非海相碳酸盐岩储层结构、成因和类似物的岩石物性特征——钙华、灌木、层状岩和球粒岩

H. Claes, J. Soete, M. Erthal, Ágnes Török, Zahra Mohammadi, Cihan Aratman, T. Miranda, A. Mancini, E. Capezzuoli, J. Schmatz, J. Aguillar, L. Zieger, R. Swennen
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引用次数: 0

摘要

对于南大西洋深部盐下碳酸盐岩储层,缺乏岩心和地震尺度间储层非均质性信息。世界范围内的非海相碳酸盐岩储层类似物提供了定量的几何和岩石物理数据。大型露头具有相似的沉积、成岩、岩石物理和构造特征,可以从岩心尺度下到地震尺度上深入了解储层控制参数
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Non-marine carbonate reservoir architecture, genesis and petrophysical characterisation from analogues - Travertines, Shrubs, Laminites and Spherulites
Summary For the deep South-Atlantic Pre-Salt carbonate reservoirs information on reservoir heterogeneity between core and seismic scale is lacking. Worldwide non-marine carbonate reservoir analogues provide quantitative geometrical and petrophysical data. Large-scale outcrops with similar sedimentological, diagenetic, petrophysical and structural features give insight in reservoir controlling parameters from below core-scale up to seismic scale
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