鄂尔多斯盆地东部高家堡地区下古生界断裂分层变形特征及形成机制

陈平; 李明瑞; 李维; 强敏; 路鹏程; 于小伟; 韩伟

doi:10.11781/sysydz202403542

鄂尔多斯盆地东部高家堡地区下古生界断裂分层变形特征及形成机制

doi: 10.11781/sysydz202403542

1.
中国石油东方地球物理勘探有限责任公司研究院长庆分院, 西安 710021
2.
中国石油长庆油田分公司勘探事业部, 西安 710018

基金项目:

中国石油科学研究与技术开发项目“海相碳酸盐岩重点领域综合地质研究与高效勘探关键技术攻关” 2022KT0103

详细信息

作者简介:
陈平(1995—)，男，硕士，工程师，从事构造地质学研究。E-mail：243801601@qq.com

中图分类号: TE121.2
计量
- 文章访问数: 252
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- PDF下载量: 35
- 被引次数: 0
出版历程
- 收稿日期: 2023-06-25
- 修回日期: 2024-03-29
- 刊出日期: 2024-05-28

Characteristics and formation mechanism of stratified deformation of Lower Paleozoic faults in Gaojiapu area, eastern Ordos Basin

1.
Changqing Branch, Geophysical Research Institute, BGP, PetroChina, Xi'an, Shaanxi 710021, China
2.
Exploration Department, Changqing Oilfield Company, PetroChina, Xi'an, Shaanxi 710018, China

摘要

摘要: 近年来，鄂尔多斯盆地奥陶系马家沟组五段以深地层相继取得勘探突破，揭示了其巨大的勘探潜力。随着高精度三维地震资料的部署以及油气勘探的深入，断裂对马五段以深气藏的控制作用越发凸显。基于高精度三维地震资料，在系统刻画高家堡地区断裂几何学特征的基础上，解剖断裂典型构造样式，建立断裂形成演化模式，并结合钻井试气资料探讨断裂对马五段以深气藏差异富集的控制作用。研究取得了以下认识：鄂尔多斯盆地高家堡地区下古生界断裂具有明显的分层变形特征，盆地内马三段、马五段两套膏盐岩是造成断裂分层的主要原因之一；高家堡地区下古生界主要发育具有压扭性质的走滑断裂和逆冲断裂；通过对高家堡地区地层构造形态及断裂样式的研究，推测燕山构造运动是对加里东构造运动形成的断裂影响最大的一期后期改造运动；高家堡地区地层构造隆升期与油气充注期耦合，断裂具有改善储层、沟通源岩、控制圈闭等多重作用。
- 燕山期 /
- 加里东期 /
- 断裂分层 /
- 奥陶系 /
- 高家堡地区 /
- 鄂尔多斯盆地
Abstract: In recent years, exploration breakthroughs have been successively achieved in the strata deeper than the fifth member of the Lower Ordovician Majiagou Formation in the Ordos Basin, revealing its tremendous exploration potential. With the deployment of high-precision 3D seismic data and the deepening of oil and gas exploration, the control exerted by faults on the gas reservoirs in the deeper layers of the fifth member has become increasingly prominent. Based on high-precision 3D seismic data, this study systematically characterized the geometric features of faults in the Gaojiabao area, dissected typical fault structural patterns, established fault formation and evolution models, and, in conjunction with drilling and testing data, discussed the control of faults on the differential enrichment of gas reservoirs in the deeper layers of the Majiagou Formation. The study yielded the following insights: Faults in the Lower Paleozoic of the Gaojiabao area in the Ordos Basin exhibit distinct stratified deformation characteristics, with the two sets of gypsum-salt rocks in the third and fifth members being major contributors to fault stratification. The Lower Paleozoic in the Gaojiabao area mainly develops strike-slip faults with compressional and torsional properties and thrust faults. Through studying the structural morphology and fault patterns of the Gaojiabao area, it is inferred that the Yanshan tectonic movement was the most significant phase of reformation affecting the faults formed during the Caledonian tectonic movement. The coupling of the structural uplift period with the oil-gas charging period in the Gaojiabao area means that faults play multiple roles, including improving reservoirs, connecting source rocks, and controlling traps.
- Yanshanian age /
- Caledonian age /
- fault stratification /
- Ordovician /
- Gaojiapu area /
- Ordos Basin
注释:

利益冲突声明/Conflict of Interests

所有作者声明不存在利益冲突。

All authors disclose no relevant conflict of interests.

作者贡献/Authors’Contributions

陈平、李维参与论文写作和修改；李明瑞、强敏提供修改意见；路鹏程、于小伟、韩伟提供资料解释和资料支持；所有作者均阅读并同意最终稿件的提交。

CHEN Ping and LI Wei participated in the writing and revision of the paper. LI Mingrui and QIANG Min provided revision suggestions. LU Pengcheng, YU Xiaowei and HAN Wei provided data interpretation and data support. All authors have read the last version of the paper and consented to its submission.

HTML全文

图 1 鄂尔多斯盆地东部高家堡地区研究区位置(a)和盆地中东部下奥陶统地层柱状图(b)

Figure 1. Regional location of study area (a) in Gaojiapu area in eastern Ordos Basin and histogram of Lower Ordovician of central and eastern Ordos Basin (b)

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图 2 鄂尔多斯盆地东部高家堡地区多层系顺层相干及断裂平面展布

Figure 2. Coherence and fault plane layout of multilayer system in Gaojiapu area, eastern Ordos Basin

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图 3 鄂尔多斯盆地东部高家堡地区典型地震剖面

剖面位置见图 2。

Figure 3. Typical seismic profile of Gaojiapu area, eastern Ordos Basin

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图 4 鄂尔多斯盆地东部高家堡地区下古生界断裂构造样式

Figure 4. Fault structure pattern of Lower Paleozoic in Gaojiapu area, eastern Ordos Basin

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图 5 鄂尔多斯盆地东部高家堡地区下古生界断裂分层模式

Figure 5. Stratification model of Lower Paleozoic faults in Gaojiapu area, eastern Ordos Basin

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图 6 鄂尔多斯盆地东部高家堡地区下伏凸起带活动性

Figure 6. Activity of underlying uplift zone in Gaojiapu area, eastern Ordos Basin

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图 7 鄂尔多斯盆地东部高家堡地区奥陶系马家沟组四段底断裂活动性

Figure 7. Activity of bottom faults of fourth member of Ordovician Majiagou Formation in Gaojiapu area, eastern Ordos Basin

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图 8 鄂尔多斯盆地东部高家堡地区断裂与构造分层结构

Figure 8. Fault and stratified structure of Gaojiapu area, eastern Ordos Basin

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图 9 鄂尔多斯盆地东部高家堡地区加里东期断裂形成演化及后期改造立体模式

Figure 9. Stereoscopic model of Caledonian fault formation and evolution and late reconstruction in Gaojiapu area, eastern Ordos Basin

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图 10 鄂尔多斯盆地东部高家堡地区米探1井与米探2井油藏剖面

Figure 10. Reservoir profiles of wells Mitan 1 and Mitan 2 in Gaojiapu area, eastern Ordos Basin

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