Abstract Xijiang302 Oil Field is located at the substructural belt in southern Huizhou Depression in the Pearl River Mouth basinThis oilfield is mainly distributed in the Zhujiang Formation and the lower part of the Hanjiang Formation of Miocene of Neogene The sedimentary facies of the studied formation is a delta in Xijiang 302 Oil Field In this area, the types of sedimentary microfacies include distributary channel, interdistributary, natural levee and crevasse splay in the delta plain and underwater distributary channel, mouth bar,distributary bar and sand sheet in the delta front The major sandbodies, such as distributary channel, underwater distributary channel and mouth bar, relatively, are thick and continuous Meanwhile, the studied formation consists of 4 longterm base level cycles and 15 midterm base level cycles in Xijiang 302 oilfield On the basis of these, 4 types of logging models about shortterm and supper shortterm base level cycles are summarized in this areaAs for this area, approximately, shortterm base level cycle, which is equal to the fifth order sequence, can be correlated with reservoir strata,while supper shortterm cycle, which corresponds to the sixth order sequence,corresponds to sand body and sedimentary microfacies When correlating the sand bodies based on high resolution sequence stratigraphy, it is very important to take into account the scale of the work area, the tectonic position,the diversities of the sedimentary microfacies and the well spacingIn Xijiang 302 Oil Field, at the reservoir top, the distributary channel or underwater distributary channel mostly with base level rising half cycle is apt to flood,however, the sand bar(distributary mouth bar or distal bar) or distributary bay mainly with base level falling half cycle is not prone to flood ,among which it is propitious to remaining oil distribution.
|
|