内蒙古开鲁盆地陆东凹陷下白垩统九佛堂组—沙海组层序地层格架及沉积相预测  

Sequence stratigraphic framework and sedimentary facies prediction of the Jiufotang and Shahai Formations of Lower Cretaceous in Ludong Sag,Kailu Basin,Inner Mongolia

作　　者：刘明洁[1] 谢庆宾[1] 刘震[1] 孙建[2] 冉波[3] 白鲁山[3] 

机构地区：[1]中国石油大学北京地球科学学院,北京102249 [2]中国石油大港油田采油三厂,河北沧州061023 [3]中国石油辽河油田勘探开发研究院,辽宁盘锦124010

出　　处：《古地理学报》2012年第6期733-746,共14页Journal of Palaeogeography：Chinese Edition

摘　　要：综合利用岩心、测井、地震等资料,对内蒙古开鲁盆地陆东凹陷九佛堂组—沙海组层序地层特征及沉积相进行了系统研究。结果表明,陆东凹陷九佛堂组—沙海组可以识别出3个三级层序界面;划分为2个三级层序(九佛堂层序和沙海层序),分别对应九佛堂组和沙海组;识别出4种主要沉积相类型:扇三角洲相、近岸浊积扇相、远岸浊积扇相及湖泊相。在层序格架内,利用钻、测井资料和二维、三维地震资料对沉积体进行分析,并以此为依据,进一步研究了体系域内沉积相平面展布特征及演化规律,最终建立了该时期沉积发育模式:在盆地陡坡带主要发育扇三角洲和近岸浊积扇,在盆地缓坡主要发育扇三角洲和滨浅湖滩坝沉积,在盆地深洼带主要发育远岸浊积扇和风暴岩。Comprehensively using cores, logging and seismic data, the sequence stratigraphic fea- tures and sedimentary facies of the Lower Cretaceous Jiufotang Formation and Shahai Formation in Ludong Sag, Kailu Basin, have been studied systematically. Three 3rd order sequence boundaries and two 3rd order sequences are identified in the two formations. Four kinds of sedimentary facies are identified, in- cluding fan delta, proximal turbidite fan, offshore turbidite fan and lacustrine facies. Within the se- quence stratigraphic framework, the depositional bodies are researched by using well drilling, logging,2D and 3D-seismic data. Furthermore, the distribution of sedimentary facies and tracts have been researched, and the depositional model of this period was built evolution law in system According to the model, fan delta dominately developed on the steep slope, while fan delta and beach bars developed on the gentle slope belt, and off-shore turbidite fan and tempestites developed in the deep depression zones in Ludong Sag.

关 键 词：开鲁盆地 陆东凹陷 下白垩统 九佛堂组 沙海组 层序地层 沉积相 

分 类 号：P539.2[天文地球—古生物学与地层学]