维也纳盆地的区域泥石压缩趋势:顶层密封评估和对提升历史的影响
Lukas Skerbisch1, David Misch1, Michael Drews2
1Montanuniversitaet Leoben, Peter Tunner Straße 5, 8700 Leoben, Austria.
概括
密封品质对于石油系统和储存至关重要. 这项研究使用泥石压缩趋势来预测维也纳盆地的密封能力,揭示了潜在的垂直碳化合物迁移途径.
科学领域:
- 地质科学是地球科学.
- 石油地质学 石油地质学
- 地质能源应用 地质能源应用
背景情况:
- 密封品质评估对于石油系统和地下储存至关重要.
- 毛细血管突破压力决定了连续密封的顶部密封能力.
- 区域压缩-孔度趋势为泥石毛细管性质提供了一个预测工具,在这种情况下,直接测量很少.
研究的目的:
- 建立维也纳盆地泥石的理论压缩趋势.
- 将理论趋势与测量的毛细血管压力数据进行比较.
- 评估泥石密封能力和碳化合物迁移潜力.
主要方法:
- 分析中高米奥森泥石核心样本 (700-3400米深).
- X射线衍光测量,C/S分析,矿物学和有机含量的岩石-Eval热解.
- 扫描电子显微镜,侵入孔径测量,以及皮cnometry 孔隙结构属性.
主要成果:
- 孔隙深度明显下降的趋势表明,维也纳盆地中部的机械紧缩是均的.
- 与全球趋势的比较表明,上米奥森时代的区域升起和侵蚀高达500米的岩层.
- 岩石质量S1和生产指数 (PI) 的增加与密封能力的下降相关,这表明垂直碳化合物迁移.
结论:
- 理论压缩模型可以使用盆地特定数据进行校准.
- 维也纳盆地泥石趋势意味着重要的区域地质历史 (升起/侵蚀).
- 观察到的趋势表明潜在的垂直迁移途径,对于未来的海研究和储存应用至关重要.
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