南海北部白云凹陷早中新世东部沉积体系研究  

Research on the Eastern Depositional System in Early Miocene,Baiyun Sag,Northern South China Sea

作　　者：王永凤[1,2] 王英民[1,2] 徐强[3] 黄振凯 李冬[1,2] 

机构地区：[1]中国石油大学(北京)地球科学学院,北京102249 [2]油气资源与探测国家重点实验室,北京102249 [3]中国海洋石油总公司研究总院,北京100027 [4]中国石油勘探开发研究,北京100083

出　　处：《沉积学报》2012年第3期461-468,共8页Acta Sedimentologica Sinica

基　　金：国家重点基础研究发展计划项目(973计划):(编号:2009CB219407);国家自然科学基金项目(批准号:40572067)资助

摘　　要：基于白云凹陷东部钻井、岩芯和地震资料,通过地震属性分析、地震相分析及钻井岩芯分析,证实了白云凹陷在23.8～21 Ma之间除存在北部物源外还存在来自东沙隆起的东部物源体系,从而扩大了白云凹陷深水碎屑岩沉积研究领域。通过层序地层学研究和沉积相分析,建立了东部沉积体系沉积及演化模式:该体系在低位域形成海底扇沉积;水进域形成碳酸盐岩和硅质碎屑岩混合沉积;高位体系域主要发育高位三角洲沉积,其主要受相对海平面变化及物源供给控制。Based on a large amount of drill,core and seismic data from the eastern Baiyun Sag,by the analysis of seismic attributes,seismic facices as well as drilling sedimentary facies,it is proved that in Baiyun Sag there is not only the north provenance but also the eastern depositional system which is derived from the Dongsha Uplift in early Miocene,and this discovery will lead to the expansion of the exploration scope for the deepwater clastic deposits of Baiyun Sag. The Eastern Depositional System is mainly developed in SQ23.8,with the bottom boundary SB23.8.Previous studies reported that the ＂Baiyun Movement＂ occurred in 23.8 Ma B.P.results in tremendous changes of Baiyun sag,causing the thermal subsidence of the sag,making the shelf neritic environment transform into slope deepwater environment,and SB23.8 is the interface of the shelf break belt migrating from the south of Baiyun sag to north.In 23.8 Ma B.P.the relative sea level fell to the lowest,which made the Panyu Low Uplift in the north and the Dongsha Uplift in the east be in a state of exposure.The formers＇ study has confirmed that the Panyu Low Uplift provides debris for the deep water of Baiyun sag,and then,whether the Dongsha Uplift which was also exposed in SQ23.8 can serve as the provenance for Baiyun sag is the breakthrough point of this paper. The erosion area of Dongsha uplift during early Miocene is about 20 000 km2,which is close to Baiyun sag,and considering such a great erosion area the uplift should provide materials for Baiyun sag.Besides,on the image of 3D seismic RMS amplitude slices present an abnormally high amplitude in the east of Baiyun sag,and the graph of sandstone/strata contour of SQ23.8 also presents high values in the east.In addition,on seismic,a wedge-shaped progradational reflection configuration with the direction from Dongsha Uplift to Baiyun sag in SQ23.8 is developed.Therefore,according to the above analysis,it is concluded that the Dongsha Uplift is one of the provenances of Baiyun sag during the period of SQ23.8 dep

关 键 词：白云凹陷 东沙隆起 物源 沉积模式 

分 类 号：TE121.3[石油与天然气工程—油气勘探]