首页> 外文期刊>Journal of Seismic Exploration >VELOCITIES OF COMPRESSIONAL AND SHEAR WAVES IN LIMESTONES AND DOLOMITES IN A GAS FIELD OF SW IRAN
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VELOCITIES OF COMPRESSIONAL AND SHEAR WAVES IN LIMESTONES AND DOLOMITES IN A GAS FIELD OF SW IRAN

机译:SW伊朗气田中石灰岩和白云岩的压缩和剪切波速度

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摘要

Carbonates are the second important lithologies, after silicates, in petroleum reserves. Using three wells and DSI tools in one of the gas reservoirs in the Persian Gulf, Iran, four equations between compressional and shear wave velocities have been determined for limestones and dolomites. Then, these relationships have been compared with Castagna's relationships. It is concluded that Castagna's relationships estimated for Vs are less than the actual values in limestones and dolomites in the area of study. Using different crossplots, the gas and dolomitization effects on seismic velocities are studied. Consequently, understanding the gas and dolomitization effects make it possible to separate gas-saturated zones from water-saturated, and dolomites from limestones.
机译:碳酸盐是石油储量中仅次于硅酸盐的第二重要岩性。在伊朗波斯湾的一个气藏中,使用三口井和DSI工具,已经确定了石灰岩和白云岩在压缩波速度和剪切波速度之间的四个方程。然后,将这些关系与Castagna的关系进行了比较。结论是,卡斯塔尼亚对Vs的估计关系小于研究区域石灰石和白云岩的实际值。使用不同的交叉图,研究了气体和白云石化对地震速度的影响。因此,了解气体和白云石化作用后,就可以将饱和气体与水饱和区分开,将白云岩与石灰石分开。

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