摘要
依据相关的岩心、薄片、野外露头等资料,对中古15井区良里塔格组沉积相特征进行研究,作出了沉积相平面展布图。研究表明,该井区海平面自下而上水体逐渐加深,发育有台地边缘相和开阔台地相。
According to the related core data,thin plate,the field outcrop,this paper studies sedimentary facies characteristics of the Middle Ages 15 wells of Lianglitage.Studies have shown that the sea-level of well area shows the process of gradually deepening from bottom to up,and develops granular limestone,micrite and biological limestone.
出处
《重庆科技学院学报（自然科学版）》
CAS
2013年第3期22-25,共4页
Journal of Chongqing University of Science and Technology：Natural Sciences Edition
基金
国家科技重大专项(2008ZX05004-004)
四川省重点学科建设项目(SZD0414)
关键词
中古15井区
良里塔格组
沉积相
middle ages 15-well area
Lianglitage group
sedimentary facies
