山东国土资源2012，Vol.28Issue(3)：1-4,4.
临清坳陷晚古生代沉积环境及演化分析
Analysis on Sedimentary Environment and Evolution in Late Paleozoic Era in Linqing Depression
摘要
Abstract
In this paper,sedimentary system and facies of Linqing depression have been analyzed.Through contrast and study on sedimentary facies of connecting wells,its vertical evolution characteristics have been summarized.It is showed that the platform-lagoon sedimentary system,barrier-lagoon-tidal flat sedimentary system,tidal flat sedimentary system,fluvial-controlled shallow-water deltaic sedimentary system and river-lake sedimentary system are mainly developed in the late Paleozoic in Linqing depression.The evolution of sedimentary facies in vertical direction is very clear.Marine environment sedimentary is mainly developed in Benxi and Taiyuan period in late Carboniferous and early Permian period;transitional facies environment sedimentary is mainly developed in Permian Shanxi period;and terrestrial environment sedimentary is mainly developed in Permian Shihezi period.关键词
晚古生代/沉积体系/沉积相/演化分析/临清坳陷Key words
Late Palaeozoic/sedimentary system/sedimentary facies/evolution analysis/Linqing depression分类
天文与地球科学引用本文复制引用
赵洪刚,梁吉坡,陈晓燕..临清坳陷晚古生代沉积环境及演化分析[J].山东国土资源,2012,28(3):1-4,4.基金项目
中国博士后科学基金第四十七批面上资助 （）
山东科技大学研究生科技创新基金资助 （）
