| 台北凹陷异常高压形成机理探讨 |
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| 引用本文： | 舒克栋,陈振林,宋超.台北凹陷异常高压形成机理探讨[J].资源环境与工程,2007,21(5):512-514. |
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| 作者姓名： | 舒克栋 陈振林 宋超 |
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| 作者单位： | 1. 中国地质大学,研究生院,湖北,武汉,430074
2. 长庆石油勘探局,井下作业处,甘肃,庆阳,745113 |
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| 摘 要： | 在系统总结沉积盆地中异常高压形成机制的基础上,以台北凹陷为实例进行研究,表明:沉积盆地中形成异常高压的机制虽多,但对盆地大规模异常地层压力形成有决定作用的地质作用主要有欠压实作用、烃类生成作用和构造作用。
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| 关 键 词： | 沉积盆地 异常高压 形成机制 台北凹陷 |
| 文章编号： | 1671-1211（2007）05-0512-03 |
| 修稿时间： | 2007-05-10 |
Discussion on the Formation Mechanism of Overpressure in Taibei Depression |
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| SHU Ke-dong,CHEN Zhen-lin,SONG Chao.Discussion on the Formation Mechanism of Overpressure in Taibei Depression[J].Resources Environment & Engineering,2007,21(5):512-514. |
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| Authors: | SHU Ke-dong CHEN Zhen-lin SONG Chao |
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| Abstract: | Based on the systematic conclusion of the overpressure formation mechanism in the sedimentary basin,the authors take Taibei depression as an example,aims to testify that the geological processes which result in large scale abnormal pressure have many reasons,but among the various formation mechanisms,the decisive geological processes mainly to be under compaction,the generation of the hydrocarbon material and tectonic stress. |
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| Keywords: | sedimentary basin overpressure formation mechanism Taibei depression |
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