[1]张新见,张曰静,穆玉庆,等.准噶尔盆地四棵树凹陷古近系沉积体系及演化分析[J].复杂油气藏,2019,12(01):17.[doi:10.16181/j.cnki.fzyqc.2019.01.004]
　ZHANG Xinjian,ZHANG Yuejing,MU Yuqing,et al.Analysis on sedimentary system and evolution of Paleogene inSikeshu Sag, Junggar Basin[J].Complex Hydrocarbon Reservoirs,2019,12(01):17.[doi:10.16181/j.cnki.fzyqc.2019.01.004]
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准噶尔盆地四棵树凹陷古近系沉积体系及演化分析()
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《复杂油气藏》[ISSN:1674-4667/CN:31-2019/TQ]

卷:
12卷
期数:
2019年01期
页码:
17
栏目:
油气勘探
出版日期:
2019-03-25

文章信息/Info

Title:
Analysis on sedimentary system and evolution of Paleogene inSikeshu Sag, Junggar Basin
作者:
张新见; 张曰静; 穆玉庆; 商丰凯; 杨东根; 陈 林
中国石化胜利油田分公司勘探开发研究院,山东 东营 257015
Author(s):
ZHANG Xinjian; ZHANG Yuejing; MU Yuqing; SHANG Fengkai; YANG Donggen; CHEN Lin
Exploration and Development Research Institute of Shengli Oilfield Company,SINOPEC,Dongying 257015,China
关键词:
沉积体系 沉积演化 古近系 四棵树凹陷 准噶尔盆地
Keywords:
sedimentary system;  sedimentary evolution;  Paleogene;  Sikeshu Sag;  Junggar Basin
分类号:
TE122
DOI:
10.16181/j.cnki.fzyqc.2019.01.004
文献标志码:
A
摘要:
通过对露头及岩心的观察和研究后发现,准噶尔盆地四棵树凹陷古近系主要接受来自北部扎伊尔山以及南部依林黑比尔根山两大物源体系的供给。发育的沉积相类型多样:紫泥泉子组沉积时期广泛发育滨浅湖亚相,仅在凹陷北部发育小型扇三角洲扇群,在南部山前带发育冲积扇相、辫状河流相以及辫状河三角洲相; 安集海河组沉积时期古气候由干旱转湿润,受湖盆扩张的影响,在凹陷北部继承性发育退积型扇三角洲,而南部山前带仅发育辫状河三角洲相,凹陷中央在XH1井—T1井一线开始出现半深湖亚相。本文明确了四棵树凹陷古近系不同物源沉积体系的展布及演化规律,对该地区有利勘探方向的优选具有一定的借鉴意义。
Abstract:
According to the observation and study of outcrops and cores, it was found that the Paleogene in Sikeshu Sag, Junggar Basin, mainly received supplies from Zaire Mountain in the north of the sag and Eren Habirga Mountain in the south of the sag. The sedimentary facies in this area are various. Shore-shallow lake subfacies are widely developed in the sedimentary period of the Ziniquanzi Formation, while small fan delta group is only developed in the north of the Sag, and alluvial fan facies, braided fluvial facies and braided river delta facies are developed in the southern piedmont zone. The paleoclimate changed from drought to wet in the sedimentary period of Anjihaihe Formation which led to the expansion of the lake basin. So retrogradation type fan deltas are developed inherently in the northern of the sag, and braided river delta facies are only developed in the southern piedmont zone. Semi-deep lacustrine subface began to appear in the area between well XH1 to well T1.In this study, the distribution and evolution of sedimentary systems of the Paleogene in Sikeshu Sag have been clarified. The results provide some reference for the optimal selection of favorable exploration direction in this area.

参考文献/References:

[1] 沈玉林,郭英海,李壮福,等.准南山前断褶带紫泥泉子组层序地层及岩相古地理[J].新疆石油地质,2006,27(2):169-172.
[2] 杨勇,陈世悦,王桂萍,等.准噶尔盆地车排子地区古近系沉积相研究[J].油气地质与采收率,2011,18(3)5-9.
[3] 高志勇,韩国猛,朱如凯,等.准噶尔盆地南缘古近纪—新近纪前陆盆地沉积格局与演变[J].古地理学报,2009,11(5):491-502.
[4] 沈玉林,郭英海,李壮福,等.准噶尔盆地南缘山前断褶带紫泥泉子组沉积相[J].新疆石油地质,2008,29(6):716-734.
[5] 肖立新,陈能贵,张健,等.准噶尔盆地南缘古近系紫泥泉子组沉积体系分析[J].天然气地球科学,2011,22(3):426-431.
[6] 庄新明.准噶尔盆地四棵树凹陷石油地质特征及勘探方向[J].新疆地质,2006,24(4):429-433.
[7] 哈丽娅,喻春辉,热依汗古丽,等.准噶尔盆地北天山山前主要勘探目的层沉积格架[J].新疆石油地质,2000,21(6):476-479.
[8] 覃军,林小云,潘虹,等.准噶尔盆地南缘四棵树凹陷及周缘油源关系研究[J].矿物岩石地球化学通报,2014,33(3):395-400.
[9] 黄彦庆,侯读杰.准噶尔盆地四棵树凹陷原油地球化学特征分析[J].天然气地球科学,2009,20(2):282-286.
[10] 程欣.准噶尔盆地四棵树凹陷油气资源评价[D].荆州:长江大学,2013:16-29.
[11] 郭春清.准噶尔盆地四棵树凹陷生油潜力评价[D].成都:成都理工大学,2005:45-46.
[12] 张枝焕,向奎,秦黎明,等.准噶尔盆地四棵树凹陷烃源岩地球化学特征及其对车排子凸起油气聚集的贡献[J].中国地质,2012,39(2):326-337.
[13] 李博.准噶尔盆地南缘紫泥泉子组沉积特征研究[D].青岛:中国石油大学(华东),2011:70-75.
[14] 李骞,田孝茹,胡瀚文,等.天山北缘安集海河组湖相灰岩氧碳同位素变化的古环境意义[J].地球科学与环境学报,2016,38(3):398-409.
[15] 邵雨,雷德文,纪有亮,等.准噶尔盆地南缘古近—新近系沉积相及储层特征[M].北京:石油工业出版社,2016:68-69.

备注/Memo

备注/Memo:
收稿日期:2018-12-17; 改回日期:2019-01-28。第一
作者简介:张新见(1982—),硕士,工程师,主要从事石油地质综合解释研究。E-Mail: tedy.zhang@163.com。
基金项目:国家科技重大专项(2016ZX05002-002); 中国石油化工股份有限公司项目(P13021)。
更新日期/Last Update: 2019-03-25