松辽盆地白垩系泉头组地层界面特征  

The Stratum Interface Characteristic of Quantou Formation in Songliao Basin

作　　者：张鲁庭[1] 韩刚[1] 

机构地区：[1]东北石油大学地球科学学院,大庆163318

出　　处：《科学技术与工程》2012年第13期3188-3191,共4页Science Technology and Engineering

基　　金：国家重点基础研究发展计划(2006CB701403);国家自然科学基金(40802012)资助

摘　　要：白垩纪是地质历史演化进程中一个重要的时期,中国东北地区乃至整个中国东部蕴含油气盆地大多是这一时期形成的。松辽盆地是白垩纪亚洲古陆上最大的陆相沉积盆地,本文依据泉头组岩心、录井及地震资料,开展了岩石地层学、生物地层学、地震地层学等地质综合应用研究,为重新认识松辽盆地沉积地质发展史和大规模烃源岩形成提供了科学依据。Cretaceous is an important period in geologic history evolvement,the formation of petroleum basin in northeast of China and even east of the hole China is almost at that time.The Songliao Basin is a terrestrial sediment basin during Cretaceous,utilizing large number of core observations,the types of rock facies and sedimentary date in Quantou formation,developing systematically studies lithostratigraphy,biostratigraphy,seismic stratigraphy.etc,providing important science evidence in comprehensioning sediment geologic history and the form of extensive source rock in Songliao Basin.

关 键 词：松辽盆地 白垩纪 泉头组 地层学 

分 类 号：P534.53[天文地球—古生物学与地层学]