材料工业地质勘查中心内蒙古总队, 内蒙古 呼和浩特 010010,中国建筑材料工业地质勘查中心内蒙古总队, 内蒙古 呼和浩特 010010,中国建筑材料工业地质勘查中心内蒙古总队, 内蒙古 呼和浩特 010010,中国建筑材料工业地质勘查中心内蒙古总队, 内蒙古 呼和浩特 010010,中国建筑材料工业地质勘查中心内蒙古总队, 内蒙古 呼和浩特 010010,中国建筑材料工业地质勘查中心内蒙古总队, 内蒙古 呼和浩特 010010,中国建筑材料工业地质勘查中心内蒙古总队, 内蒙古 呼和浩特 010010,中国建筑材料工业地质勘查中心内蒙古总队, 内蒙古 呼和浩特 010010 |
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| 基金项目： | 内蒙古自治区地质勘查基金项目《内蒙古自治区阿拉善左旗乌兰尚德等五幅1∶5万区域矿产地质调查》（编号：NMKD2016-14） |
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| 摘 要： | 阿拉善盟阿拉善左旗杭乌拉山以北哈日奥布日格断凹陷盆地两侧,北东向出露770km2的哑地层,前人将其划为二叠系双堡塘组,但该套地层的岩性和岩石组合及层序特征,与内蒙古岩石地层所述的双堡塘组的现在定义和地质特征及区域变化完全相悖。采用现代沉积学理论和层序地层学方法,开展岩石组合、基本层序、沉积构造与沉积环境研究,划分出3个段级填图单元。根据发现的笔石化石和被晚泥盆世中粗粒黑云母花岗闪长岩侵入的关系,将地层时代确定为早志留世,改划为志留系圆包山组。泥盆纪区域变质变形作用使其发生浅变质和片理化变形,并形成轴向北东的复式向斜构造。后期叠加构造变形,形成紧闭倒转褶皱。志留系圆包山组的确定对本区地层划分和区域构造演化研究有重要意义。
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| 关 键 词： | 地层划分 岩石组合 笔石化石 圆包山组 阿拉善盟 |
| 收稿时间： | 2019/1/17 0:00:00 |
| 修稿时间： | 2019/3/12 0:00:00 |
The discovery of Silurian Yuanbaoshan Formation graptolite in Wulanshangde area of Alxa Left Banner, Inner Mongolia, and its geological significance |
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| WANG Aishun,MA Yunfei,ZHANG Baoyan,WU Lijun,ZHANG Yunxue,XING Zhiqiang,LIU Mingjun,YANG Fuguang,LIANG Zhibao,JIA Yongqi,ZHAO Jiaji,ZHANG Qiang and SUN Zechen.The discovery of Silurian Yuanbaoshan Formation graptolite in Wulanshangde area of Alxa Left Banner, Inner Mongolia, and its geological significance[J].Geologcal Bulletin OF China,2019,38(6):950-958. |
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| Authors: | WANG Aishun MA Yunfei ZHANG Baoyan WU Lijun ZHANG Yunxue XING Zhiqiang LIU Mingjun YANG Fuguang LIANG Zhibao JIA Yongqi ZHAO Jiaji ZHANG Qiang and SUN Zechen |
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| Institution: | Geological Survey Institute of Inner Mongolia, Hohhot 010010, Inner Mongolia, China,Inner Mongolia Branch of China National Geological Exploration Center of Building Materials Industry, Hohhot 010010, Inner Mongolia, China,Inner Mongolia Branch of China National Geological Exploration Center of Building Materials Industry, Hohhot 010010, Inner Mongolia, China,Inner Mongolia Branch of China National Geological Exploration Center of Building Materials Industry, Hohhot 010010, Inner Mongolia, China,Inner Mongolia Branch of China National Geological Exploration Center of Building Materials Industry, Hohhot 010010, Inner Mongolia, China,Inner Mongolia Branch of China National Geological Exploration Center of Building Materials Industry, Hohhot 010010, Inner Mongolia, China,Inner Mongolia Branch of China National Geological Exploration Center of Building Materials Industry, Hohhot 010010, Inner Mongolia, China,Inner Mongolia Branch of China National Geological Exploration Center of Building Materials Industry, Hohhot 010010, Inner Mongolia, China,Inner Mongolia Branch of China National Geological Exploration Center of Building Materials Industry, Hohhot 010010, Inner Mongolia, China,Inner Mongolia Branch of China National Geological Exploration Center of Building Materials Industry, Hohhot 010010, Inner Mongolia, China,Inner Mongolia Branch of China National Geological Exploration Center of Building Materials Industry, Hohhot 010010, Inner Mongolia, China,Inner Mongolia Branch of China National Geological Exploration Center of Building Materials Industry, Hohhot 010010, Inner Mongolia, China and Inner Mongolia Branch of China National Geological Exploration Center of Building Materials Industry, Hohhot 010010, Inner Mongolia, China |
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| Abstract: | A puzzling stratum is identified as Permian Shuangbaotang Formation,which is outcropped in NE direction for 770km2 on both sides of Hariaoribuge sag in northern Hangwula Mountain of Alxa Left Banner. However, the summarized lithology, rock association and sequence characteristics of strata is in contradiction with the definition, geological characteristics and regional change of Shuangbaotang Formation named by Inner Mongolian lithostratigraphic researchers. In this study, 1:50,000 regional mineral geological survey adopted modern sedimentology theory and sequence stratigraphy working method to study rock association,basic sequence, sedimentary structure and sedimentary environment. The authors divided the strata into three lithologic section-level geological units. According to the first discovery of graptolite and the invading contact of biotite granodiorites in the Late Devonian (U-Pb/379±2.9Ma), the strata age should be Early Silurian and it was changed into Silurian Yuanbaoshan Formation.The Devonian regional deformation and metamorphic process produced low-grade metamorphism and schistositilization deformation and formed NE-trending compound syncline structure. Then it experienced superimposition ofstructural deformation and formed closed-reverse fold. The establishment of Silurian Yuanbaoshan Formation plays an important role in stratigraphic subdivision and regional tectonic evolution study. |
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| Keywords: | stratigraphic subdivision rock association graptolite Yuanbaoshan Formation Alxa League |
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