冀中坳陷调节带构造特征及演化

劳海港; 吴孔友; 陈清华

冀中坳陷调节带构造特征及演化

中国石油大学(华东)地球资源与信息学院, 山东东营 257061

基金项目:

中石油股份有限公司重点科技攻关项目 HBYT-WTY-2008-JS-1

详细信息

作者简介:
劳海港(1978-), 男, 山东东营人, 硕士研究生, 主要从事油区构造解释研究工作, E-mail:920197209@qq.com

中图分类号: TE121.2
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- 文章访问数: 208
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- 被引次数: 0
出版历程
- 收稿日期: 2010-02-21
- 刊出日期: 2010-09-28

GEOLOGIC CHARACTER AND EVOLUTION OF THE ACCOMMODATION ZONE IN THE JIZHONG DEPRESSION

Faculty of Geo-Resource and Information, China University of Petroleum, Dongying 257061, China

摘要

摘要: 利用Morley等的调节构造理论和构造几何学分析, 借助地质构造图、断层垂直位移分析等, 在冀中坳陷识别出5种调节带类型和7种调节带构造形式, 进而探讨了它们各自出现的特定构造部位、调节作用、主要构造特点和典型实例。同向趋近型调节带呈现鼻状、地垒状和转换断层3种构造形式, 在断层段连接处以鼻状构造形式出现, 而在控凹断层连接处则以转换断层与横向凸起并存的形式出现; 同向叠覆型调节带以走向斜坡形式调节应变; 同向平行型调节带以翘曲的形式改造河西务潜山带。对向平行型调节带以低凸起的形式发育于雁翎地区; 对向趋近型调节带以鄚州枢纽带为典型, 受两期应变的调节形成了底部以断层分叉斜滑与上部呈宽阔翘弯带的双层变形系统。产生调节作用的断层在地质演化过程中活动强度均呈现此起彼伏、此消彼长的构造特征。受调节带的影响与改造, 在潜山断坡上可形成以古构造脊为优势运移通道的油气运移路径。
- 冀中坳陷 /
- 调节带 /
- 构造形式 /
- 构造演化 /
- 优势运移通道
Abstract: According to the accommodation structure theory, in combination with the analysis on geological map and paleo-fall, five accommodation zones and seven structure forms have be recognized in Jizhong Depression.The synthetic approaching-type accommodation zone can occur as nose structure, horst and transform fault, e.g., it occurs as nose structure exist in fault segment joints, but as coexistence of transform fault and transverse salient in the joints of faults controlling depression.The synthetic overlap-type accommodation zone transfers strain in the form of trend slope.The synthetic collateral-type accommodation zone reforms the Hexiwu buried hill belt in the form of warping.The convergent collateral-type accommodation zone develops in Yanling area in the form of low uplift.The convergent approaching-type accommodation zone, typically observed in the Maozhou hub zone, forms double-layer deformation system, which comprises a bottom of fault bifurcation oblique slip and an upper of wide cup zone.In the geological evolution, a relation of ebb and flow can be obserbed among the activity intensities of the faults which play the part of accommodation.With the effect and reformation of accommodation zone, a migration path for oil and gas, with ancient structural ridge as dominant migration pathway, can be formed on the slop of buried hill.
- Jizhong depression /
- accommodation zone /
- structure form /
- structure evolution /
- dominant migration pathway

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图 1 冀中坳陷基底断层及调节构造分布图

Figure 1. A map showing distribution of basement faults and accommodation structures in Jozhing Depression

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图 2 冀中坳陷中部第三系底(Tg)构造图

Figure 2. Structural map showing Tertiary bottom boundary(Tg)in central Jizhong Depression

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图 3 冀中坳陷北部基底断层及调节带

Figure 3. Basement faults and accommodation zones in northern Jozhing Depression

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图 4 桐柏镇地垒状横向凸起调节带地震剖面(T2481测线)

Figure 4. Seismic section on the horst-type transverse salient accommodation zone around Tongbai Town

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图 5 苏桥-杨村地区第三系底(Tg)构造图

Figure 5. Structural map showing Tertiary bottom boundary (Tg) in Suqiao-Yangcun area

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图 6 冀中坳陷沙三期沉积环境图^[30]

Figure 6. The deposition environment diagram of Sha 3stage in Jizhong Depression^[30]

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图 7 雁翎潜山带地震剖面(L6470测线)

Figure 7. Seismic section in the Yanling buried hill zone (through 6470 survey line)

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图 8 产生同向趋近型调节带断层在各时期的运动轨迹

Figure 8. The motion trace of the faults which produce the synthetic approaching-type accommodation zone in different period

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图 9 产生同向叠覆型调节带断层在各时期的运动轨迹

Figure 9. The motion trace of the faults which produces the synthetic overlap-type accommodation zone in different periods

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图 10 产生同向平行型调节带断层在各时期的运动轨迹

Figure 10. The motion trace of the faults which produces the synthetic collateral-type accommodation zone in different periods

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图 11 产生对向平行型调节带断层在各时期的运动轨迹

Figure 11. The motion trace of the faults which produce the convergent collateral-type accommodation zone in different period

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图 12 产生对向趋近型调节带断层在各时期的运动轨迹

Figure 12. The motion trace of the faults which produce the convergent approaching-type accommodation zone in different periods

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图 13 任丘潜山断坡Tg构造图(虚线为构造脊延伸方向, 圆圈处为马西洼槽断鼻)

Figure 13. Tg structural map in fault ramp of Renqiu buried hill (dashed line is the extension direction of structure ridge, the circle is fault nose of Maxi)

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表 1 冀中坳陷调节带类型及特征

Table 1. Types and charactetistics of accomodation zone in Jizhong Depression

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