石油学报 ›› 1992, Vol. 13 ›› Issue (2): 245-251.DOI: 10.7623/syxb199202040

• 论文 • 上一篇    下一篇

应用生态地层学观点改善地层对比——以辽河断陷东营组一、二段分界为例

李明阁1, 王铁玲1, 傅景华1, 孙镇城2   

  1. 1. 辽河石油勘探局勘探开发研究院;
    2. 石油大学 北京
  • 收稿日期:1991-02-07 出版日期:1992-04-25 发布日期:2013-07-08

IMPROVING STRATIGRAPHIC CORRELATION FROM AN ECOLOGY STRATIGRAPHIC VIEW——A STUDY OF THE BOUNDARY BETWEEN THE 1st AND 2nd MEMBER OF DONGYING FORMATION, LIAOHE FAULT DEPRESSION

Li Mingge1, Wang Tieling1, Fu Jinghua1, Sun Zhencheng2   

  1. 1. Institute of Exploration and Development, Liaohe Petroleum Exploration;
    2. Petroleum University, Beijing
  • Received:1991-02-07 Online:1992-04-25 Published:2013-07-08

摘要: 以辽河断陷东二段与东一段分界为例,阐明了处在湖水退缩的盆地中,湖盆边缘地区分布的化石组合特征,不一定与湖盆中心地区一致.适应性较强的广布种类比窄布种类有较长的延续时限.要正确对比地层必须把化石组合分解成标志化石带,结合古生态、沉积环境,尤其要把标志化石带与电测、岩性标准层、地震界面的追索,综合起来进行研究.

关键词: 辽河断陷, 第三纪, 东营组, 介形虫纲, 化石, 古生态学, 生物地层学, 地层对比

Abstract: Taking the boundary between the First and the Second Member of the Dongying For-mation of Liaohe Fault-depression as an example,the authors clarify that the characteristics of fossil assemblages below or above the boundary in the marginal areas of a regression lake basin are different from that of the centre part,and that widely spreaded species with stronger adaptation lasted for a longer geologic time than the narrowly spreaded ones.The fossil zones separated out from the fossil assemblage,paleoecology and sedimentary environment should be synthetically studied,and the seismic reflection boundary should be followed,so that a stratigraphic correlation may be improved.