歧口凹陷中奥陶统沉积相特征再认识
Acta Geologica Sichuan(2012)
Abstract
歧口凹陷奥陶系地层发育碳酸盐岩沉积,主要为泥晶灰岩、泥晶白云岩、岩溶角砾岩。综合岩相、沉积构造特征及测井相分析重新确定其沉积相类型为开阔台地、局限台地和蒸发台地,提高了对歧口凹陷奥陶系古岩溶发育情况的认识,为该区油气勘探预测有利区带提供了可靠依据。
MoreTranslated text
Key words
restricted platform,Ordovician,Qikou depression,sedimentary facies,open platform
AI Read Science
Must-Reading Tree
Example
![](https://originalfileserver.aminer.cn/sys/aminer/pubs/mrt_preview.jpeg)
Generate MRT to find the research sequence of this paper
Chat Paper
Summary is being generated by the instructions you defined