J4

• 基础地质·矿产·盆地 • 上一篇    下一篇

山东沾化凹陷孤岛油田馆上段浅水湖泊沉积

王 蛟1,2   

  1. 1.中国石油化工股份有限公司 胜利油田有限公司孤岛采油厂,山东 东营 257231;2.中国石油化工股份有限公司 胜利油田有限公司博士后科研工作站,山东 东营 257015
  • 收稿日期:2006-07-15 修回日期:1900-01-01 出版日期:2007-05-26 发布日期:2007-05-26
  • 通讯作者: 王蛟

Oscillating Shallow Lacustrine Sediment of the Upper Guantao Formation of Gudao Oilfield in Zhanhua Seg,Shandong Province

WANG Jiao1,2   

  1. 1.Gudao Oil Production Factory, Shengli Oil Field, SINOPEC, Dongying, Shandong 257231, China;2.Work Station of Postdoctoral, Shengli Oil Field, SINOPEC, Dongying, Shandong 257015, China
  • Received:2006-07-15 Revised:1900-01-01 Online:2007-05-26 Published:2007-05-26
  • Contact: WANG Jiao

摘要: 综合研究钻井、古生物和测井资料,认为孤岛油田新近系馆陶组上段馆1+2砂层组沉积时期发育浅水湖泊而非单一的河流相沉积。浅水湖泊湖盆地形平坦,湖面广阔,水体极浅;湖区受气候影响,湖平面频繁振荡式升降变化;沉积物多表现为氧化、还原环境交替的红灰相间的细粒沉积物;湖泊沉积构造发育,生物富集,水进→水退沉积旋回性明显。通过取心井的观察描述和分析化验,识别出水道砂坝、砂坪、混合坪、泥坪和沼泽5种沉积微相类型,建立了孤岛油田馆1+2砂层组浅水湖泊沉积模式。

关键词: 孤岛油田, 馆陶组, 馆1+2砂层组, 浅水湖泊, 沉积模式

Abstract: Based on comprehensive study of outcrops, fossils, drilling data and well logging, shallow lacustrine facies, instead of unitary fluvial facies, were recognized in the sandstone-bearing sequence of upper Guantou Formabion, in Gudao oilfield. The shallow lacustrine deposits are special in that the lake topography is smooth, lake surface is wide, water body is very shallow. Lake level changes are frequent influenced by mainly the corresponding climate changes. Deposit mainly are alternative mostlyred mudstone and grey mudstone which showing oxidizing and reducing environment. Sedimentary features show that sedimentary structure generally occur in shallow lakes and creature genesis structure growing, waterplane rise→decline depositoinal cycle obviously. Through taking the observation of core hole, describe and analyse lab test, five microfacies(water channel, sand flat, mixed flat, mud flat and marsh) can be distinguished, established the sedimentary model of Ng1+2 sand sets in Gudao oilfield.

Key words: Gudao oilfield, Guantao Formation, Ng1+2 sand sets, shallow lakes, sedimentary model

中图分类号: 

  • P512.2
[1] 刘海, 林承焰, 张宪国, 王宏伟, 付晓亮, 李佳. 孔店油田馆陶组辫状河储层构型及剩余油分布规律[J]. 吉林大学学报(地球科学版), 2018, 48(3): 665-677.
[2] 朱兆群, 林承焰, 张宪国, 李志鹏, 谢晶晶, 魏肃东, 程平. 断陷湖盆早期浅水三角洲沉积——以高邮凹陷永安地区戴一段为例[J]. 吉林大学学报(地球科学版), 2017, 47(3): 659-673.
[3] 张建坤, 杨国涛, 吴吉忠, 吴鑫, 王方鲁. 黄骅坳陷北部马头营凸起馆陶组砂体成因及展布特征[J]. 吉林大学学报(地球科学版), 2017, 47(1): 48-60.
[4] 单敬福, 张吉, 王继平, 赵忠军, 李浮萍, 陈治华, 石林辉, 刘利峰. 苏里格气田西区盒8亚段辫状河沉积论证与分析[J]. 吉林大学学报(地球科学版), 2015, 45(6): 1597-1607.
[5] 张晶, 刘化清, 李双文, 冀虎山, 袁淑琴, 洪忠. 断陷湖盆深水重力流水道的识别标志及沉积模式——以歧口凹陷歧南斜坡沙一段为例[J]. 吉林大学学报(地球科学版), 2015, 45(3): 701-711.
[6] 李顺明, 宋新民, 刘曰强, 王友启, 李艳明, 唐后军. 温米退积型与进积型浅水辫状河三角洲沉积模式[J]. J4, 2011, 41(3): 665-672.
[7] 伊振林, 吴胜和, 杜庆龙, 张保国, 岳大力, 李艳平. 冲积扇储层构型精细解剖方法--以克拉玛依油田六中区下克拉玛依组为例[J]. J4, 2010, 40(4): 939-946.
[8] 孔庆莹, 程日辉. 塔里木盆地孔雀河地区寒武系-下奥陶统沉积特征[J]. J4, 2010, 40(3): 527-534.
[9] 刘士林,刘蕴华,林 舸,周 叶,龚发雄,张德圣. 南堡凹陷新近系馆陶组砂岩地球化学、构造背景和物源探讨[J]. J4, 2007, 37(3): 475-0483.
[10] 张 晶,王伟锋,荣启宏,史文东. 东营凹陷永55区块沙四上亚段深水浊积扇沉积与油气[J]. J4, 2007, 37(3): 519-0524.
[11] 张健,刘招君,杜江峰,柳蓉,王伟涛,柳世友,荆保泽. 黑龙江省依兰盆地古近系达连河组油页岩沉积特征[J]. J4, 2006, 36(6): 980-0985.
[12] 王 蛟,姜在兴,操应长,邢焕清,王艳忠,罗文生. 山东东营凹陷永921地区沙四上亚段扇三角洲沉积与油气[J]. J4, 2005, 35(06): 725-0731.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
No Suggested Reading articles found!