| 吐鲁番—哈密盆地的构造特征 |
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| 引用本文： | 赵文智,袁非.吐鲁番—哈密盆地的构造特征[J].石油学报,1992,13(3):9-18. |
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| 作者姓名： | 赵文智 袁非 |
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| 作者单位： | 1. 北京石油勘探开发科学研究院;2. 石油地球物理勘探局;3. 玉门石油管理局 |
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| 摘 要： | 根据地震、重磁力与露头资料的分析,认为吐哈盆地具有双层基底,即中新生界之下存在上古生界褶皱与前寒武系结晶基底;周边山系属三大不同构造单元,其中以博格达陆内裂谷带和克拉美丽——麦钦乌拉山岛弧——大洋碰撞缝合带对盆地生成发展控制最明显;盆地为多盆地原型迭合复合的盆地;将局部构造分为正花状、反转、冲断与秃顶和短轴背斜等构造样式,使之统一于扭动、冲断与基岩生长三大构造组合之中.
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| 关 键 词： | 吐鲁番—哈密盆地 构造特征 盆地类型 基底 残留坳陷 拉分盆地 花状构造 反转构造 构造组合 |
| 收稿时间： | 1991-03-29 |
THE STRUCTURAL CHARACTERISTICS OF TURPAN-HARMY BASIN |
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| Zhao Wenzhi,Yuan Fei,Zeng Xiaoming.THE STRUCTURAL CHARACTERISTICS OF TURPAN-HARMY BASIN[J].Acta Petrolei Sinica,1992,13(3):9-18. |
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| Authors: | Zhao Wenzhi Yuan Fei Zeng Xiaoming |
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| Affiliation: | 1. Research Institute of Petroleum Explorationand Development, Beijing;2. Petroleum Geophysical Exploration, CNPC;3. Yumen Petroleum Administration |
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| Abstract: | Based on an analysis of seismic,gravity and magnetic data,and the data from a study of outorops,it is suggested that there are double basements in the Turpan-Harmy basin; Combrian crystalline basement being underneath the upper paleozoic folding baseuevt beneath the Ceno-mesozoic formations.Boundary mountains belong to 3 different tectonic units.Among them Bogeda intracontinental rift and Kelameili-Maiqinwula island arcocenic collisson stylolit belt controls the formation and development of the basin most sinificantly.This basin is a composite basin with a super position of multiple prototype basins; Local structures are divided into various types,such as positive flower,reversed,overthrust,frustum,and short axis anticlines and is unified into a combination of 3 main tectonic movementstorsional,overthrust,and basement growing. |
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