准噶尔盆地四棵树凹陷多期应力场作用下的构造演化特征

郭宏辉; 何新明; 朱林涛; 冯建伟; 杜赫; 曲君晓

doi:10.19509/j.cnki.dzkq.tb20240006

准噶尔盆地四棵树凹陷多期应力场作用下的构造演化特征

doi: 10.19509/j.cnki.dzkq.tb20240006

1.
中国石化西北油田分公司, 乌鲁木齐 830011
2.
中国矿业大学资源与地球科学学院, 江苏徐州 221116
3.
中国石油大学(华东)地球科学与技术学院, 山东青岛 266580
4.
山东黄金三山子金矿, 山东莱州 261442

基金项目:

国家自然科学基金项目 42072234

中石化科研项目 P23064

详细信息

作者简介:
郭宏辉, E-mail: guohonghui_0326@126.com

通讯作者:
冯建伟, E-mail: linqu_fengjw@126.com

中图分类号: P618.13
计量
- 文章访问数: 67
- PDF下载量: 8
- 被引次数: 0
出版历程
- 收稿日期: 2024-01-05
- 录用日期: 2024-05-06
- 修回日期: 2024-03-17

Evolution of structural characteristics with multistage stress fields in the Sikeshu Sag, Junggar Basin

1.
Northwest Oilfield Company, SINOPEC, Urumqi 830011, China
2.
School of Resources and Geosciences, China University of Mining and Technology, Xuzhou Jiangsu 221116, China
3.
School of Geosciences, China University of Petroleum(East China), Qingdao Shandong 266580, China
4.
Sanshanzi Gold Mine, Shandong Gold Group, Laizhou Shandong 261442, China

More Information

Author Bio:
GUO Honghui, E-mail: guohonghui_0326@126.com

Corresponding author: FENG Jianwei, E-mail: linqu_fengjw@126.com

摘要

摘要:
准噶尔盆地南缘四棵树凹陷位于北天山山前冲断带西段, 盆地自古生代以来经历了多期、多向的构造运动; 明确研究区构造系统特征及其演化过程, 对此类含油气盆地的油气勘探开发具有重要意义。在前人地质研究的基础上, 结合详细的地震资料解释、地质调查与地层发育特征, 根据研究区构造发育背景, 以四棵树凹陷构造格局的变动和多期应力场为线索, 对四棵树凹陷构造演化过程进行了系统性分析。研究表明, 四棵树凹陷深部发育挤压反转-走滑构造层、浅部发育推覆-滑脱构造层; 平面上根据构造样式发育特征可划分为南部挤压断褶带、中部走滑压扭带、北部隆起带; 凹陷经历了2期强烈的构造隆升期, 对应2期断裂活动高峰期; 构造环境及应力场条件发生了多次转变, 晚石炭世至早中二叠世为弧后裂陷背景下的NNW-SSE向伸展裂陷期、晚二叠世至三叠纪为扎伊尔山造山运动下NNW-SSE向挤压的断坳转换期、晚侏罗世至古近纪为周缘造山带与车排子凸起的共同作用下NNW-SSE向挤压陆内坳陷期、新近纪为北天山强烈的造山活动背景下NS向挤压作用的复活前陆盆地期。通过探讨多期应力场作用下四棵树凹陷的构造演化特征, 进一步深入认识了此类含油气盆地整体构造格局的变动过程, 也为研究区油气资源下一步勘探提供了新思路。
- 准噶尔盆地南缘 /
- 四棵树凹陷 /
- 山前冲断带 /
- 构造系统 /
- 构造演化 /
- 应力场
Abstract: Objective
The Sikeshu Sag of the southern Junggar Basin is tectonically located in the western thrust belt of the North Tianshan Mountains. The basin has undergone multiple stages and multidirectional tectonic movements since the Palaeozoic. Clarifying the structural characteristics and evolutionary process of the structural system in the study area is critical for petroleum exploration and development in such petroliferous basins.
Methods
Utilizing the seismic data interpretation and the outcrop geological investigation of the Sikeshu Sag, spatial-temporal variations in the structural patterns and stress fields were revealed, and a tectonic evolution model was established.
Results
This study indicates that the compressional inversion and strike-slip structures were widely developed in the deep-buried layers of the Sikeshu Sag, but the thrust and decollement structures were more prevail in the shallow layers of the Sikeshu Sag. According to the structural style, the Sikeshu Sag can be divided into the southern compressional fault-fold belt, central strike-slip compressive-torsional belt, and northern uplift belt. The Sikeshu Sag experienced two periods of strong tectonic uplift, corresponding to the peak period of two stages of fault activity. The tectonic environment and stress field conditions underwent multiple changes: the NNW-SSE extension driven by the back-arc rifting during the late Carboniferous to early-middle Permian, the rift-depression transition triggered by the NNW-SSE extrusion of the Zaire orogenic movement during the late Permian to Triassic, the regional depression induced by the NNW-SSE extrusion of the peripheral orogenic belt and Chepaizi uplift during the late Jurassic to Palaeogene, and the reactivation of foreland caused by NS extrusion of North Tianshan Mountains during the Neogene.
Conclusion
This study explores the tectonic evolution of the Sikeshu Sag under multiphase stress fields, which favors the better understanding of the overall tectonic pattern changes in similar petroliferous basins and provides new insights for the next steps of petroleum exploration in the study area.
- southern Junggar Basin /
- Sikeshu Sag /
- foreland thrust belt /
- structural pattern /
- structural evolution /
- stress field
注释:

