首页> 外文期刊>Arabian Journal for Science and Engineering. Section A, Sciences >Rock Physics Relations Derived from Petrophysical Logs for Indus Offshore Area, Pakistan
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Rock Physics Relations Derived from Petrophysical Logs for Indus Offshore Area, Pakistan

机译:巴基斯坦梧桐近海地区从岩石物理测井得到的岩石物理关系

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摘要

Conventional seismic interpretation provides subsurface geometric information, while quantitative seismic interpretation can provide lithologic and fluid information, including saturations, porosity, density, Poisson's ratio and other elastic parameters. Rock physics is the main science behind quantitative interpretation and includes a number of transforms, in the form of empirical relations, for the computation of various rock properties. In addition, crossplot templates of these properties help in facies modeling and reservoir characterization. This paper presents rock physics transforms between compressional velocity, shear velocity, density, porosity, resistivity and gamma ray radiation for Cretaceous to Miocene strata in the Indus offshore area, Pakistan. These transforms are empirical relations established through regression analysis between various petrophysical parameters. Logs from twelve wells have been used in the analysis to give a good representation of rock properties in the area. Most of the relations have a linear correlation coefficient above 0.74 and therefore can be used reliably in quantitative interpretation of seismic data.
机译:常规地震解释可提供地下几何信息,而定量地震解释可提供岩性和流体信息,包括饱和度,孔隙率,密度,泊松比和其他弹性参数。岩石物理学是定量解释背后的主要科学,包括经验关系形式的许多变换,用于计算各种岩石特性。此外,这些属性的交叉图模板还有助于进行相模型和储层表征。本文介绍了巴基斯坦印度河近海地区白垩纪至中新世地层在压缩速度,剪切速度,密度,孔隙度,电阻率和伽马射线辐射之间的岩石物理转换。这些转换是通过各种岩石物理参数之间的回归分析建立的经验关系。分析中使用了来自12口井的测井数据,以很好地表示该地区的岩石特性。大多数关系具有大于0.74的线性相关系数,因此可以可靠地用于地震数据的定量解释。

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