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| 中国中西部前陆盆地含油气的有序性 | |
| 引用本文： | 郭海洋,常智,赵容容,莫耀汉.中国中西部前陆盆地含油气的有序性[J].沉积与特提斯地质,2008,28(1):65-69. |
| 作者姓名： | 郭海洋 常智 赵容容 莫耀汉 |
| 作者单位： | 1. 成都理工大学能源学院,四川,成都,610059;四川石油管理局地球物理勘探公司,四川,成都,610213 2. 四川石油管理局地球物理勘探公司,四川,成都,610213 3. 中国石油,西安油气田分公司勘探事业部,四川,成都,610041 |
| 摘 要： | 前陆盆地是世界上油气资源最丰富、大油气田最多的一类盆地。笔者通过分析发现中国中西部的前陆盆地有丰富的烃源岩,配套的生储盖组合,油气在纵横向上的发育都有其有序性：前陆盆地的沉积演化控制着盆地油气纵向上的有序性,构造单元控制着油气横向上的有序性。前陆冲断带构造活动强烈,主要形成背斜油气藏,中浅层都含气,适宜采用立体勘探思路。前渊凹陷带主要发育有岩性油气藏,前缘隆起由于地层向克拉通方向尖灭,常形成岩性油气藏。 |
| 关 键 词： | 前陆盆地 构造单元 沉积演化 有序性 |
| 文章编号： | 1009-3850(2008)01-0065-05 |
| 修稿时间： | 2007年6月30日 |
Regularity of the oil and gas accumulation in the foreland basins in western China |
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| GUO Hai-yang,CHANG Zhi,ZHAO Rong-rong,MO Yao-han.Regularity of the oil and gas accumulation in the foreland basins in western China[J].Sedimentary Geology and Tethyan Geology,2008,28(1):65-69. | |
| Authors: | GUO Hai-yang CHANG Zhi ZHAO Rong-rong MO Yao-han |
| Institution: | GUO Hai-yang, CHANG Zhi , ZHAO Rong-rong , MO Yao-han( 1. Chengdu University of Technology, Chengdu 610059, Siehuan, China; 2. Geophysical Prospecting Company, Sichuan Petroleum Administration Bureau, Chengdu 610212, Sichuan, China ; 3. Prospecting Company, Southwestern Branch, PetroChina , Chengdu 610041, Siehuan , China) |
| Abstract: | It is widely perceived that the foreland basins tend to be rich in oil and gas resources throughout the world. The foreland basins in western China also have an abundance of source rocks and advantaged reservoir rocks, and excellent source-reservoir-seal associations. The present paper focuses on the regularity of the horizontal and longitudinal accumulation of oil and gas in the foreland basins in western China. The longitudinal accumulation of oil and gas tend to be controlled by sedimentary evolution, while the horizontal accumulation of oil and gas by tectonic units. The lithologic oil and gas reservoirs are developed in the foreland thrust fault zones due to highly structural activity. The lithologic oil and gas reservoirs are devoloped in the foredeep depression zones and forebulge zones due to the cratonward pinching of strata. |
| Keywords: | foreland basin tectonic unit sedimentary evolution regularity |
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