首页 | 本学科首页   官方微博 | 高级检索  
     检索      

辽河断陷古潜山古生界的厘定及其地质意义
引用本文:魏喜,邓晋福,王仁厚,王云喆,宋柏荣,崔向东,李学万,赵国春.辽河断陷古潜山古生界的厘定及其地质意义[J].地质通报,2005,24(3):264-271.
作者姓名:魏喜  邓晋福  王仁厚  王云喆  宋柏荣  崔向东  李学万  赵国春
作者单位:1. 中国地质大学地球科学与资源学院,北京,100083;中国石油辽河油田南海油气勘探分公司,辽宁,盘锦,124010
2. 中国地质大学地球科学与资源学院,北京,100083
3. 中国石油辽河油田分公司勘探开发研究院,辽宁,盘锦,124010
4. 吉林油田采油二厂,吉林,松原,131200
基金项目:国家自然科学基金重点项目(40234048)资助。
摘    要:辽河断陷以碳酸盐岩和砂页岩为主的古潜山地层一直全部划归中、新元古界。由于在该套地层的部分岩石薄片中发现交代残余的动物化石碎片,因此提出辽河断陷有古生界存在的新观点。通过牙形石、微古植物、动物化石和岩性组合的研究,对这套地层进行了重新厘定,建立了古生代寒武纪、奥陶纪、石炭纪和二叠纪地层层序。研究成果表明,辽河断陷存在古生界储层,古生代潜山并非单斜.而是由被断裂改造的褶皱组成的断块。这一成果为重新认识潜山的内幕构造特征和油气储层分布规律奠定了基础。

关 键 词:古生界的厘定  地质意义  古潜山  辽河断陷
文章编号:1671-2552(2005)03-0264-08
修稿时间:9/2/2004 12:00:00 AM

Determination of the Paleozoic in buried hills of the Liaohe fault depression and its geological significance
WEI Xi,DENG Jinfu,WANG Renhou,WANG YunzheSONG Bairong,CUI Xiangdong,LI Xuewan,ZHAO Guochun College of Earth Sciences and Resources,China University of Geosciences,Beijing,Chin,South China Sea Hydrocarbon Exploration Branch Company,Liaohe Oilfiel,PetroChin,Panjin,Liaoning,Chin,Institute of Research and Exploration,Liaohe Oilfield Branch Company,PetroChin,Panjin,Liaoning,Chin,Second Oil Extraction Plant,Jilin Oilfiel,Songyuan,Jilin,China.Determination of the Paleozoic in buried hills of the Liaohe fault depression and its geological significance[J].Geologcal Bulletin OF China,2005,24(3):264-271.
Authors:WEI Xi  DENG Jinfu  WANG Renhou  WANG YunzheSONG Bairong  CUI Xiangdong  LI Xuewan  ZHAO Guochun College of Earth Sciences and Resources  China University of Geosciences  Beijing  Chin  South China Sea Hydrocarbon Exploration Branch Company  Liaohe Oilfiel  PetroChin  Panjin  Liaoning  Chin  Institute of Research and Exploration  Liaohe Oilfield Branch Company  PetroChin  Panjin  Liaoning  Chin  Second Oil Extraction Plant  Jilin Oilfiel  Songyuan  Jilin  China
Institution:WEI Xi,DENG Jinfu,WANG Renhou,WANG YunzheSONG Bairong,CUI Xiangdong,LI Xuewan,ZHAO Guochun College of Earth Sciences and Resources,China University of Geosciences,Beijing,Chin,South China Sea Hydrocarbon Exploration Branch Company,Liaohe Oilfiel,PetroChin,Panjin,Liaoning,Chin,Institute of Research and Exploration,Liaohe Oilfield Branch Company,PetroChin,Panjin,Liaoning,Chin,Second Oil Extraction Plant,Jilin Oilfiel,Songyuan,Jilin,China
Abstract:The strata of buried hills in the Liaohe fault depression consist mainly of carbonate rocks and sandstone-shale, which were all assigned to the Meso- and Neoproterozoic. A new view of the existence of the Paleozoic in the Liaohe fault depression was put forward as residual animal fossil fragments were found in some rock sections from the strata. This succession of strata was redefined and the stratal sequence of the Cambrian, Ordovician, Carboniferous and Permian was established on the basis of a study of conodonts, microfloras, animal fossils and rock associations. The results of this study indicate that Paleozoic reservoir rocks exist in the Liaohe fault depression, and that the buried hills of the Liaohe fault depression are not a monocline but a complex faulted block composed of a part of a fold reworked by faults. The conclusion is a new basis on which a new knowledge of the structural features and hydrocarbon reservoir distribution characteristics of the Paleozoic inside the buried hills of the Liaohe fault depression may be gained.
Keywords:determination of the Paleozoic  geological significance  buried hill  Liaohe fault depression
本文献已被 CNKI 维普 万方数据 等数据库收录!
点击此处可从《地质通报》浏览原始摘要信息
点击此处可从《地质通报》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号