| 鄂尔多斯盆地中部奥陶系方解石脉中包裹体流体势研究 |
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| 引用本文： | 单秀琴 胡国艺 高嘉玉. 鄂尔多斯盆地中部奥陶系方解石脉中包裹体流体势研究[J]. 岩石学报, 2003, 19(2): 355-358 |
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| 作者姓名： | 单秀琴 胡国艺 高嘉玉 |
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| 作者单位： | 中国石油勘探开发研究院廊坊分院,廊坊,065007 |
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| 摘 要： | 结合前人研究成果，归纳出了一种利用盐水包裹体均一温度与盐度确定流体势的方法，并对鄂尔多斯盆地中部气田奥陶系方解石脉中包裹体进行了流体势计算，推算出了古流体运移方向。
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| 关 键 词： | 流体包裹体 流体势 方解石 鄂尔多斯 |
| 修稿时间： | 2002-11-20 |
Paleocurrent energy study with inclusion of calcite gangue for Ordovician system in central Ordos basin. |
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| SHAN XiuQin,HU GuoYi and GAO JiaYu Lang fang Branch of RIPED of PetroChin,Langfang,China. Paleocurrent energy study with inclusion of calcite gangue for Ordovician system in central Ordos basin.[J]. Acta Petrologica Sinica, 2003, 19(2): 355-358 |
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| Authors: | SHAN XiuQin HU GuoYi GAO JiaYu Lang fang Branch of RIPED of PetroChin Langfang China |
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| Abstract: | Paleocurrent potential energy is an important parameter to determine directions of paleocurrent migration. This paper puts forward a method to calculate paleocurrent potential energy with homogenization temperature and salinity of brine inclusion. Paleocurrent potential energy with inclusions of calcite gangue for Ordovician System in central Ordos Basin is calculated using this method and directions of paleocurrent migration is reckoned in this area. |
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| Keywords: | Fluid inclusion Paleocurrent potential energy Calcite Ordors |
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