THE INFLUENTIAL FACTORS AND CHARACTRISTICSOF TRIASSIC YANCHANG FORMATION RESERVIORIN LONGDONG AREA, ORDOS BASIN
-
摘要: 以三角洲-湖泊沉积体系为主的陇东地区三叠系延长组主产油层组长3、长6、长7和长8储层岩石类型主要有长石砂岩、岩屑长石砂岩及岩屑砂岩,成分成熟度普遍较低,结构成熟度中等-较好;经历了压实作用、胶结作用和溶解作用,孔隙类型以粒间孔、次生溶孔为主。纵向上,长3油层组储层物性最好;平面上,东北部储层物性明显优于西南部。优质储层多出现在三角洲前缘水下分流河道和河口坝中,碎屑组成、粒级、填隙物含量和成岩作用均对储层性能有重要影响。在陇东地区延长组中识别出简单韵律、复合韵律2大类6种类型储层物性垂向分布模式,而高频基准面旋回的升降控制着本区储层物性韵律的分布规律。Abstract: Chang 3,Chang 6,Chang 7 and Chang 8 Triassic Yanchang formations are the main producing oil layers in Longdong area,Ordos basin.The reservoir-rock types in these formations are arkose,lithic arkose and litharenite with delta and lacustrine facies.Their compositional maturity is low and textural maturity is medium.The clastic rocks experienced compaction,cementation and dissolution,thus producing intergranular pores and secondary solution pores.In profile,the physical properties of Chang 3 reservoirs are the best and in plane,the physical properties of reservoirs in the northeast are obviously better than that in the southwest.Favorable reservoirs mostly occur in the sand bodies in delta-front underwater distributary river channel and river mouth bars.All the composition of clasts,grade scale,content of interstitial materials and diagensis have important effects on the reservoir properties.Six vertical distributional models of reservoir are identified in Yanchang formation in Longdong area.The ascend and descend of base-level cycle with high frequency are main factors which control the distribution of reservoir physical properties.
-
[1] 李凤杰,王多云,郑希民等.陕甘宁盆地陇东地区长3油组坳陷湖盆岩性油藏成藏模式[J].西安石油大学学报(自然科学版),2004,19(3):1~4 [2] 周瑞,胡学智.鄂尔多斯盆地西北部灵盐定地区油藏类型及其控制因素[J].石油实验地质,2001,23(4):390~394 [3] 史基安,王金鹏,毛明陆等.鄂尔多斯盆地西峰油田三叠系延长组长6-8段储层砂岩成岩作用研究[J].沉积学报,2003,21(3):372~380 [4] 窦伟坦.鄂尔多斯盆地城华地区长33油组油气富集的控制因素[J].西安石油学院学报(自然科学版),1999,14(5):1~4 [5] 王志坤,王多云,郑希民等.陕甘宁盆地陇东地区三叠系延长统长6-长8储层沉积特征及物性分析[J].天然气地球科学,2003,14(5):380~385 [6] 席胜利,刘新社,王涛.鄂尔多斯盆地中生界石油运移特征分析[J].石油实验地质.2004,26(3):229~235 [7] 朱怡翔,田昌炳,于兴河等.鄂尔多斯盆地苏里格气田相对高渗砂体的成因及其岩石物理测井识别方法[J].石油实验地质,2004,26(4):389~393 [8] 李春玉,谢渊,刘绍光等.陕北富县延长组特低孔渗砂岩储层控制因素分析[J].成都理工学院学报,2002,29(3):285~289 [9] 郑荣才,尹世民,彭军.基准面旋回结构与叠加式样的沉积动力学分析[J].沉积学报,2000,18(3):369~375 [10] 邓宏文,王洪亮,李熙喆.层序地层基准面的识别、对比技术及应用[J].石油与天然气地质,1996,17(3):177~183 [11] 王多云,郑希民,李凤杰等.低孔渗油气富集区优质储层形成条件及相关问题[J].天然气地球科学,2003,14(2):87~91 [12] 杜春彦,郑荣才.陕北长6油层组短期基准面旋回与储层非均质性的关系[J].成都理工学院学报,1999,26(1):17~22 [13] 李凤杰,王多云,宋广寿等.陕甘宁盆地坳陷型湖盆缓坡带三角洲前缘短期基准面旋回与储层成因分析[J].沉积学报,2004,21(1):73~78
计量
- 文章访问数: 805
- HTML全文浏览量: 131
- PDF下载量: 426
- 被引次数: 0