山东孤岛油田馆陶组沉积晚期浅水振荡湖泊沉积

ISSN 1000-0550 CN 62-1038/P

高级搜索

留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名
邮箱
手机号码
标题
留言内容
验证码

山东孤岛油田馆陶组沉积晚期浅水振荡湖泊沉积

文章导航 > 沉积学报 > 2007 > 25(1): 82-89

王蛟. 山东孤岛油田馆陶组沉积晚期浅水振荡湖泊沉积[J]. 沉积学报, 2007, 25(1): 82-89.

引用本文:

王蛟. 山东孤岛油田馆陶组沉积晚期浅水振荡湖泊沉积[J]. 沉积学报, 2007, 25(1): 82-89.

WANG Jiao. Shallow Oscillating Lacustrine Sediment of the Late Guantao Formation in Gudao Oilfield, Shandong Province[J]. Acta Sedimentologica Sinica, 2007, 25(1): 82-89.

Citation:

WANG Jiao. Shallow Oscillating Lacustrine Sediment of the Late Guantao Formation in Gudao Oilfield, Shandong Province[J]. Acta Sedimentologica Sinica, 2007, 25(1): 82-89.

王蛟. 山东孤岛油田馆陶组沉积晚期浅水振荡湖泊沉积[J]. 沉积学报, 2007, 25(1): 82-89.

引用本文:

王蛟. 山东孤岛油田馆陶组沉积晚期浅水振荡湖泊沉积[J]. 沉积学报, 2007, 25(1): 82-89.

WANG Jiao. Shallow Oscillating Lacustrine Sediment of the Late Guantao Formation in Gudao Oilfield, Shandong Province[J]. Acta Sedimentologica Sinica, 2007, 25(1): 82-89.

Citation:

WANG Jiao. Shallow Oscillating Lacustrine Sediment of the Late Guantao Formation in Gudao Oilfield, Shandong Province[J]. Acta Sedimentologica Sinica, 2007, 25(1): 82-89.

山东孤岛油田馆陶组沉积晚期浅水振荡湖泊沉积

王蛟

中国石油化工股份有限公司胜利油田分公司博士后科研工作站山东东营 257015

通讯作者:
王蛟

计量

文章访问数: 1995
HTML全文浏览量: 16
PDF下载量: 603
被引次数: 0

Shallow Oscillating Lacustrine Sediment of the Late Guantao Formation in Gudao Oilfield, Shandong Province

WANG Jiao

Work Station of Postdoctoral, Shengli Oil Field , SINOPEC, Dongying, Shandong 257015

More Information

Corresponding author: WANG Jiao

摘要: 浅水振荡湖泊是一种特殊的浅水湖泊沉积类型，湖盆地形平坦、湖面广阔、水体极浅，广大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。馆陶组馆1+2砂层组沉积时期浅水振荡湖泊广泛发育，表现为高频红、灰泥岩互层、物源供应不足、浅水湖泊沉积构造及生物成因构造发育、水进→水退沉积旋回明显的沉积特征。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砂层组浅水振荡湖泊沉积模式。
- 孤岛油田 /
- 馆陶组 /
- 馆1+2砂层组 /
- 浅水湖泊 /
- 沉积模式
Abstract: Shallow oscillating lacustrine deposit is a special kind of shallow lake, while the lake topography is smooth, lake surface is wide, and water body is very shallow. Lake plane which mainly influenced by climate rise or fall in vibrating type. Deposit mainly is mostly alternative red mudstone and grey mudstone, indicating oxidizing and reducing environment. Shallow oscillating lacustrine deposit extensively developed in the late period of Guantao Formation (Ng1+2 sand sets) in Gudao Oilfield. Deposit features show that high frequency alternative mostly red and grey mudstone, sedimentary structure generally occur in shallow lakes and creature structure growing, water plane rise to decline depositional cycle obviously. Through taking the observation of core hole, describing and analyzing lab test results, five microfacies(water channel, sand flat, mixed flat, mud flat and marsh) can be distinguished and established the high water period and low flow period sedimentary model of Ng1+2 sand sets in Gudao Oilfield.
- Gudao Oilfield /
- Guantao Formation /
- Ng1+2 sand sets /
- shallow lakes /
- sedimentary model

参考文献(0)

资源附件(0)

WeChat

点击查看大图

计量

文章访问数: 1995
HTML全文浏览量: 16
PDF下载量: 603
被引次数: 0

山东孤岛油田馆陶组沉积晚期浅水振荡湖泊沉积

王蛟

中国石油化工股份有限公司胜利油田分公司博士后科研工作站山东东营 257015

通讯作者: 王蛟

收稿日期: 1900-01-01
修回日期: 1900-01-01
刊出日期: 2007-02-10

关键词:

馆1+2砂层组 /

摘要: 浅水振荡湖泊是一种特殊的浅水湖泊沉积类型，湖盆地形平坦、湖面广阔、水体极浅，广大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。馆陶组馆1+2砂层组沉积时期浅水振荡湖泊广泛发育，表现为高频红、灰泥岩互层、物源供应不足、浅水湖泊沉积构造及生物成因构造发育、水进→水退沉积旋回明显的沉积特征。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砂层组浅水振荡湖泊沉积模式。

English Abstract

王蛟. 山东孤岛油田馆陶组沉积晚期浅水振荡湖泊沉积[J]. 沉积学报, 2007, 25(1): 82-89.

引用本文:

王蛟. 山东孤岛油田馆陶组沉积晚期浅水振荡湖泊沉积[J]. 沉积学报, 2007, 25(1): 82-89.

WANG Jiao. Shallow Oscillating Lacustrine Sediment of the Late Guantao Formation in Gudao Oilfield, Shandong Province[J]. Acta Sedimentologica Sinica, 2007, 25(1): 82-89.

Citation:

WANG Jiao. Shallow Oscillating Lacustrine Sediment of the Late Guantao Formation in Gudao Oilfield, Shandong Province[J]. Acta Sedimentologica Sinica, 2007, 25(1): 82-89.

全文HTML

/

下载: 全尺寸图片幻灯片

分享

用微信扫码二维码

分享至好友和朋友圈

返回

x 关闭永久关闭