合肥盆地安参1井中生代地层特征

留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名

邮箱

手机号码

标题

留言内容

验证码

CHARACTERISTICS OF THE MESOZOIC STRATA IN WELL AN’CAN-1 OF THE HEFEI BASIN

1.
Research Institute of Geological Sciences, Shengli Oilfield, SINOPEC, Dongying, Shandong 257015, China
2. Logging Company, Shengli Petroleum Administration, SINOPEC, Dongying, Shandong 257064, China

摘要: 地层是一切地质问题的基础,地层的划分直接影响着对盆地构造演化、沉积环境甚至对全盆地含油气远景的认识。该文从岩性、电性及地震反射特征等方面对安参1井已钻遇地层特征进行研究,初步建立了合肥盆地中生代地层层序格架,对深入认识和解剖盆地的构造演化、地层展布特征、沉积环境及含油气远景具有一定的指导意义。
- 地层特征 /
- 中生代 /
- 安参1井 /
- 合肥盆地
Abstract: The classification of strata has a great effect on the knowledge about structural evolution, sedimentary environment and even evaluation of hydrocarbon potential in a basin. This paper discussed the characteristics of the Mesozoic stratigraphy in well An'can-1 based on lithology, logging response and seismic reflectance. The framework of the Mesozoic stratigraphic sequence was set up, which is meaningful for the appraisal of hydrocarbon potential in the Hefei Basin.
- stratigraphic characteristics /
- Mesozoic /
- well An’can-1 /
- the Hefei Basin

[1]	安徽省地质矿产局.安徽省区域地质志[M]. 北京:地质出版社,1987.165-172.
[2]	韩树,等.安徽北部中新代沉积盆地分析[M]. 北京:地质出版社,1996.84-99.
[3]	朱光,等.郯庐断裂带平移时代的同位素年龄证据[J]. 地质论评,1995,41(5):452-456.