摘要
胡状集油沙三＾３亚段浊积岩除发育鲍马层序外，还发育有各种准同生变形构造，槽模，大型交错层理，浪成沙纹层理和深水遗迹化石，该浊积岩复合体为一浊积扇体系，水道浊积岩由砾质和砂质高密度浊流沉积序列组成，而非水道只岩则主要同经典浊积岩组成。
esides developing Bouma sequence, the turbidite in the third submember of Shahejie formation,Huzhuangji Oil Field developed various parasyngennetic deformed structures,flute casts,large scale cross beddings, wave ripple cross beddings and deep water trace fossils.The turbidite complex body belongs to a turbid fan system. The channel turbidite is composed of high density gravel and sand sequence. The non-channel turbidite consists of classic turbidites with Bouma sequence.
出处
《西安石油学院学报》
1996年第2期35-37,共3页
Journal of Xi'an Petroleum Institute
关键词
浊积岩
交错层理
油田
沉积特征
turbidite. cross bedding, trace fossil/[Huzhuangji Oil Field, Dongpu depression. Bouma sequence]
