利用地温梯度变化在埃及尼罗河三角洲后中新世层序分区中的应用

A. Helaly
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引用次数: 0

摘要

地温梯度是岩石及其组成矿物最重要的热参数之一。地温梯度是反映一个地区地下热状况的重要指标。在对手头的热数据进行必要的校正后,它被用于估计和说明地热梯度随深度的变化。利用这些结果,根据不同地下岩性的热特征,尝试利用这些变化来识别研究区地下岩性成分的变化。在尼罗河三角洲内确定并绘制了四个主要的地下单元。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
USE OF THE GEOTHERMAL GRADIENT VARIATIONS IN ZONING OF POSTMIOCENE SEQUENCE IN THE NILE DELTA, EGYPT
Among the most important thermal parameters of the rocks and their composing minerals is the Geothermal Gradient. Geothermal gradient plays an important role in expressing the subsurface thermal conditions in any area. After carrying out the required corrections for the thermal data in hand, it was used for estimating and illustrating the Geothermal Gradient variations with depth. Using such results, an attempt was carried out to use such variations to identify the subsurface lithologic compositional variations in the study area based on the thermal characteristics of the different subsurface lithologies.Four main subsurface units were identified and mapped within the Nile Delta.
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