[1]朱 键,王小军,吴宝成,等.准噶尔盆地南缘玛河气田紫泥泉子组沉积相[J].新疆石油地质,2015,36(06):648.[doi:10.7657/XJPG20150604]
 ZHU Jian,WANG Xiaojun,WU Baocheng,et al.Sedimentary Facies of Palaeogene Ziniquanzi Formation in Mahe Gas Field in Southern Margin of Junggar Basin[J].Xinjiang Petroleum Geology,2015,36(06):648.[doi:10.7657/XJPG20150604]
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准噶尔盆地南缘玛河气田紫泥泉子组沉积相()
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《新疆石油地质》[ISSN:1001-3873/CN:65-1107/TE]

卷:
36
期数:
2015年06期
页码:
648
栏目:
出版日期:
2015-12-01

文章信息/Info

Title:
Sedimentary Facies of Palaeogene Ziniquanzi Formation in Mahe Gas Field in Southern Margin of Junggar Basin
文章编号:
1001-3873(2015)06-0648-08
作者:
朱 键王小军吴宝成姜元刚高 阳谢宗瑞
(中国石油 新疆油田分公司 勘探开发研究院,新疆 克拉玛依 834000)
Author(s):
ZHU Jian WANG Xiaojun WU Baocheng JIANG Yuangang GAO Yang XIE Zongrui
(Research Institute of Exploration and Development, Xinjiang Oilfield Company, PetroChina, Karamay, Xinjiang 834000, China)
关键词:
准噶尔盆地南缘玛河气田紫泥泉子组辫状河三角洲沉积相
Keywords:
Junggar basin southern margin Mahe gas field Ziniquanzi formation braided river delta sedimentary facies
分类号:
TE111.3
DOI:
10.7657/XJPG20150604
文献标志码:
A
摘要:
对准噶尔盆地南缘古近系紫泥泉子组的沉积构造背景、沉积相标志进行分析,认为玛河气田紫泥泉子组为辫状河三角洲沉积,发育辫状河三角洲平原、三角洲前缘、前三角洲3种亚相及水下分流河道等8种微相,整体显示湖退—湖侵的沉积演化特征。对比沉积相与物性、产能特征后认为,最有利的沉积微相为水下分流河道。
Abstract:
This paper analyzes the sedimentary structural setting and sedimentary facies symbol of Ziniquanzi formation of the Paleogene in southern margin of Junggar basin, and suggests that the Ziniquanzi formation in this area appears braided river delta deposits, and develops such three subfacies as delta plain, delta front and prodelta as well as eight microfacies like underwater distributary channel and others. The overall displays the evolution characteristics of lake regression and transpression. The contrast of the sedimentary facies, petrophysical property and productivity performance indicates that the most favorable sedimentary microfacies is the underwater distributary channel

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更新日期/Last Update: 2015-12-25