[1]陆梅娟,于雯泉,王 路,等.高邮凹陷阜一段含油砂岩成岩作用特征[J].复杂油气藏,2013,(04):11.
 Lu Meijuan,Yu Wenquan,Wang Lu,et al.Diagenetic character of oil-bearing sandstone in the first member of Funing Formation in Gaoyou Sag[J].Complex Hydrocarbon Reservoirs,2013,(04):11.
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高邮凹陷阜一段含油砂岩成岩作用特征
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《复杂油气藏》[ISSN:1674-4667/CN:31-2019/TQ]

卷:
期数:
2013年04期
页码:
11
栏目:
油气勘探
出版日期:
2013-12-25

文章信息/Info

Title:
Diagenetic character of oil-bearing sandstone in the first member of Funing Formation in Gaoyou Sag
作者:
陆梅娟于雯泉王 路张 哲李 翔
中国石化江苏油田分公司地质科学研究院,江苏 扬州 225009
Author(s):
Lu MeijuanYu WenquanWang LuZhang ZheLi Xiang
Geological Scientific Research Institute of Jiangsu Oilfield Company,SINOPEC,Yangzhou,Jiangsu 225009
关键词:
含油砂岩 次生溶蚀孔隙 阜一段 高邮凹陷
Keywords:
oil-bearing sandstone secondary corrosion pore 1st member of Funing Formation Gaoyou Sag
分类号:
TE122.23
文献标志码:
A
摘要:
通过实验室微观分析,直观展示了高邮凹陷阜一段含油砂岩的成岩特征及孔隙特征。阜一段含油砂岩成岩早期在微晶、粉晶状碳酸盐胶结、压实作用下,使原生孔隙遭受大部分损失; 成岩后期显著的成岩作用特点是早期碳酸盐胶结物发生了溶解作用,储集空间主要为次生溶蚀孔隙,具有较高的孔隙度。研究认为含油砂岩次生溶蚀孔隙的形成与油气运移聚集之间有必然的相关性,它是烃类活动的必然结果。
Abstract:
The diagenesis and pore characteristics of oil-bearing sandstones in Gaoyou Sag are visually studied by means of the micro-analysis in laboratory.Cementation and compaction of microcrystalline and powder crystalline carbonate in oil-bearing sandstone of the 1st member of Funing Formation are prevailing in the early stage of diagenesis which contribute to the major loss of the primary pore.Oil-bearing sandstone in the later stage of diagenesis is characterized by dissolution of early carbonate cement which brings secondary corrosion pores with high porosity.It is implied that the inevitable correlation between the formation of secondary corrosion pores and the migration and accumulation of hydrocarbon.

参考文献/References:

[1] 牛世忠.红岗油田高台子油藏成岩相研究[J].石油天然气学报,2012,34(6):43-46.
[2] 朱世发,朱筱敏.准格尔盆地西北缘克百地区三叠系储层溶蚀作用特征及孔隙演化[J].沉积学报,2010,28(3):547-554.
[3] 宋秋花.高邮凹陷北斜坡阜宁组储层成岩作用特征[J].断块油气田,2009,16(5):20-22.
[4] 施振飞.苏北盆地高邮凹陷阜宁组储层次生孔隙成因机制探讨[J].沉积学报,2005,23(3):429-435.
[5] 傅强,陈海洲.苏北盆地高邮凹陷古近系阜宁组储层成岩相特征[J].成都理工大学学报(自然科学版),2008,35(3):225-231.
[6] 西北大学地质系(编译).碎屑岩的成岩作用[M].陕西:西北大学出版社,1986:25-85.
[7] 张琴.东营凹陷下第三系碎屑岩储层孔隙演化与次生孔隙成因[J].石油与天然气地质,2003,24(3):281-284.
[8] 王芙蓉,何生.准噶尔盆地腹部永进地区砂岩储层中碳酸盐胶结物特征及其成因意义[J].岩石矿物学杂志,2009,28(2):170-177.
[9] 张厚福,方朝亮,高先志,等.石油地质学[M].北京:石油工业出版社,1999:109-112.
[10] 袁静,王乾泽.东营凹陷下第三系深部碎屑岩储层次生孔隙垂向分布及成因分析[J].石油学报,2003,24(1):44-48.

备注/Memo

备注/Memo:
收稿日期:2013-06-26; 改回日期:2013-07-31
作者简介:陆梅娟(1963—),女,高级工程师,现主要从事石油地质勘探生产及研究工作。电话:0514-87761347,E-mail:lumj.jsyt@sinopec.com。
攻关项目:江苏油田分公司(JS 12005)
更新日期/Last Update: 2013-12-25