地学前缘 ›› 2016, Vol. 23 ›› Issue (4): 22-28.DOI: 10.13745/j.esf.2016.04.002

• 大别造山带构造与成矿 • 上一篇    下一篇

华北地块南缘白大山群的层序、时代及地质意义

 张春雷, 查世新, 毕治国, 宫维莉, 夏琼, 马国明, 高雅   

  1. 1. 安徽省地质实验研究所, 安徽 合肥 230001
    2. 安徽省地质矿产勘查局 327地质队, 安徽 合肥 230011
    3. 安徽省地质博物馆, 安徽 合肥 230031
  • 收稿日期:2015-06-01 修回日期:2015-08-18 出版日期:2016-07-15 发布日期:2016-07-15
  • 通讯作者: 查世新(1956—)，男，教授级高级工程师。E-mail:1542677122@qq.com
  • 作者简介:张春雷(1983—)，男，工程师，从事区域地质、水工环地质研究。E-mail:chunleizhang1983@163.com
  • 基金资助:

    2012年度安徽省公益性地质工作项目(2012-g-36)

New progress and understanding of the Baidashan group, southern margin of the North China Block.

 ZHANG  Chun-Lei, CHA  Shi-Xin, BI  Chi-Guo, GONG  Wei-Chi, JIA  Qiong, MA  Guo-Meng, GAO  Ya   

  1. 1. Institute of Geoanalysis of Anhui Province, Hefei 230001, China
    2. No.327 Geological Party of Anhui Province, Hefei 230011, China
    3. Anhui Geological Museum, Hefei 230031, China
  • Received:2015-06-01 Revised:2015-08-18 Online:2016-07-15 Published:2016-07-15

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摘要：

笔者等近期对华北地块南缘豫皖交界处出露的一套层序连续完整的白大山群进行了剖面测制，在该套地层的碳酸盐岩中发现了中、晚奥陶世牙形刺分子Belodina compressa，Panderodus gracilis，Pseudobelodina dispansa(?)以及苔藓虫、海绵骨针、小壳类、古介形类等化石，填补了该地区一直无可靠化石记录的空白。同时依据地层层序特征、岩性组合、生物群面貌、古地理沉积环境，并结合大量灰岩薄片鉴定结果，将白大山群时代划归早古生代。同时，将华北地块南缘界限向北推移至蒋集—龙潭一线，并认为本区牙形刺生物群应属北方型牙形刺地理分区。

关键词: 华北地块, 早古生代, 白大山群, 牙形刺

Abstract:

Recently, the author has measured Baidashan group section which exposed a sequence of complete and continuous layer on the HenanAnhui border of southern margin on the north China Block. There are conodonts molecules of the MiddleLate Ordovician in carbonatite of Baidashan group: Belodina compressa,Panderodus gracilis,Pseudobelodina dispansa(?) and Bryozo, Calthrop, Small shells, Archaeostraca etc., which filled the blank of the region that has been no fossil record. According to the characteristics of stratigraphic sequence, lithologic combination, the biota appearance, the ancient sedimentary environment of geography, and combined with a large number of limestone thin section results, it is concluded that the Baidashan group belongs to the Early Paleozoic era. The southern margin of North China massif line was redrawn to JiangjiLongtan sets. We consider that the conodonts biota in this area should belong to the northern type conodonts geographical partition.

Key words: North China Block, Early Paleozoic, Baidashan group, conodont

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