所有作者声明不存在利益冲突。

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图 1 四棵树凹陷区域构造特征

a.准噶尔盆地构造单元划分; b.准噶尔盆地周缘断层发育纲要; c.四棵树凹陷侏罗系顶面构造图; d.四棵树凹陷地层综合柱状图

Figure 1. Regional tectonic characteristics of Sikeshu Sag

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图 2 四棵树凹陷地震剖面构造解释(地层代号同图 1, 地震剖面位置见图 1c)

Figure 2. Structural interpretation of seismic section in the Sikeshu Sag

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图 3 四棵树凹陷构造样式分布规律

a.垂向分层构造特征；b.平面构造样式分布特征

Figure 3. Distribution characteristics of structural styles in the Sikeshu Sag

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图 4 四棵树凹陷构造分带特征

a.四棵树凹陷构造分带；b.各分带褶皱发育特征

Figure 4. Structural zoning characteristics of the Sikeshu Sag

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图 5 四棵树凹陷地质露头构造缝发育特征

a.四棵树凹陷南部地质特征；b.石炭系多期缝切割关系；c.三叠系多期共轭缝发育特征；d.石炭系共轭缝指示最大主应力方向；e.石炭系张性缝与剪切缝的限制关系; f.A—A′剖面特征

Figure 5. Structural characteristics on outcrops of Sikeshu Sag

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图 6 四棵树凹陷各层系地层共轭剪切缝走向

Figure 6. Strikes of conjugate fractures in each layer of Sikeshu Sag

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图 7 四棵树凹陷周缘新生代板块运动及应力场

a.北天山构造带板块运动矢量图；b.四棵树凹陷内各区域应力场特征

Figure 7. Cenozoic plate movement and stress field around the Sikeshu Sag

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图 8 四棵树凹陷构造演化剖面(剖面位置见图 1c, 下同)

a.GT1-SC1井构造演化剖面；b.G1-GT1井构造演化剖面

Figure 8. Structural evolution profiles of the Sikeshu Sag

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图 9 四棵树凹陷各沉积时期地层压缩特征

Figure 9. Stratum compression characteristics of different periods in the Sikeshu Sag

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图 10 四棵树凹陷地层格架(a, b)及盆地剖面演化特征(c)

a.研究区北部地层格架；b.研究区南部地层格架；c.盆地剖面演化特征

Figure 10. Stratigraphic framework(a, b) and basin profile evolution characteristics(c) of the Sikeshu Sag

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图 11 四棵树凹陷各阶段构造演化三维模式

Figure 11. Three-dimensional model of tectonic evolution in different stages of the Sikeshu sag

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表 1 二叠系岩墙走向与共轭缝指示应力方向

Table 1. Strike of the Permian dyke and the stress direction indicated by conjugate joints

二叠系岩墙走向/(°)	数量/条	C-P共轭缝应力方向/(°)	数量/组	J-K共轭缝应力方向/(°)	数量/组	E-N共轭缝应力方向/(°)	数量/组
[0, 15)	0	[0, 15)	0	[0, 15)	21	[0, 15)	11
[15, 30)	0	[15, 30)	0	[15, 30)	13	[15, 30)	15
[30, 45)	0	[30, 45)	0	[30, 45)	0	[30, 45)	0
[45, 60)	0	[45, 60)	0	[45, 60)	0	[45, 60)	8
[60, 75)	0	[60, 75)	0	[60, 75)	4	[60, 75)	0
[75, 90)	0	[75, 90)	0	[75, 90)	0	[75, 90)	0
[90, 105)	0	[90, 105)	10	[90, 105)	2	[90, 105)	0
[105, 120)	12	[105, 120)	20	[105, 120)	0	[105, 120)	0
[120, 135)	5	[120, 135)	0	[120, 135)	0	[120, 135)	0
[135, 150)	3	[135, 150)	16	[135, 150)	0	[135, 150)	5
[150, 165)	0	[150, 165)	0	[150, 165)	6	[150, 165)	0
[165, 180]	0	[165, 180]	4	[165, 180]	12	[165, 180]	24

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表 2 四棵树凹陷南缘断层产状数据

Table 2. Fault occurrence data for the south margin of the Sikeshu Sag

断层倾向/(°)	数量/条	断层倾角/(°)	数量/条
[0, 30)	15	[0, 15)	49
[30, 60)	21	[15, 30)	28
[60, 90)	6	[30, 45)	19
[90, 120)	4	[45, 60)	14
[120, 150)	7	[60, 75)	7
[150, 180)	12	[75, 90]	6
[180, 210)	16
[210, 240)	26
[240, 270)	5
[270, 300)	2
[300, 330)	5
[330, 360]	4

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