| 缓坡带成藏模式研究--以陈家庄地区为例 |
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| 引用本文： | 范振峰. 缓坡带成藏模式研究--以陈家庄地区为例[J]. 新疆石油天然气, 2005, 1(1): 39-42 |
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| 作者姓名： | 范振峰 |
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| 作者单位： | 胜利油田地质院,山东,东营,257015 |
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| 摘 要： | 陈家庄地区属于典型的宽缓型缓坡带，依据其构造特点，可划分为凸起带、斜坡带和构造坡折带三大构造单元，不同的构造单元上发育有不同的沉积类型和油藏类型，其成藏控制因素亦有较大的差别。
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| 关 键 词： | 缓坡带 构造单元 成藏控制因素 |
| 文章编号： | 1673-2677(2005)01-0039-04 |
| 修稿时间： | 2005-01-12 |
THE HYBROCARBON RESERVOIR FORMING MODEL OF THE GENTLE SLOPE--TAKING CHENJIAZHUANG AREA AS AN EXAMPLE |
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| FAN Zhen-feng. THE HYBROCARBON RESERVOIR FORMING MODEL OF THE GENTLE SLOPE--TAKING CHENJIAZHUANG AREA AS AN EXAMPLE[J]. Xinjiang Oil & Gas, 2005, 1(1): 39-42 |
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| Authors: | FAN Zhen-feng |
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| Affiliation: | FAN Zhen-feng. Geological Institue,ShengliOilfield,dongying Shandong 257015 |
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| Abstract: | Chenjiazhuang area is attributed to the typical broad gentle slope. There are three structure units, the bumpsalience zone, the clinoform zone, and the slope break zone, according to the structural characteristics. The differentdepositional type and hydrocarbon reservoir type developed on the different structure units, and the controlling factorsof hydrocarbon reservoir forming are different too. |
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| Keywords: | the gentle slope the structure unit the controlling factor of hydrocarbon reservoir forming |
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